Late Paleozoic-Early Mesozoic tectonic evolution in the east margin of the Jiamusi massif, eastern northeastern China
Abstract The Jiamusi massif is a major tectonic unit in the eastern part of NE China and composed chiefly of the Early Paleozoic (about 500 Ma) metamorphosed crystalline basement containing Precambrian, even Archean crust and three suites of unmetamorphosed continental marginal sedimentary formation...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Zhang, Xing Zhou [verfasserIn] Guo, Ye [verfasserIn] Zhou, Jian Bo [verfasserIn] Zeng, Zhen [verfasserIn] Pu, Jian Bin [verfasserIn] Fu, Qiu Lin [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Russian journal of Pacific geology - Moscow : MAIK Nauka/Interperiodica Publ., 2007, 9(2015), 1 vom: Jan., Seite 1-10 |
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| Übergeordnetes Werk: |
volume:9 ; year:2015 ; number:1 ; month:01 ; pages:1-10 |
| Links: |
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| DOI / URN: |
10.1134/S181971401501008X |
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| Katalog-ID: |
SPR022017488 |
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| 245 | 1 | 0 | |a Late Paleozoic-Early Mesozoic tectonic evolution in the east margin of the Jiamusi massif, eastern northeastern China |
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| 520 | |a Abstract The Jiamusi massif is a major tectonic unit in the eastern part of NE China and composed chiefly of the Early Paleozoic (about 500 Ma) metamorphosed crystalline basement containing Precambrian, even Archean crust and three suites of unmetamorphosed continental marginal sedimentary formations of the Devonian-Lower Carboniferous, the Late Carboniferous-Permian and the Late Triassic, which are similar to those in the Bureya and Khanka massifs in Russia. In the Devonian-Lower Carboniferous, the microcontinent consisting of the Jiamusi and Songnen massifs in China and the Bureya and Khanka massifs in Russia evolved independently, the eastern part of which was a passive continental margin, where a suite of the marine sedimentary-volcanic formation is overlain unconformably on the crystalline basement. The regional stratigraphic break in the middle Carboniferous in the whole northeastern China was related to the collision of the microcontinent with the Argun-Hinggan microcontinent in the west, indicating the formation of a new amalgamated continent (Heilongjiang plate). Therefore, the Late Carboniferous-Permian volcanic-sedimentary formation is the first unitary cover on the Heilongjiang plate. The Late Carboniferous-Permian and the Late Triassic sedimentary formations in the eastern part of the Jiamusi-Bureya-Khanka microcontinent represent the evolutional features of the eastern continental margin of the Heilongjiang plate. Summarily, the eastern margin of the Heilongjiang plate mainly suffered the following evolution stages from the Late Carboniferous to the Late Triassic: (1) the transform or passive continental margin in the Late Carboniferous, characterized by terrestrial facies clastic rocks with interbeded recoverable coal layers; (2) the active continental margin in the Permian marked by the magmatic arc composed mainly of intermediate-acid volcanics and granites; (3) the transform margin in the Early-Middle Triassic indicated by the simultaneous stratigraphic break, and (4) the passive continental margin in the Late Triassic characterized by the marine-terrigenous facies sedimentary formation. | ||
| 650 | 4 | |a Jiamusi massif |7 (dpeaa)DE-He213 | |
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| 650 | 4 | |a continental margin |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Northeastern China |7 (dpeaa)DE-He213 | |
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| 700 | 1 | |a Pu, Jian Bin |e verfasserin |4 aut | |
| 700 | 1 | |a Fu, Qiu Lin |e verfasserin |4 aut | |
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10.1134/S181971401501008X doi (DE-627)SPR022017488 (SPR)S181971401501008X-e DE-627 ger DE-627 rakwb eng 550 ASE Zhang, Xing Zhou verfasserin aut Late Paleozoic-Early Mesozoic tectonic evolution in the east margin of the Jiamusi massif, eastern northeastern China 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Jiamusi massif is a major tectonic unit in the eastern part of NE China and composed chiefly of the Early Paleozoic (about 500 Ma) metamorphosed crystalline basement containing Precambrian, even Archean crust and three suites of unmetamorphosed continental marginal sedimentary formations of the Devonian-Lower Carboniferous, the Late Carboniferous-Permian and the Late Triassic, which are similar to those in the Bureya and Khanka massifs in Russia. In the Devonian-Lower Carboniferous, the microcontinent consisting of the Jiamusi and Songnen massifs in China and the Bureya and Khanka massifs in Russia evolved independently, the eastern part of which was a passive continental margin, where a suite of the marine sedimentary-volcanic formation is overlain unconformably on the crystalline basement. The regional stratigraphic break in the middle Carboniferous in the whole northeastern China was related to the collision of the microcontinent with the Argun-Hinggan microcontinent in the west, indicating the formation of a new amalgamated continent (Heilongjiang plate). Therefore, the Late Carboniferous-Permian volcanic-sedimentary formation is the first unitary cover on the Heilongjiang plate. The Late Carboniferous-Permian and the Late Triassic sedimentary formations in the eastern part of the Jiamusi-Bureya-Khanka microcontinent represent the evolutional features of the eastern continental margin of the Heilongjiang plate. Summarily, the eastern margin of the Heilongjiang plate mainly suffered the following evolution stages from the Late Carboniferous to the Late Triassic: (1) the transform or passive continental margin in the Late Carboniferous, characterized by terrestrial facies clastic rocks with interbeded recoverable coal layers; (2) the active continental margin in the Permian marked by the magmatic arc composed mainly of intermediate-acid volcanics and granites; (3) the transform margin in the Early-Middle Triassic indicated by the simultaneous stratigraphic break, and (4) the passive continental margin in the Late Triassic characterized by the marine-terrigenous facies sedimentary formation. Jiamusi massif (dpeaa)DE-He213 Heilongjiang plate (dpeaa)DE-He213 continental margin (dpeaa)DE-He213 Northeastern China (dpeaa)DE-He213 Guo, Ye verfasserin aut Zhou, Jian Bo verfasserin aut Zeng, Zhen verfasserin aut Pu, Jian Bin verfasserin aut Fu, Qiu Lin verfasserin aut Enthalten in Russian journal of Pacific geology Moscow : MAIK Nauka/Interperiodica Publ., 2007 9(2015), 1 vom: Jan., Seite 1-10 (DE-627)54766284X (DE-600)2391890-1 1819-7159 nnns volume:9 year:2015 number:1 month:01 pages:1-10 https://dx.doi.org/10.1134/S181971401501008X 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_65 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_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 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_4046 GBV_ILN_4112 GBV_ILN_4125 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 9 2015 1 01 1-10 |
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10.1134/S181971401501008X doi (DE-627)SPR022017488 (SPR)S181971401501008X-e DE-627 ger DE-627 rakwb eng 550 ASE Zhang, Xing Zhou verfasserin aut Late Paleozoic-Early Mesozoic tectonic evolution in the east margin of the Jiamusi massif, eastern northeastern China 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Jiamusi massif is a major tectonic unit in the eastern part of NE China and composed chiefly of the Early Paleozoic (about 500 Ma) metamorphosed crystalline basement containing Precambrian, even Archean crust and three suites of unmetamorphosed continental marginal sedimentary formations of the Devonian-Lower Carboniferous, the Late Carboniferous-Permian and the Late Triassic, which are similar to those in the Bureya and Khanka massifs in Russia. In the Devonian-Lower Carboniferous, the microcontinent consisting of the Jiamusi and Songnen massifs in China and the Bureya and Khanka massifs in Russia evolved independently, the eastern part of which was a passive continental margin, where a suite of the marine sedimentary-volcanic formation is overlain unconformably on the crystalline basement. The regional stratigraphic break in the middle Carboniferous in the whole northeastern China was related to the collision of the microcontinent with the Argun-Hinggan microcontinent in the west, indicating the formation of a new amalgamated continent (Heilongjiang plate). Therefore, the Late Carboniferous-Permian volcanic-sedimentary formation is the first unitary cover on the Heilongjiang plate. The Late Carboniferous-Permian and the Late Triassic sedimentary formations in the eastern part of the Jiamusi-Bureya-Khanka microcontinent represent the evolutional features of the eastern continental margin of the Heilongjiang plate. Summarily, the eastern margin of the Heilongjiang plate mainly suffered the following evolution stages from the Late Carboniferous to the Late Triassic: (1) the transform or passive continental margin in the Late Carboniferous, characterized by terrestrial facies clastic rocks with interbeded recoverable coal layers; (2) the active continental margin in the Permian marked by the magmatic arc composed mainly of intermediate-acid volcanics and granites; (3) the transform margin in the Early-Middle Triassic indicated by the simultaneous stratigraphic break, and (4) the passive continental margin in the Late Triassic characterized by the marine-terrigenous facies sedimentary formation. Jiamusi massif (dpeaa)DE-He213 Heilongjiang plate (dpeaa)DE-He213 continental margin (dpeaa)DE-He213 Northeastern China (dpeaa)DE-He213 Guo, Ye verfasserin aut Zhou, Jian Bo verfasserin aut Zeng, Zhen verfasserin aut Pu, Jian Bin verfasserin aut Fu, Qiu Lin verfasserin aut Enthalten in Russian journal of Pacific geology Moscow : MAIK Nauka/Interperiodica Publ., 2007 9(2015), 1 vom: Jan., Seite 1-10 (DE-627)54766284X (DE-600)2391890-1 1819-7159 nnns volume:9 year:2015 number:1 month:01 pages:1-10 https://dx.doi.org/10.1134/S181971401501008X 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_65 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_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 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_4046 GBV_ILN_4112 GBV_ILN_4125 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 9 2015 1 01 1-10 |
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10.1134/S181971401501008X doi (DE-627)SPR022017488 (SPR)S181971401501008X-e DE-627 ger DE-627 rakwb eng 550 ASE Zhang, Xing Zhou verfasserin aut Late Paleozoic-Early Mesozoic tectonic evolution in the east margin of the Jiamusi massif, eastern northeastern China 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Jiamusi massif is a major tectonic unit in the eastern part of NE China and composed chiefly of the Early Paleozoic (about 500 Ma) metamorphosed crystalline basement containing Precambrian, even Archean crust and three suites of unmetamorphosed continental marginal sedimentary formations of the Devonian-Lower Carboniferous, the Late Carboniferous-Permian and the Late Triassic, which are similar to those in the Bureya and Khanka massifs in Russia. In the Devonian-Lower Carboniferous, the microcontinent consisting of the Jiamusi and Songnen massifs in China and the Bureya and Khanka massifs in Russia evolved independently, the eastern part of which was a passive continental margin, where a suite of the marine sedimentary-volcanic formation is overlain unconformably on the crystalline basement. The regional stratigraphic break in the middle Carboniferous in the whole northeastern China was related to the collision of the microcontinent with the Argun-Hinggan microcontinent in the west, indicating the formation of a new amalgamated continent (Heilongjiang plate). Therefore, the Late Carboniferous-Permian volcanic-sedimentary formation is the first unitary cover on the Heilongjiang plate. The Late Carboniferous-Permian and the Late Triassic sedimentary formations in the eastern part of the Jiamusi-Bureya-Khanka microcontinent represent the evolutional features of the eastern continental margin of the Heilongjiang plate. Summarily, the eastern margin of the Heilongjiang plate mainly suffered the following evolution stages from the Late Carboniferous to the Late Triassic: (1) the transform or passive continental margin in the Late Carboniferous, characterized by terrestrial facies clastic rocks with interbeded recoverable coal layers; (2) the active continental margin in the Permian marked by the magmatic arc composed mainly of intermediate-acid volcanics and granites; (3) the transform margin in the Early-Middle Triassic indicated by the simultaneous stratigraphic break, and (4) the passive continental margin in the Late Triassic characterized by the marine-terrigenous facies sedimentary formation. Jiamusi massif (dpeaa)DE-He213 Heilongjiang plate (dpeaa)DE-He213 continental margin (dpeaa)DE-He213 Northeastern China (dpeaa)DE-He213 Guo, Ye verfasserin aut Zhou, Jian Bo verfasserin aut Zeng, Zhen verfasserin aut Pu, Jian Bin verfasserin aut Fu, Qiu Lin verfasserin aut Enthalten in Russian journal of Pacific geology Moscow : MAIK Nauka/Interperiodica Publ., 2007 9(2015), 1 vom: Jan., Seite 1-10 (DE-627)54766284X (DE-600)2391890-1 1819-7159 nnns volume:9 year:2015 number:1 month:01 pages:1-10 https://dx.doi.org/10.1134/S181971401501008X 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_65 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_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 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_4046 GBV_ILN_4112 GBV_ILN_4125 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 9 2015 1 01 1-10 |
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10.1134/S181971401501008X doi (DE-627)SPR022017488 (SPR)S181971401501008X-e DE-627 ger DE-627 rakwb eng 550 ASE Zhang, Xing Zhou verfasserin aut Late Paleozoic-Early Mesozoic tectonic evolution in the east margin of the Jiamusi massif, eastern northeastern China 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Jiamusi massif is a major tectonic unit in the eastern part of NE China and composed chiefly of the Early Paleozoic (about 500 Ma) metamorphosed crystalline basement containing Precambrian, even Archean crust and three suites of unmetamorphosed continental marginal sedimentary formations of the Devonian-Lower Carboniferous, the Late Carboniferous-Permian and the Late Triassic, which are similar to those in the Bureya and Khanka massifs in Russia. In the Devonian-Lower Carboniferous, the microcontinent consisting of the Jiamusi and Songnen massifs in China and the Bureya and Khanka massifs in Russia evolved independently, the eastern part of which was a passive continental margin, where a suite of the marine sedimentary-volcanic formation is overlain unconformably on the crystalline basement. The regional stratigraphic break in the middle Carboniferous in the whole northeastern China was related to the collision of the microcontinent with the Argun-Hinggan microcontinent in the west, indicating the formation of a new amalgamated continent (Heilongjiang plate). Therefore, the Late Carboniferous-Permian volcanic-sedimentary formation is the first unitary cover on the Heilongjiang plate. The Late Carboniferous-Permian and the Late Triassic sedimentary formations in the eastern part of the Jiamusi-Bureya-Khanka microcontinent represent the evolutional features of the eastern continental margin of the Heilongjiang plate. Summarily, the eastern margin of the Heilongjiang plate mainly suffered the following evolution stages from the Late Carboniferous to the Late Triassic: (1) the transform or passive continental margin in the Late Carboniferous, characterized by terrestrial facies clastic rocks with interbeded recoverable coal layers; (2) the active continental margin in the Permian marked by the magmatic arc composed mainly of intermediate-acid volcanics and granites; (3) the transform margin in the Early-Middle Triassic indicated by the simultaneous stratigraphic break, and (4) the passive continental margin in the Late Triassic characterized by the marine-terrigenous facies sedimentary formation. Jiamusi massif (dpeaa)DE-He213 Heilongjiang plate (dpeaa)DE-He213 continental margin (dpeaa)DE-He213 Northeastern China (dpeaa)DE-He213 Guo, Ye verfasserin aut Zhou, Jian Bo verfasserin aut Zeng, Zhen verfasserin aut Pu, Jian Bin verfasserin aut Fu, Qiu Lin verfasserin aut Enthalten in Russian journal of Pacific geology Moscow : MAIK Nauka/Interperiodica Publ., 2007 9(2015), 1 vom: Jan., Seite 1-10 (DE-627)54766284X (DE-600)2391890-1 1819-7159 nnns volume:9 year:2015 number:1 month:01 pages:1-10 https://dx.doi.org/10.1134/S181971401501008X 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_65 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_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 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_4046 GBV_ILN_4112 GBV_ILN_4125 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 9 2015 1 01 1-10 |
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10.1134/S181971401501008X doi (DE-627)SPR022017488 (SPR)S181971401501008X-e DE-627 ger DE-627 rakwb eng 550 ASE Zhang, Xing Zhou verfasserin aut Late Paleozoic-Early Mesozoic tectonic evolution in the east margin of the Jiamusi massif, eastern northeastern China 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The Jiamusi massif is a major tectonic unit in the eastern part of NE China and composed chiefly of the Early Paleozoic (about 500 Ma) metamorphosed crystalline basement containing Precambrian, even Archean crust and three suites of unmetamorphosed continental marginal sedimentary formations of the Devonian-Lower Carboniferous, the Late Carboniferous-Permian and the Late Triassic, which are similar to those in the Bureya and Khanka massifs in Russia. In the Devonian-Lower Carboniferous, the microcontinent consisting of the Jiamusi and Songnen massifs in China and the Bureya and Khanka massifs in Russia evolved independently, the eastern part of which was a passive continental margin, where a suite of the marine sedimentary-volcanic formation is overlain unconformably on the crystalline basement. The regional stratigraphic break in the middle Carboniferous in the whole northeastern China was related to the collision of the microcontinent with the Argun-Hinggan microcontinent in the west, indicating the formation of a new amalgamated continent (Heilongjiang plate). Therefore, the Late Carboniferous-Permian volcanic-sedimentary formation is the first unitary cover on the Heilongjiang plate. The Late Carboniferous-Permian and the Late Triassic sedimentary formations in the eastern part of the Jiamusi-Bureya-Khanka microcontinent represent the evolutional features of the eastern continental margin of the Heilongjiang plate. Summarily, the eastern margin of the Heilongjiang plate mainly suffered the following evolution stages from the Late Carboniferous to the Late Triassic: (1) the transform or passive continental margin in the Late Carboniferous, characterized by terrestrial facies clastic rocks with interbeded recoverable coal layers; (2) the active continental margin in the Permian marked by the magmatic arc composed mainly of intermediate-acid volcanics and granites; (3) the transform margin in the Early-Middle Triassic indicated by the simultaneous stratigraphic break, and (4) the passive continental margin in the Late Triassic characterized by the marine-terrigenous facies sedimentary formation. Jiamusi massif (dpeaa)DE-He213 Heilongjiang plate (dpeaa)DE-He213 continental margin (dpeaa)DE-He213 Northeastern China (dpeaa)DE-He213 Guo, Ye verfasserin aut Zhou, Jian Bo verfasserin aut Zeng, Zhen verfasserin aut Pu, Jian Bin verfasserin aut Fu, Qiu Lin verfasserin aut Enthalten in Russian journal of Pacific geology Moscow : MAIK Nauka/Interperiodica Publ., 2007 9(2015), 1 vom: Jan., Seite 1-10 (DE-627)54766284X (DE-600)2391890-1 1819-7159 nnns volume:9 year:2015 number:1 month:01 pages:1-10 https://dx.doi.org/10.1134/S181971401501008X 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_65 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_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 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_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_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 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_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 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_4046 GBV_ILN_4112 GBV_ILN_4125 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_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 9 2015 1 01 1-10 |
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Enthalten in Russian journal of Pacific geology 9(2015), 1 vom: Jan., Seite 1-10 volume:9 year:2015 number:1 month:01 pages:1-10 |
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Enthalten in Russian journal of Pacific geology 9(2015), 1 vom: Jan., Seite 1-10 volume:9 year:2015 number:1 month:01 pages:1-10 |
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Jiamusi massif Heilongjiang plate continental margin Northeastern China |
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Russian journal of Pacific geology |
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Zhang, Xing Zhou @@aut@@ Guo, Ye @@aut@@ Zhou, Jian Bo @@aut@@ Zeng, Zhen @@aut@@ Pu, Jian Bin @@aut@@ Fu, Qiu Lin @@aut@@ |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR022017488</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220111090808.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201006s2015 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1134/S181971401501008X</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR022017488</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)S181971401501008X-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="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhang, Xing Zhou</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Late Paleozoic-Early Mesozoic tectonic evolution in the east margin of the Jiamusi massif, eastern northeastern China</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2015</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="520" ind1=" " ind2=" "><subfield code="a">Abstract The Jiamusi massif is a major tectonic unit in the eastern part of NE China and composed chiefly of the Early Paleozoic (about 500 Ma) metamorphosed crystalline basement containing Precambrian, even Archean crust and three suites of unmetamorphosed continental marginal sedimentary formations of the Devonian-Lower Carboniferous, the Late Carboniferous-Permian and the Late Triassic, which are similar to those in the Bureya and Khanka massifs in Russia. In the Devonian-Lower Carboniferous, the microcontinent consisting of the Jiamusi and Songnen massifs in China and the Bureya and Khanka massifs in Russia evolved independently, the eastern part of which was a passive continental margin, where a suite of the marine sedimentary-volcanic formation is overlain unconformably on the crystalline basement. The regional stratigraphic break in the middle Carboniferous in the whole northeastern China was related to the collision of the microcontinent with the Argun-Hinggan microcontinent in the west, indicating the formation of a new amalgamated continent (Heilongjiang plate). Therefore, the Late Carboniferous-Permian volcanic-sedimentary formation is the first unitary cover on the Heilongjiang plate. The Late Carboniferous-Permian and the Late Triassic sedimentary formations in the eastern part of the Jiamusi-Bureya-Khanka microcontinent represent the evolutional features of the eastern continental margin of the Heilongjiang plate. Summarily, the eastern margin of the Heilongjiang plate mainly suffered the following evolution stages from the Late Carboniferous to the Late Triassic: (1) the transform or passive continental margin in the Late Carboniferous, characterized by terrestrial facies clastic rocks with interbeded recoverable coal layers; (2) the active continental margin in the Permian marked by the magmatic arc composed mainly of intermediate-acid volcanics and granites; (3) the transform margin in the Early-Middle Triassic indicated by the simultaneous stratigraphic break, and (4) the passive continental margin in the Late Triassic characterized by the marine-terrigenous facies sedimentary formation.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Jiamusi massif</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Heilongjiang plate</subfield><subfield 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Zhang, Xing Zhou |
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Zhang, Xing Zhou ddc 550 misc Jiamusi massif misc Heilongjiang plate misc continental margin misc Northeastern China Late Paleozoic-Early Mesozoic tectonic evolution in the east margin of the Jiamusi massif, eastern northeastern China |
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550 ASE Late Paleozoic-Early Mesozoic tectonic evolution in the east margin of the Jiamusi massif, eastern northeastern China Jiamusi massif (dpeaa)DE-He213 Heilongjiang plate (dpeaa)DE-He213 continental margin (dpeaa)DE-He213 Northeastern China (dpeaa)DE-He213 |
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ddc 550 misc Jiamusi massif misc Heilongjiang plate misc continental margin misc Northeastern China |
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ddc 550 misc Jiamusi massif misc Heilongjiang plate misc continental margin misc Northeastern China |
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ddc 550 misc Jiamusi massif misc Heilongjiang plate misc continental margin misc Northeastern China |
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Late Paleozoic-Early Mesozoic tectonic evolution in the east margin of the Jiamusi massif, eastern northeastern China |
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Late Paleozoic-Early Mesozoic tectonic evolution in the east margin of the Jiamusi massif, eastern northeastern China |
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Zhang, Xing Zhou Guo, Ye Zhou, Jian Bo Zeng, Zhen Pu, Jian Bin Fu, Qiu Lin |
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late paleozoic-early mesozoic tectonic evolution in the east margin of the jiamusi massif, eastern northeastern china |
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Late Paleozoic-Early Mesozoic tectonic evolution in the east margin of the Jiamusi massif, eastern northeastern China |
| abstract |
Abstract The Jiamusi massif is a major tectonic unit in the eastern part of NE China and composed chiefly of the Early Paleozoic (about 500 Ma) metamorphosed crystalline basement containing Precambrian, even Archean crust and three suites of unmetamorphosed continental marginal sedimentary formations of the Devonian-Lower Carboniferous, the Late Carboniferous-Permian and the Late Triassic, which are similar to those in the Bureya and Khanka massifs in Russia. In the Devonian-Lower Carboniferous, the microcontinent consisting of the Jiamusi and Songnen massifs in China and the Bureya and Khanka massifs in Russia evolved independently, the eastern part of which was a passive continental margin, where a suite of the marine sedimentary-volcanic formation is overlain unconformably on the crystalline basement. The regional stratigraphic break in the middle Carboniferous in the whole northeastern China was related to the collision of the microcontinent with the Argun-Hinggan microcontinent in the west, indicating the formation of a new amalgamated continent (Heilongjiang plate). Therefore, the Late Carboniferous-Permian volcanic-sedimentary formation is the first unitary cover on the Heilongjiang plate. The Late Carboniferous-Permian and the Late Triassic sedimentary formations in the eastern part of the Jiamusi-Bureya-Khanka microcontinent represent the evolutional features of the eastern continental margin of the Heilongjiang plate. Summarily, the eastern margin of the Heilongjiang plate mainly suffered the following evolution stages from the Late Carboniferous to the Late Triassic: (1) the transform or passive continental margin in the Late Carboniferous, characterized by terrestrial facies clastic rocks with interbeded recoverable coal layers; (2) the active continental margin in the Permian marked by the magmatic arc composed mainly of intermediate-acid volcanics and granites; (3) the transform margin in the Early-Middle Triassic indicated by the simultaneous stratigraphic break, and (4) the passive continental margin in the Late Triassic characterized by the marine-terrigenous facies sedimentary formation. |
| abstractGer |
Abstract The Jiamusi massif is a major tectonic unit in the eastern part of NE China and composed chiefly of the Early Paleozoic (about 500 Ma) metamorphosed crystalline basement containing Precambrian, even Archean crust and three suites of unmetamorphosed continental marginal sedimentary formations of the Devonian-Lower Carboniferous, the Late Carboniferous-Permian and the Late Triassic, which are similar to those in the Bureya and Khanka massifs in Russia. In the Devonian-Lower Carboniferous, the microcontinent consisting of the Jiamusi and Songnen massifs in China and the Bureya and Khanka massifs in Russia evolved independently, the eastern part of which was a passive continental margin, where a suite of the marine sedimentary-volcanic formation is overlain unconformably on the crystalline basement. The regional stratigraphic break in the middle Carboniferous in the whole northeastern China was related to the collision of the microcontinent with the Argun-Hinggan microcontinent in the west, indicating the formation of a new amalgamated continent (Heilongjiang plate). Therefore, the Late Carboniferous-Permian volcanic-sedimentary formation is the first unitary cover on the Heilongjiang plate. The Late Carboniferous-Permian and the Late Triassic sedimentary formations in the eastern part of the Jiamusi-Bureya-Khanka microcontinent represent the evolutional features of the eastern continental margin of the Heilongjiang plate. Summarily, the eastern margin of the Heilongjiang plate mainly suffered the following evolution stages from the Late Carboniferous to the Late Triassic: (1) the transform or passive continental margin in the Late Carboniferous, characterized by terrestrial facies clastic rocks with interbeded recoverable coal layers; (2) the active continental margin in the Permian marked by the magmatic arc composed mainly of intermediate-acid volcanics and granites; (3) the transform margin in the Early-Middle Triassic indicated by the simultaneous stratigraphic break, and (4) the passive continental margin in the Late Triassic characterized by the marine-terrigenous facies sedimentary formation. |
| abstract_unstemmed |
Abstract The Jiamusi massif is a major tectonic unit in the eastern part of NE China and composed chiefly of the Early Paleozoic (about 500 Ma) metamorphosed crystalline basement containing Precambrian, even Archean crust and three suites of unmetamorphosed continental marginal sedimentary formations of the Devonian-Lower Carboniferous, the Late Carboniferous-Permian and the Late Triassic, which are similar to those in the Bureya and Khanka massifs in Russia. In the Devonian-Lower Carboniferous, the microcontinent consisting of the Jiamusi and Songnen massifs in China and the Bureya and Khanka massifs in Russia evolved independently, the eastern part of which was a passive continental margin, where a suite of the marine sedimentary-volcanic formation is overlain unconformably on the crystalline basement. The regional stratigraphic break in the middle Carboniferous in the whole northeastern China was related to the collision of the microcontinent with the Argun-Hinggan microcontinent in the west, indicating the formation of a new amalgamated continent (Heilongjiang plate). Therefore, the Late Carboniferous-Permian volcanic-sedimentary formation is the first unitary cover on the Heilongjiang plate. The Late Carboniferous-Permian and the Late Triassic sedimentary formations in the eastern part of the Jiamusi-Bureya-Khanka microcontinent represent the evolutional features of the eastern continental margin of the Heilongjiang plate. Summarily, the eastern margin of the Heilongjiang plate mainly suffered the following evolution stages from the Late Carboniferous to the Late Triassic: (1) the transform or passive continental margin in the Late Carboniferous, characterized by terrestrial facies clastic rocks with interbeded recoverable coal layers; (2) the active continental margin in the Permian marked by the magmatic arc composed mainly of intermediate-acid volcanics and granites; (3) the transform margin in the Early-Middle Triassic indicated by the simultaneous stratigraphic break, and (4) the passive continental margin in the Late Triassic characterized by the marine-terrigenous facies sedimentary formation. |
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| title_short |
Late Paleozoic-Early Mesozoic tectonic evolution in the east margin of the Jiamusi massif, eastern northeastern China |
| url |
https://dx.doi.org/10.1134/S181971401501008X |
| remote_bool |
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| author2 |
Guo, Ye Zhou, Jian Bo Zeng, Zhen Pu, Jian Bin Fu, Qiu Lin |
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2024-07-04T01:25:39.313Z |
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| score |
7.3984814 |