Quaternary monogenetic volcanoes in southern China: eruption styles and controlling factors
Abstract The Hainan Island-Leizhou Peninsula-Beibu Gulf volcanic field (HLBVF) in southern China (covering an area of over 7000 $ km^{2} $) contains at least 50 cinder cones and 12 maar volcanoes. It is one of a few barely studied volcanic fields of Quaternary age in China. The eruption styles, and...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Li, Yongquan [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2022 |
|---|
| Schlagwörter: |
|---|
| Anmerkung: |
© International Association of Volcanology & Chemistry of the Earth's Interior 2022 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Bulletin of volcanology - Berlin : Springer, 1924, 84(2022), 8 vom: 01. Aug. |
|---|---|
| Übergeordnetes Werk: |
volume:84 ; year:2022 ; number:8 ; day:01 ; month:08 |
| Links: |
|---|
| DOI / URN: |
10.1007/s00445-022-01587-z |
|---|
| Katalog-ID: |
SPR04773566X |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | SPR04773566X | ||
| 003 | DE-627 | ||
| 005 | 20230509105034.0 | ||
| 007 | cr uuu---uuuuu | ||
| 008 | 220802s2022 xx |||||o 00| ||eng c | ||
| 024 | 7 | |a 10.1007/s00445-022-01587-z |2 doi | |
| 035 | |a (DE-627)SPR04773566X | ||
| 035 | |a (SPR)s00445-022-01587-z-e | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 100 | 1 | |a Li, Yongquan |e verfasserin |0 (orcid)0000-0002-4491-0618 |4 aut | |
| 245 | 1 | 0 | |a Quaternary monogenetic volcanoes in southern China: eruption styles and controlling factors |
| 264 | 1 | |c 2022 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a Computermedien |b c |2 rdamedia | ||
| 338 | |a Online-Ressource |b cr |2 rdacarrier | ||
| 500 | |a © International Association of Volcanology & Chemistry of the Earth's Interior 2022 | ||
| 520 | |a Abstract The Hainan Island-Leizhou Peninsula-Beibu Gulf volcanic field (HLBVF) in southern China (covering an area of over 7000 $ km^{2} $) contains at least 50 cinder cones and 12 maar volcanoes. It is one of a few barely studied volcanic fields of Quaternary age in China. The eruption styles, and controlling factors that led to the formation of this volcanic field, are thus not yet clear. This study provides a first investigation of the general geology of the HLBVF volcanoes as well as preliminary discussion of the controlling factors affecting the eruption styles. Early Pleistocene (> 1 Ma) and/or earlier (Pliocene) volcanic activity mainly occurred in the form of high-flux magmatic eruptions that formed a large amount of thick lava units and/or cinder cones, which have since experienced intense erosion. The late early Pleistocene to late Pleistocene (~ 1.08–0.03 Ma) phreatomagmatism is represented by maar volcanoes and shows that the initial eruptions were commonly phreatomagmatic events but had increasingly magmatic components in later periods, which reflects sustained, but lower magma fluxes than in the early Pleistocene. The Holocene magmatic eruptions (< 10 ka) primarily formed agglutinate, bomb, and lapilli units, as well as lava flows. These deposits were emplaced mainly by pyroclastic fallout from Hawaiian-style eruptions. This work indicates that eruption styles between magmatic and phreatomagmatic eruptions in the HLBVF were not directly related to fluctuations in annual precipitation and magma compositions. Pre-existing NW-trending faults likely controlled the vent locations, and water fed along fault zones might have supported sustained phreatomagmatism, which formed the large maar volcanoes. The fluctuation of magma fluxes, and water supply linked to long-term tropical climate changes, coupled with regional faults, were likely the three main factors that controlled eruption styles in the HLBVF. | ||
| 650 | 4 | |a Monogenetic volcanoes |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Eruption styles |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Controlling factors |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Magma flux |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Tropical climate |7 (dpeaa)DE-He213 | |
| 773 | 0 | 8 | |i Enthalten in |t Bulletin of volcanology |d Berlin : Springer, 1924 |g 84(2022), 8 vom: 01. Aug. |w (DE-627)253390397 |w (DE-600)1458483-9 |x 1432-0819 |7 nnns |
| 773 | 1 | 8 | |g volume:84 |g year:2022 |g number:8 |g day:01 |g month:08 |
| 856 | 4 | 0 | |u https://dx.doi.org/10.1007/s00445-022-01587-z |z lizenzpflichtig |3 Volltext |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_SPRINGER | ||
| 912 | |a GBV_ILN_11 | ||
| 912 | |a GBV_ILN_20 | ||
| 912 | |a GBV_ILN_22 | ||
| 912 | |a GBV_ILN_23 | ||
| 912 | |a GBV_ILN_24 | ||
| 912 | |a GBV_ILN_31 | ||
| 912 | |a GBV_ILN_32 | ||
| 912 | |a GBV_ILN_39 | ||
| 912 | |a GBV_ILN_40 | ||
| 912 | |a GBV_ILN_60 | ||
| 912 | |a GBV_ILN_62 | ||
| 912 | |a GBV_ILN_63 | ||
| 912 | |a GBV_ILN_69 | ||
| 912 | |a GBV_ILN_70 | ||
| 912 | |a GBV_ILN_73 | ||
| 912 | |a GBV_ILN_74 | ||
| 912 | |a GBV_ILN_90 | ||
| 912 | |a GBV_ILN_95 | ||
| 912 | |a GBV_ILN_100 | ||
| 912 | |a GBV_ILN_105 | ||
| 912 | |a GBV_ILN_110 | ||
| 912 | |a GBV_ILN_120 | ||
| 912 | |a GBV_ILN_138 | ||
| 912 | |a GBV_ILN_150 | ||
| 912 | |a GBV_ILN_151 | ||
| 912 | |a GBV_ILN_152 | ||
| 912 | |a GBV_ILN_161 | ||
| 912 | |a GBV_ILN_170 | ||
| 912 | |a GBV_ILN_171 | ||
| 912 | |a GBV_ILN_187 | ||
| 912 | |a GBV_ILN_213 | ||
| 912 | |a GBV_ILN_224 | ||
| 912 | |a GBV_ILN_230 | ||
| 912 | |a GBV_ILN_250 | ||
| 912 | |a GBV_ILN_267 | ||
| 912 | |a GBV_ILN_281 | ||
| 912 | |a GBV_ILN_285 | ||
| 912 | |a GBV_ILN_293 | ||
| 912 | |a GBV_ILN_370 | ||
| 912 | |a GBV_ILN_381 | ||
| 912 | |a GBV_ILN_602 | ||
| 912 | |a GBV_ILN_636 | ||
| 912 | |a GBV_ILN_702 | ||
| 912 | |a GBV_ILN_2001 | ||
| 912 | |a GBV_ILN_2003 | ||
| 912 | |a GBV_ILN_2004 | ||
| 912 | |a GBV_ILN_2005 | ||
| 912 | |a GBV_ILN_2006 | ||
| 912 | |a GBV_ILN_2007 | ||
| 912 | |a GBV_ILN_2008 | ||
| 912 | |a GBV_ILN_2009 | ||
| 912 | |a GBV_ILN_2010 | ||
| 912 | |a GBV_ILN_2011 | ||
| 912 | |a GBV_ILN_2014 | ||
| 912 | |a GBV_ILN_2015 | ||
| 912 | |a GBV_ILN_2018 | ||
| 912 | |a GBV_ILN_2020 | ||
| 912 | |a GBV_ILN_2021 | ||
| 912 | |a GBV_ILN_2025 | ||
| 912 | |a GBV_ILN_2026 | ||
| 912 | |a GBV_ILN_2027 | ||
| 912 | |a GBV_ILN_2031 | ||
| 912 | |a GBV_ILN_2034 | ||
| 912 | |a GBV_ILN_2037 | ||
| 912 | |a GBV_ILN_2038 | ||
| 912 | |a GBV_ILN_2039 | ||
| 912 | |a GBV_ILN_2044 | ||
| 912 | |a GBV_ILN_2048 | ||
| 912 | |a GBV_ILN_2049 | ||
| 912 | |a GBV_ILN_2050 | ||
| 912 | |a GBV_ILN_2055 | ||
| 912 | |a GBV_ILN_2056 | ||
| 912 | |a GBV_ILN_2057 | ||
| 912 | |a GBV_ILN_2059 | ||
| 912 | |a GBV_ILN_2061 | ||
| 912 | |a GBV_ILN_2064 | ||
| 912 | |a GBV_ILN_2065 | ||
| 912 | |a GBV_ILN_2068 | ||
| 912 | |a GBV_ILN_2088 | ||
| 912 | |a GBV_ILN_2093 | ||
| 912 | |a GBV_ILN_2106 | ||
| 912 | |a GBV_ILN_2107 | ||
| 912 | |a GBV_ILN_2108 | ||
| 912 | |a GBV_ILN_2110 | ||
| 912 | |a GBV_ILN_2111 | ||
| 912 | |a GBV_ILN_2112 | ||
| 912 | |a GBV_ILN_2113 | ||
| 912 | |a GBV_ILN_2118 | ||
| 912 | |a GBV_ILN_2122 | ||
| 912 | |a GBV_ILN_2129 | ||
| 912 | |a GBV_ILN_2143 | ||
| 912 | |a GBV_ILN_2144 | ||
| 912 | |a GBV_ILN_2147 | ||
| 912 | |a GBV_ILN_2148 | ||
| 912 | |a GBV_ILN_2153 | ||
| 912 | |a GBV_ILN_2188 | ||
| 912 | |a GBV_ILN_2190 | ||
| 912 | |a GBV_ILN_2232 | ||
| 912 | |a GBV_ILN_2336 | ||
| 912 | |a GBV_ILN_2446 | ||
| 912 | |a GBV_ILN_2470 | ||
| 912 | |a GBV_ILN_2472 | ||
| 912 | |a GBV_ILN_2507 | ||
| 912 | |a GBV_ILN_2522 | ||
| 912 | |a GBV_ILN_2548 | ||
| 912 | |a GBV_ILN_4035 | ||
| 912 | |a GBV_ILN_4037 | ||
| 912 | |a GBV_ILN_4112 | ||
| 912 | |a GBV_ILN_4125 | ||
| 912 | |a GBV_ILN_4126 | ||
| 912 | |a GBV_ILN_4242 | ||
| 912 | |a GBV_ILN_4246 | ||
| 912 | |a GBV_ILN_4249 | ||
| 912 | |a GBV_ILN_4251 | ||
| 912 | |a GBV_ILN_4305 | ||
| 912 | |a GBV_ILN_4306 | ||
| 912 | |a GBV_ILN_4307 | ||
| 912 | |a GBV_ILN_4313 | ||
| 912 | |a GBV_ILN_4322 | ||
| 912 | |a GBV_ILN_4323 | ||
| 912 | |a GBV_ILN_4324 | ||
| 912 | |a GBV_ILN_4325 | ||
| 912 | |a GBV_ILN_4326 | ||
| 912 | |a GBV_ILN_4328 | ||
| 912 | |a GBV_ILN_4333 | ||
| 912 | |a GBV_ILN_4334 | ||
| 912 | |a GBV_ILN_4335 | ||
| 912 | |a GBV_ILN_4336 | ||
| 912 | |a GBV_ILN_4338 | ||
| 912 | |a GBV_ILN_4393 | ||
| 912 | |a GBV_ILN_4700 | ||
| 951 | |a AR | ||
| 952 | |d 84 |j 2022 |e 8 |b 01 |c 08 | ||
| author_variant |
y l yl |
|---|---|
| matchkey_str |
article:14320819:2022----::utrayooeeivlaosnotenhneutosyea |
| hierarchy_sort_str |
2022 |
| publishDate |
2022 |
| allfields |
10.1007/s00445-022-01587-z doi (DE-627)SPR04773566X (SPR)s00445-022-01587-z-e DE-627 ger DE-627 rakwb eng Li, Yongquan verfasserin (orcid)0000-0002-4491-0618 aut Quaternary monogenetic volcanoes in southern China: eruption styles and controlling factors 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © International Association of Volcanology & Chemistry of the Earth's Interior 2022 Abstract The Hainan Island-Leizhou Peninsula-Beibu Gulf volcanic field (HLBVF) in southern China (covering an area of over 7000 $ km^{2} $) contains at least 50 cinder cones and 12 maar volcanoes. It is one of a few barely studied volcanic fields of Quaternary age in China. The eruption styles, and controlling factors that led to the formation of this volcanic field, are thus not yet clear. This study provides a first investigation of the general geology of the HLBVF volcanoes as well as preliminary discussion of the controlling factors affecting the eruption styles. Early Pleistocene (> 1 Ma) and/or earlier (Pliocene) volcanic activity mainly occurred in the form of high-flux magmatic eruptions that formed a large amount of thick lava units and/or cinder cones, which have since experienced intense erosion. The late early Pleistocene to late Pleistocene (~ 1.08–0.03 Ma) phreatomagmatism is represented by maar volcanoes and shows that the initial eruptions were commonly phreatomagmatic events but had increasingly magmatic components in later periods, which reflects sustained, but lower magma fluxes than in the early Pleistocene. The Holocene magmatic eruptions (< 10 ka) primarily formed agglutinate, bomb, and lapilli units, as well as lava flows. These deposits were emplaced mainly by pyroclastic fallout from Hawaiian-style eruptions. This work indicates that eruption styles between magmatic and phreatomagmatic eruptions in the HLBVF were not directly related to fluctuations in annual precipitation and magma compositions. Pre-existing NW-trending faults likely controlled the vent locations, and water fed along fault zones might have supported sustained phreatomagmatism, which formed the large maar volcanoes. The fluctuation of magma fluxes, and water supply linked to long-term tropical climate changes, coupled with regional faults, were likely the three main factors that controlled eruption styles in the HLBVF. Monogenetic volcanoes (dpeaa)DE-He213 Eruption styles (dpeaa)DE-He213 Controlling factors (dpeaa)DE-He213 Magma flux (dpeaa)DE-He213 Tropical climate (dpeaa)DE-He213 Enthalten in Bulletin of volcanology Berlin : Springer, 1924 84(2022), 8 vom: 01. Aug. (DE-627)253390397 (DE-600)1458483-9 1432-0819 nnns volume:84 year:2022 number:8 day:01 month:08 https://dx.doi.org/10.1007/s00445-022-01587-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 84 2022 8 01 08 |
| spelling |
10.1007/s00445-022-01587-z doi (DE-627)SPR04773566X (SPR)s00445-022-01587-z-e DE-627 ger DE-627 rakwb eng Li, Yongquan verfasserin (orcid)0000-0002-4491-0618 aut Quaternary monogenetic volcanoes in southern China: eruption styles and controlling factors 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © International Association of Volcanology & Chemistry of the Earth's Interior 2022 Abstract The Hainan Island-Leizhou Peninsula-Beibu Gulf volcanic field (HLBVF) in southern China (covering an area of over 7000 $ km^{2} $) contains at least 50 cinder cones and 12 maar volcanoes. It is one of a few barely studied volcanic fields of Quaternary age in China. The eruption styles, and controlling factors that led to the formation of this volcanic field, are thus not yet clear. This study provides a first investigation of the general geology of the HLBVF volcanoes as well as preliminary discussion of the controlling factors affecting the eruption styles. Early Pleistocene (> 1 Ma) and/or earlier (Pliocene) volcanic activity mainly occurred in the form of high-flux magmatic eruptions that formed a large amount of thick lava units and/or cinder cones, which have since experienced intense erosion. The late early Pleistocene to late Pleistocene (~ 1.08–0.03 Ma) phreatomagmatism is represented by maar volcanoes and shows that the initial eruptions were commonly phreatomagmatic events but had increasingly magmatic components in later periods, which reflects sustained, but lower magma fluxes than in the early Pleistocene. The Holocene magmatic eruptions (< 10 ka) primarily formed agglutinate, bomb, and lapilli units, as well as lava flows. These deposits were emplaced mainly by pyroclastic fallout from Hawaiian-style eruptions. This work indicates that eruption styles between magmatic and phreatomagmatic eruptions in the HLBVF were not directly related to fluctuations in annual precipitation and magma compositions. Pre-existing NW-trending faults likely controlled the vent locations, and water fed along fault zones might have supported sustained phreatomagmatism, which formed the large maar volcanoes. The fluctuation of magma fluxes, and water supply linked to long-term tropical climate changes, coupled with regional faults, were likely the three main factors that controlled eruption styles in the HLBVF. Monogenetic volcanoes (dpeaa)DE-He213 Eruption styles (dpeaa)DE-He213 Controlling factors (dpeaa)DE-He213 Magma flux (dpeaa)DE-He213 Tropical climate (dpeaa)DE-He213 Enthalten in Bulletin of volcanology Berlin : Springer, 1924 84(2022), 8 vom: 01. Aug. (DE-627)253390397 (DE-600)1458483-9 1432-0819 nnns volume:84 year:2022 number:8 day:01 month:08 https://dx.doi.org/10.1007/s00445-022-01587-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 84 2022 8 01 08 |
| allfields_unstemmed |
10.1007/s00445-022-01587-z doi (DE-627)SPR04773566X (SPR)s00445-022-01587-z-e DE-627 ger DE-627 rakwb eng Li, Yongquan verfasserin (orcid)0000-0002-4491-0618 aut Quaternary monogenetic volcanoes in southern China: eruption styles and controlling factors 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © International Association of Volcanology & Chemistry of the Earth's Interior 2022 Abstract The Hainan Island-Leizhou Peninsula-Beibu Gulf volcanic field (HLBVF) in southern China (covering an area of over 7000 $ km^{2} $) contains at least 50 cinder cones and 12 maar volcanoes. It is one of a few barely studied volcanic fields of Quaternary age in China. The eruption styles, and controlling factors that led to the formation of this volcanic field, are thus not yet clear. This study provides a first investigation of the general geology of the HLBVF volcanoes as well as preliminary discussion of the controlling factors affecting the eruption styles. Early Pleistocene (> 1 Ma) and/or earlier (Pliocene) volcanic activity mainly occurred in the form of high-flux magmatic eruptions that formed a large amount of thick lava units and/or cinder cones, which have since experienced intense erosion. The late early Pleistocene to late Pleistocene (~ 1.08–0.03 Ma) phreatomagmatism is represented by maar volcanoes and shows that the initial eruptions were commonly phreatomagmatic events but had increasingly magmatic components in later periods, which reflects sustained, but lower magma fluxes than in the early Pleistocene. The Holocene magmatic eruptions (< 10 ka) primarily formed agglutinate, bomb, and lapilli units, as well as lava flows. These deposits were emplaced mainly by pyroclastic fallout from Hawaiian-style eruptions. This work indicates that eruption styles between magmatic and phreatomagmatic eruptions in the HLBVF were not directly related to fluctuations in annual precipitation and magma compositions. Pre-existing NW-trending faults likely controlled the vent locations, and water fed along fault zones might have supported sustained phreatomagmatism, which formed the large maar volcanoes. The fluctuation of magma fluxes, and water supply linked to long-term tropical climate changes, coupled with regional faults, were likely the three main factors that controlled eruption styles in the HLBVF. Monogenetic volcanoes (dpeaa)DE-He213 Eruption styles (dpeaa)DE-He213 Controlling factors (dpeaa)DE-He213 Magma flux (dpeaa)DE-He213 Tropical climate (dpeaa)DE-He213 Enthalten in Bulletin of volcanology Berlin : Springer, 1924 84(2022), 8 vom: 01. Aug. (DE-627)253390397 (DE-600)1458483-9 1432-0819 nnns volume:84 year:2022 number:8 day:01 month:08 https://dx.doi.org/10.1007/s00445-022-01587-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 84 2022 8 01 08 |
| allfieldsGer |
10.1007/s00445-022-01587-z doi (DE-627)SPR04773566X (SPR)s00445-022-01587-z-e DE-627 ger DE-627 rakwb eng Li, Yongquan verfasserin (orcid)0000-0002-4491-0618 aut Quaternary monogenetic volcanoes in southern China: eruption styles and controlling factors 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © International Association of Volcanology & Chemistry of the Earth's Interior 2022 Abstract The Hainan Island-Leizhou Peninsula-Beibu Gulf volcanic field (HLBVF) in southern China (covering an area of over 7000 $ km^{2} $) contains at least 50 cinder cones and 12 maar volcanoes. It is one of a few barely studied volcanic fields of Quaternary age in China. The eruption styles, and controlling factors that led to the formation of this volcanic field, are thus not yet clear. This study provides a first investigation of the general geology of the HLBVF volcanoes as well as preliminary discussion of the controlling factors affecting the eruption styles. Early Pleistocene (> 1 Ma) and/or earlier (Pliocene) volcanic activity mainly occurred in the form of high-flux magmatic eruptions that formed a large amount of thick lava units and/or cinder cones, which have since experienced intense erosion. The late early Pleistocene to late Pleistocene (~ 1.08–0.03 Ma) phreatomagmatism is represented by maar volcanoes and shows that the initial eruptions were commonly phreatomagmatic events but had increasingly magmatic components in later periods, which reflects sustained, but lower magma fluxes than in the early Pleistocene. The Holocene magmatic eruptions (< 10 ka) primarily formed agglutinate, bomb, and lapilli units, as well as lava flows. These deposits were emplaced mainly by pyroclastic fallout from Hawaiian-style eruptions. This work indicates that eruption styles between magmatic and phreatomagmatic eruptions in the HLBVF were not directly related to fluctuations in annual precipitation and magma compositions. Pre-existing NW-trending faults likely controlled the vent locations, and water fed along fault zones might have supported sustained phreatomagmatism, which formed the large maar volcanoes. The fluctuation of magma fluxes, and water supply linked to long-term tropical climate changes, coupled with regional faults, were likely the three main factors that controlled eruption styles in the HLBVF. Monogenetic volcanoes (dpeaa)DE-He213 Eruption styles (dpeaa)DE-He213 Controlling factors (dpeaa)DE-He213 Magma flux (dpeaa)DE-He213 Tropical climate (dpeaa)DE-He213 Enthalten in Bulletin of volcanology Berlin : Springer, 1924 84(2022), 8 vom: 01. Aug. (DE-627)253390397 (DE-600)1458483-9 1432-0819 nnns volume:84 year:2022 number:8 day:01 month:08 https://dx.doi.org/10.1007/s00445-022-01587-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 84 2022 8 01 08 |
| allfieldsSound |
10.1007/s00445-022-01587-z doi (DE-627)SPR04773566X (SPR)s00445-022-01587-z-e DE-627 ger DE-627 rakwb eng Li, Yongquan verfasserin (orcid)0000-0002-4491-0618 aut Quaternary monogenetic volcanoes in southern China: eruption styles and controlling factors 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © International Association of Volcanology & Chemistry of the Earth's Interior 2022 Abstract The Hainan Island-Leizhou Peninsula-Beibu Gulf volcanic field (HLBVF) in southern China (covering an area of over 7000 $ km^{2} $) contains at least 50 cinder cones and 12 maar volcanoes. It is one of a few barely studied volcanic fields of Quaternary age in China. The eruption styles, and controlling factors that led to the formation of this volcanic field, are thus not yet clear. This study provides a first investigation of the general geology of the HLBVF volcanoes as well as preliminary discussion of the controlling factors affecting the eruption styles. Early Pleistocene (> 1 Ma) and/or earlier (Pliocene) volcanic activity mainly occurred in the form of high-flux magmatic eruptions that formed a large amount of thick lava units and/or cinder cones, which have since experienced intense erosion. The late early Pleistocene to late Pleistocene (~ 1.08–0.03 Ma) phreatomagmatism is represented by maar volcanoes and shows that the initial eruptions were commonly phreatomagmatic events but had increasingly magmatic components in later periods, which reflects sustained, but lower magma fluxes than in the early Pleistocene. The Holocene magmatic eruptions (< 10 ka) primarily formed agglutinate, bomb, and lapilli units, as well as lava flows. These deposits were emplaced mainly by pyroclastic fallout from Hawaiian-style eruptions. This work indicates that eruption styles between magmatic and phreatomagmatic eruptions in the HLBVF were not directly related to fluctuations in annual precipitation and magma compositions. Pre-existing NW-trending faults likely controlled the vent locations, and water fed along fault zones might have supported sustained phreatomagmatism, which formed the large maar volcanoes. The fluctuation of magma fluxes, and water supply linked to long-term tropical climate changes, coupled with regional faults, were likely the three main factors that controlled eruption styles in the HLBVF. Monogenetic volcanoes (dpeaa)DE-He213 Eruption styles (dpeaa)DE-He213 Controlling factors (dpeaa)DE-He213 Magma flux (dpeaa)DE-He213 Tropical climate (dpeaa)DE-He213 Enthalten in Bulletin of volcanology Berlin : Springer, 1924 84(2022), 8 vom: 01. Aug. (DE-627)253390397 (DE-600)1458483-9 1432-0819 nnns volume:84 year:2022 number:8 day:01 month:08 https://dx.doi.org/10.1007/s00445-022-01587-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 84 2022 8 01 08 |
| language |
English |
| source |
Enthalten in Bulletin of volcanology 84(2022), 8 vom: 01. Aug. volume:84 year:2022 number:8 day:01 month:08 |
| sourceStr |
Enthalten in Bulletin of volcanology 84(2022), 8 vom: 01. Aug. volume:84 year:2022 number:8 day:01 month:08 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
Monogenetic volcanoes Eruption styles Controlling factors Magma flux Tropical climate |
| isfreeaccess_bool |
false |
| container_title |
Bulletin of volcanology |
| authorswithroles_txt_mv |
Li, Yongquan @@aut@@ |
| publishDateDaySort_date |
2022-08-01T00:00:00Z |
| hierarchy_top_id |
253390397 |
| id |
SPR04773566X |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR04773566X</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230509105034.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">220802s2022 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s00445-022-01587-z</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR04773566X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s00445-022-01587-z-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Li, Yongquan</subfield><subfield code="e">verfasserin</subfield><subfield code="0">(orcid)0000-0002-4491-0618</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Quaternary monogenetic volcanoes in southern China: eruption styles and controlling factors</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© International Association of Volcanology & Chemistry of the Earth's Interior 2022</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The Hainan Island-Leizhou Peninsula-Beibu Gulf volcanic field (HLBVF) in southern China (covering an area of over 7000 $ km^{2} $) contains at least 50 cinder cones and 12 maar volcanoes. It is one of a few barely studied volcanic fields of Quaternary age in China. The eruption styles, and controlling factors that led to the formation of this volcanic field, are thus not yet clear. This study provides a first investigation of the general geology of the HLBVF volcanoes as well as preliminary discussion of the controlling factors affecting the eruption styles. Early Pleistocene (> 1 Ma) and/or earlier (Pliocene) volcanic activity mainly occurred in the form of high-flux magmatic eruptions that formed a large amount of thick lava units and/or cinder cones, which have since experienced intense erosion. The late early Pleistocene to late Pleistocene (~ 1.08–0.03 Ma) phreatomagmatism is represented by maar volcanoes and shows that the initial eruptions were commonly phreatomagmatic events but had increasingly magmatic components in later periods, which reflects sustained, but lower magma fluxes than in the early Pleistocene. The Holocene magmatic eruptions (< 10 ka) primarily formed agglutinate, bomb, and lapilli units, as well as lava flows. These deposits were emplaced mainly by pyroclastic fallout from Hawaiian-style eruptions. This work indicates that eruption styles between magmatic and phreatomagmatic eruptions in the HLBVF were not directly related to fluctuations in annual precipitation and magma compositions. Pre-existing NW-trending faults likely controlled the vent locations, and water fed along fault zones might have supported sustained phreatomagmatism, which formed the large maar volcanoes. The fluctuation of magma fluxes, and water supply linked to long-term tropical climate changes, coupled with regional faults, were likely the three main factors that controlled eruption styles in the HLBVF.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Monogenetic volcanoes</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Eruption styles</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Controlling factors</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Magma flux</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Tropical climate</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Bulletin of volcanology</subfield><subfield code="d">Berlin : Springer, 1924</subfield><subfield code="g">84(2022), 8 vom: 01. Aug.</subfield><subfield code="w">(DE-627)253390397</subfield><subfield code="w">(DE-600)1458483-9</subfield><subfield code="x">1432-0819</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:84</subfield><subfield code="g">year:2022</subfield><subfield code="g">number:8</subfield><subfield code="g">day:01</subfield><subfield code="g">month:08</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://dx.doi.org/10.1007/s00445-022-01587-z</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_SPRINGER</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_32</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_39</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_74</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_90</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_100</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_120</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_138</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_150</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_152</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_170</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_171</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_187</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_213</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_224</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_230</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_250</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_267</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_281</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_381</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_636</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_702</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2001</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2003</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2004</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2005</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2006</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2007</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2008</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2009</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2010</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2011</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2015</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2018</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2020</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2021</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2025</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2026</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2031</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2034</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2038</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2039</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2044</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2048</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2049</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2050</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2055</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2056</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2057</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2059</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2061</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2064</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2065</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2068</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2088</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2093</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2106</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2107</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2108</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2111</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2113</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2118</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2122</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2129</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2143</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2144</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2147</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2148</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2153</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2188</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2190</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2232</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2336</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2446</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2470</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2472</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2507</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2522</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2548</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4035</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4242</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4246</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4249</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4251</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4322</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4326</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4328</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4333</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4334</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4335</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4336</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4338</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4393</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4700</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">84</subfield><subfield code="j">2022</subfield><subfield code="e">8</subfield><subfield code="b">01</subfield><subfield code="c">08</subfield></datafield></record></collection>
|
| author |
Li, Yongquan |
| spellingShingle |
Li, Yongquan misc Monogenetic volcanoes misc Eruption styles misc Controlling factors misc Magma flux misc Tropical climate Quaternary monogenetic volcanoes in southern China: eruption styles and controlling factors |
| authorStr |
Li, Yongquan |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)253390397 |
| format |
electronic Article |
| delete_txt_mv |
keep |
| author_role |
aut |
| collection |
springer |
| remote_str |
true |
| illustrated |
Not Illustrated |
| issn |
1432-0819 |
| topic_title |
Quaternary monogenetic volcanoes in southern China: eruption styles and controlling factors Monogenetic volcanoes (dpeaa)DE-He213 Eruption styles (dpeaa)DE-He213 Controlling factors (dpeaa)DE-He213 Magma flux (dpeaa)DE-He213 Tropical climate (dpeaa)DE-He213 |
| topic |
misc Monogenetic volcanoes misc Eruption styles misc Controlling factors misc Magma flux misc Tropical climate |
| topic_unstemmed |
misc Monogenetic volcanoes misc Eruption styles misc Controlling factors misc Magma flux misc Tropical climate |
| topic_browse |
misc Monogenetic volcanoes misc Eruption styles misc Controlling factors misc Magma flux misc Tropical climate |
| format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
cr |
| hierarchy_parent_title |
Bulletin of volcanology |
| hierarchy_parent_id |
253390397 |
| hierarchy_top_title |
Bulletin of volcanology |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)253390397 (DE-600)1458483-9 |
| title |
Quaternary monogenetic volcanoes in southern China: eruption styles and controlling factors |
| ctrlnum |
(DE-627)SPR04773566X (SPR)s00445-022-01587-z-e |
| title_full |
Quaternary monogenetic volcanoes in southern China: eruption styles and controlling factors |
| author_sort |
Li, Yongquan |
| journal |
Bulletin of volcanology |
| journalStr |
Bulletin of volcanology |
| lang_code |
eng |
| isOA_bool |
false |
| recordtype |
marc |
| publishDateSort |
2022 |
| contenttype_str_mv |
txt |
| author_browse |
Li, Yongquan |
| container_volume |
84 |
| format_se |
Elektronische Aufsätze |
| author-letter |
Li, Yongquan |
| doi_str_mv |
10.1007/s00445-022-01587-z |
| normlink |
(ORCID)0000-0002-4491-0618 |
| normlink_prefix_str_mv |
(orcid)0000-0002-4491-0618 |
| title_sort |
quaternary monogenetic volcanoes in southern china: eruption styles and controlling factors |
| title_auth |
Quaternary monogenetic volcanoes in southern China: eruption styles and controlling factors |
| abstract |
Abstract The Hainan Island-Leizhou Peninsula-Beibu Gulf volcanic field (HLBVF) in southern China (covering an area of over 7000 $ km^{2} $) contains at least 50 cinder cones and 12 maar volcanoes. It is one of a few barely studied volcanic fields of Quaternary age in China. The eruption styles, and controlling factors that led to the formation of this volcanic field, are thus not yet clear. This study provides a first investigation of the general geology of the HLBVF volcanoes as well as preliminary discussion of the controlling factors affecting the eruption styles. Early Pleistocene (> 1 Ma) and/or earlier (Pliocene) volcanic activity mainly occurred in the form of high-flux magmatic eruptions that formed a large amount of thick lava units and/or cinder cones, which have since experienced intense erosion. The late early Pleistocene to late Pleistocene (~ 1.08–0.03 Ma) phreatomagmatism is represented by maar volcanoes and shows that the initial eruptions were commonly phreatomagmatic events but had increasingly magmatic components in later periods, which reflects sustained, but lower magma fluxes than in the early Pleistocene. The Holocene magmatic eruptions (< 10 ka) primarily formed agglutinate, bomb, and lapilli units, as well as lava flows. These deposits were emplaced mainly by pyroclastic fallout from Hawaiian-style eruptions. This work indicates that eruption styles between magmatic and phreatomagmatic eruptions in the HLBVF were not directly related to fluctuations in annual precipitation and magma compositions. Pre-existing NW-trending faults likely controlled the vent locations, and water fed along fault zones might have supported sustained phreatomagmatism, which formed the large maar volcanoes. The fluctuation of magma fluxes, and water supply linked to long-term tropical climate changes, coupled with regional faults, were likely the three main factors that controlled eruption styles in the HLBVF. © International Association of Volcanology & Chemistry of the Earth's Interior 2022 |
| abstractGer |
Abstract The Hainan Island-Leizhou Peninsula-Beibu Gulf volcanic field (HLBVF) in southern China (covering an area of over 7000 $ km^{2} $) contains at least 50 cinder cones and 12 maar volcanoes. It is one of a few barely studied volcanic fields of Quaternary age in China. The eruption styles, and controlling factors that led to the formation of this volcanic field, are thus not yet clear. This study provides a first investigation of the general geology of the HLBVF volcanoes as well as preliminary discussion of the controlling factors affecting the eruption styles. Early Pleistocene (> 1 Ma) and/or earlier (Pliocene) volcanic activity mainly occurred in the form of high-flux magmatic eruptions that formed a large amount of thick lava units and/or cinder cones, which have since experienced intense erosion. The late early Pleistocene to late Pleistocene (~ 1.08–0.03 Ma) phreatomagmatism is represented by maar volcanoes and shows that the initial eruptions were commonly phreatomagmatic events but had increasingly magmatic components in later periods, which reflects sustained, but lower magma fluxes than in the early Pleistocene. The Holocene magmatic eruptions (< 10 ka) primarily formed agglutinate, bomb, and lapilli units, as well as lava flows. These deposits were emplaced mainly by pyroclastic fallout from Hawaiian-style eruptions. This work indicates that eruption styles between magmatic and phreatomagmatic eruptions in the HLBVF were not directly related to fluctuations in annual precipitation and magma compositions. Pre-existing NW-trending faults likely controlled the vent locations, and water fed along fault zones might have supported sustained phreatomagmatism, which formed the large maar volcanoes. The fluctuation of magma fluxes, and water supply linked to long-term tropical climate changes, coupled with regional faults, were likely the three main factors that controlled eruption styles in the HLBVF. © International Association of Volcanology & Chemistry of the Earth's Interior 2022 |
| abstract_unstemmed |
Abstract The Hainan Island-Leizhou Peninsula-Beibu Gulf volcanic field (HLBVF) in southern China (covering an area of over 7000 $ km^{2} $) contains at least 50 cinder cones and 12 maar volcanoes. It is one of a few barely studied volcanic fields of Quaternary age in China. The eruption styles, and controlling factors that led to the formation of this volcanic field, are thus not yet clear. This study provides a first investigation of the general geology of the HLBVF volcanoes as well as preliminary discussion of the controlling factors affecting the eruption styles. Early Pleistocene (> 1 Ma) and/or earlier (Pliocene) volcanic activity mainly occurred in the form of high-flux magmatic eruptions that formed a large amount of thick lava units and/or cinder cones, which have since experienced intense erosion. The late early Pleistocene to late Pleistocene (~ 1.08–0.03 Ma) phreatomagmatism is represented by maar volcanoes and shows that the initial eruptions were commonly phreatomagmatic events but had increasingly magmatic components in later periods, which reflects sustained, but lower magma fluxes than in the early Pleistocene. The Holocene magmatic eruptions (< 10 ka) primarily formed agglutinate, bomb, and lapilli units, as well as lava flows. These deposits were emplaced mainly by pyroclastic fallout from Hawaiian-style eruptions. This work indicates that eruption styles between magmatic and phreatomagmatic eruptions in the HLBVF were not directly related to fluctuations in annual precipitation and magma compositions. Pre-existing NW-trending faults likely controlled the vent locations, and water fed along fault zones might have supported sustained phreatomagmatism, which formed the large maar volcanoes. The fluctuation of magma fluxes, and water supply linked to long-term tropical climate changes, coupled with regional faults, were likely the three main factors that controlled eruption styles in the HLBVF. © International Association of Volcanology & Chemistry of the Earth's Interior 2022 |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 |
| container_issue |
8 |
| title_short |
Quaternary monogenetic volcanoes in southern China: eruption styles and controlling factors |
| url |
https://dx.doi.org/10.1007/s00445-022-01587-z |
| remote_bool |
true |
| ppnlink |
253390397 |
| mediatype_str_mv |
c |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| doi_str |
10.1007/s00445-022-01587-z |
| up_date |
2024-07-03T14:38:54.949Z |
| _version_ |
1803569106729828352 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR04773566X</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230509105034.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">220802s2022 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s00445-022-01587-z</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR04773566X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s00445-022-01587-z-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Li, Yongquan</subfield><subfield code="e">verfasserin</subfield><subfield code="0">(orcid)0000-0002-4491-0618</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Quaternary monogenetic volcanoes in southern China: eruption styles and controlling factors</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© International Association of Volcanology & Chemistry of the Earth's Interior 2022</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The Hainan Island-Leizhou Peninsula-Beibu Gulf volcanic field (HLBVF) in southern China (covering an area of over 7000 $ km^{2} $) contains at least 50 cinder cones and 12 maar volcanoes. It is one of a few barely studied volcanic fields of Quaternary age in China. The eruption styles, and controlling factors that led to the formation of this volcanic field, are thus not yet clear. This study provides a first investigation of the general geology of the HLBVF volcanoes as well as preliminary discussion of the controlling factors affecting the eruption styles. Early Pleistocene (> 1 Ma) and/or earlier (Pliocene) volcanic activity mainly occurred in the form of high-flux magmatic eruptions that formed a large amount of thick lava units and/or cinder cones, which have since experienced intense erosion. The late early Pleistocene to late Pleistocene (~ 1.08–0.03 Ma) phreatomagmatism is represented by maar volcanoes and shows that the initial eruptions were commonly phreatomagmatic events but had increasingly magmatic components in later periods, which reflects sustained, but lower magma fluxes than in the early Pleistocene. The Holocene magmatic eruptions (< 10 ka) primarily formed agglutinate, bomb, and lapilli units, as well as lava flows. These deposits were emplaced mainly by pyroclastic fallout from Hawaiian-style eruptions. This work indicates that eruption styles between magmatic and phreatomagmatic eruptions in the HLBVF were not directly related to fluctuations in annual precipitation and magma compositions. Pre-existing NW-trending faults likely controlled the vent locations, and water fed along fault zones might have supported sustained phreatomagmatism, which formed the large maar volcanoes. The fluctuation of magma fluxes, and water supply linked to long-term tropical climate changes, coupled with regional faults, were likely the three main factors that controlled eruption styles in the HLBVF.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Monogenetic volcanoes</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Eruption styles</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Controlling factors</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Magma flux</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Tropical climate</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Bulletin of volcanology</subfield><subfield code="d">Berlin : Springer, 1924</subfield><subfield code="g">84(2022), 8 vom: 01. Aug.</subfield><subfield code="w">(DE-627)253390397</subfield><subfield code="w">(DE-600)1458483-9</subfield><subfield code="x">1432-0819</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:84</subfield><subfield code="g">year:2022</subfield><subfield code="g">number:8</subfield><subfield code="g">day:01</subfield><subfield code="g">month:08</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://dx.doi.org/10.1007/s00445-022-01587-z</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_SPRINGER</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_32</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_39</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_74</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_90</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_100</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_120</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_138</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_150</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_152</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_170</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_171</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_187</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_213</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_224</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_230</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_250</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_267</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_281</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_381</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_636</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_702</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2001</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2003</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2004</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2005</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2006</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2007</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2008</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2009</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2010</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2011</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2015</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2018</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2020</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2021</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2025</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2026</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2031</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2034</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2038</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2039</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2044</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2048</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2049</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2050</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2055</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2056</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2057</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2059</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2061</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2064</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2065</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2068</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2088</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2093</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2106</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2107</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2108</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2111</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2113</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2118</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2122</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2129</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2143</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2144</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2147</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2148</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2153</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2188</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2190</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2232</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2336</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2446</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2470</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2472</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2507</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2522</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2548</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4035</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4242</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4246</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4249</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4251</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4322</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4326</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4328</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4333</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4334</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4335</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4336</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4338</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4393</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4700</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">84</subfield><subfield code="j">2022</subfield><subfield code="e">8</subfield><subfield code="b">01</subfield><subfield code="c">08</subfield></datafield></record></collection>
|
| score |
7.401102 |