Lithogeochemistry of Vendian fine-grained clastic rocks in the Nepa-Zhuya region of the Siberian Platform
Abstract The possibility of reconstructing lithogenetic settings, composition of rocks in provenances, and geodynamic regimes characteristic of the formation of Vendian rocks in the Patom and Nepa–Botuoba sedimentary basins during the late Dal’nyaya Taiga–early Zhuya time and defining interrelations...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Podkovyrov, V. N. [verfasserIn] Kotova, L. N. [verfasserIn] Golubkova, E. Yu. [verfasserIn] Ivanovskaya, A. V. [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: Lithology and mineral resources - Moscow : MAIK Nauka/Interperiodica Publ., 2000, 50(2015), 4 vom: Juli, Seite 299-310 |
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| Übergeordnetes Werk: |
volume:50 ; year:2015 ; number:4 ; month:07 ; pages:299-310 |
| Links: |
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| DOI / URN: |
10.1134/S0024490215040057 |
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| Katalog-ID: |
SPR01537937X |
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| 520 | |a Abstract The possibility of reconstructing lithogenetic settings, composition of rocks in provenances, and geodynamic regimes characteristic of the formation of Vendian rocks in the Patom and Nepa–Botuoba sedimentary basins during the late Dal’nyaya Taiga–early Zhuya time and defining interrelations between organic-walled fossils and depositional environments is considered on the basis of the lithogeochemical data. For reconstructing paleogeodynamic depositional settings of sedimentary sequences, several well-known discriminant diagrams, such as $ K_{2} $O/$ Na_{2} $O-$ SiO_{2} $/$ Al_{2} %$ O_{3} $, $ SiO_{2} $-$ K_{2} $O/$ Na_{2} $O, and Th-La-Sc, were used. It is shown that some of them may be used with a variable degree of reliability for reconstructing depositional environments for platformal sedimentary successions composed of both sandstones and fine-grained clastic rocks. The most taxonomically diverse and abundant microfossil assemblages from the Ura and Parsha formations of the Zhuya-Lena area and Nepa–Botuoba anticlinorium, respectively, are confined to structurally and mineralogically immature silty–clayey shelf sediments buried rapidly under new portions of sediments in disoxic environments. | ||
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| 700 | 1 | |a Kotova, L. N. |e verfasserin |4 aut | |
| 700 | 1 | |a Golubkova, E. Yu. |e verfasserin |4 aut | |
| 700 | 1 | |a Ivanovskaya, A. V. |e verfasserin |4 aut | |
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10.1134/S0024490215040057 doi (DE-627)SPR01537937X (SPR)S0024490215040057-e DE-627 ger DE-627 rakwb eng 550 ASE 38.25 bkl 38.50 bkl Podkovyrov, V. N. verfasserin aut Lithogeochemistry of Vendian fine-grained clastic rocks in the Nepa-Zhuya region of the Siberian Platform 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The possibility of reconstructing lithogenetic settings, composition of rocks in provenances, and geodynamic regimes characteristic of the formation of Vendian rocks in the Patom and Nepa–Botuoba sedimentary basins during the late Dal’nyaya Taiga–early Zhuya time and defining interrelations between organic-walled fossils and depositional environments is considered on the basis of the lithogeochemical data. For reconstructing paleogeodynamic depositional settings of sedimentary sequences, several well-known discriminant diagrams, such as $ K_{2} $O/$ Na_{2} $O-$ SiO_{2} $/$ Al_{2} %$ O_{3} $, $ SiO_{2} $-$ K_{2} $O/$ Na_{2} $O, and Th-La-Sc, were used. It is shown that some of them may be used with a variable degree of reliability for reconstructing depositional environments for platformal sedimentary successions composed of both sandstones and fine-grained clastic rocks. The most taxonomically diverse and abundant microfossil assemblages from the Ura and Parsha formations of the Zhuya-Lena area and Nepa–Botuoba anticlinorium, respectively, are confined to structurally and mineralogically immature silty–clayey shelf sediments buried rapidly under new portions of sediments in disoxic environments. Mudstone (dpeaa)DE-He213 Siberian Platform (dpeaa)DE-He213 Active Continental Margin (dpeaa)DE-He213 Passive Continental Margin (dpeaa)DE-He213 Silty Mudstone (dpeaa)DE-He213 Kotova, L. N. verfasserin aut Golubkova, E. Yu. verfasserin aut Ivanovskaya, A. V. verfasserin aut Enthalten in Lithology and mineral resources Moscow : MAIK Nauka/Interperiodica Publ., 2000 50(2015), 4 vom: Juli, Seite 299-310 (DE-627)334711576 (DE-600)2058091-5 1608-3229 nnns volume:50 year:2015 number:4 month:07 pages:299-310 https://dx.doi.org/10.1134/S0024490215040057 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_206 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_2056 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 38.25 ASE 38.50 ASE AR 50 2015 4 07 299-310 |
| spelling |
10.1134/S0024490215040057 doi (DE-627)SPR01537937X (SPR)S0024490215040057-e DE-627 ger DE-627 rakwb eng 550 ASE 38.25 bkl 38.50 bkl Podkovyrov, V. N. verfasserin aut Lithogeochemistry of Vendian fine-grained clastic rocks in the Nepa-Zhuya region of the Siberian Platform 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The possibility of reconstructing lithogenetic settings, composition of rocks in provenances, and geodynamic regimes characteristic of the formation of Vendian rocks in the Patom and Nepa–Botuoba sedimentary basins during the late Dal’nyaya Taiga–early Zhuya time and defining interrelations between organic-walled fossils and depositional environments is considered on the basis of the lithogeochemical data. For reconstructing paleogeodynamic depositional settings of sedimentary sequences, several well-known discriminant diagrams, such as $ K_{2} $O/$ Na_{2} $O-$ SiO_{2} $/$ Al_{2} %$ O_{3} $, $ SiO_{2} $-$ K_{2} $O/$ Na_{2} $O, and Th-La-Sc, were used. It is shown that some of them may be used with a variable degree of reliability for reconstructing depositional environments for platformal sedimentary successions composed of both sandstones and fine-grained clastic rocks. The most taxonomically diverse and abundant microfossil assemblages from the Ura and Parsha formations of the Zhuya-Lena area and Nepa–Botuoba anticlinorium, respectively, are confined to structurally and mineralogically immature silty–clayey shelf sediments buried rapidly under new portions of sediments in disoxic environments. Mudstone (dpeaa)DE-He213 Siberian Platform (dpeaa)DE-He213 Active Continental Margin (dpeaa)DE-He213 Passive Continental Margin (dpeaa)DE-He213 Silty Mudstone (dpeaa)DE-He213 Kotova, L. N. verfasserin aut Golubkova, E. Yu. verfasserin aut Ivanovskaya, A. V. verfasserin aut Enthalten in Lithology and mineral resources Moscow : MAIK Nauka/Interperiodica Publ., 2000 50(2015), 4 vom: Juli, Seite 299-310 (DE-627)334711576 (DE-600)2058091-5 1608-3229 nnns volume:50 year:2015 number:4 month:07 pages:299-310 https://dx.doi.org/10.1134/S0024490215040057 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_206 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_2056 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 38.25 ASE 38.50 ASE AR 50 2015 4 07 299-310 |
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10.1134/S0024490215040057 doi (DE-627)SPR01537937X (SPR)S0024490215040057-e DE-627 ger DE-627 rakwb eng 550 ASE 38.25 bkl 38.50 bkl Podkovyrov, V. N. verfasserin aut Lithogeochemistry of Vendian fine-grained clastic rocks in the Nepa-Zhuya region of the Siberian Platform 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The possibility of reconstructing lithogenetic settings, composition of rocks in provenances, and geodynamic regimes characteristic of the formation of Vendian rocks in the Patom and Nepa–Botuoba sedimentary basins during the late Dal’nyaya Taiga–early Zhuya time and defining interrelations between organic-walled fossils and depositional environments is considered on the basis of the lithogeochemical data. For reconstructing paleogeodynamic depositional settings of sedimentary sequences, several well-known discriminant diagrams, such as $ K_{2} $O/$ Na_{2} $O-$ SiO_{2} $/$ Al_{2} %$ O_{3} $, $ SiO_{2} $-$ K_{2} $O/$ Na_{2} $O, and Th-La-Sc, were used. It is shown that some of them may be used with a variable degree of reliability for reconstructing depositional environments for platformal sedimentary successions composed of both sandstones and fine-grained clastic rocks. The most taxonomically diverse and abundant microfossil assemblages from the Ura and Parsha formations of the Zhuya-Lena area and Nepa–Botuoba anticlinorium, respectively, are confined to structurally and mineralogically immature silty–clayey shelf sediments buried rapidly under new portions of sediments in disoxic environments. Mudstone (dpeaa)DE-He213 Siberian Platform (dpeaa)DE-He213 Active Continental Margin (dpeaa)DE-He213 Passive Continental Margin (dpeaa)DE-He213 Silty Mudstone (dpeaa)DE-He213 Kotova, L. N. verfasserin aut Golubkova, E. Yu. verfasserin aut Ivanovskaya, A. V. verfasserin aut Enthalten in Lithology and mineral resources Moscow : MAIK Nauka/Interperiodica Publ., 2000 50(2015), 4 vom: Juli, Seite 299-310 (DE-627)334711576 (DE-600)2058091-5 1608-3229 nnns volume:50 year:2015 number:4 month:07 pages:299-310 https://dx.doi.org/10.1134/S0024490215040057 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_206 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_2056 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 38.25 ASE 38.50 ASE AR 50 2015 4 07 299-310 |
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10.1134/S0024490215040057 doi (DE-627)SPR01537937X (SPR)S0024490215040057-e DE-627 ger DE-627 rakwb eng 550 ASE 38.25 bkl 38.50 bkl Podkovyrov, V. N. verfasserin aut Lithogeochemistry of Vendian fine-grained clastic rocks in the Nepa-Zhuya region of the Siberian Platform 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract The possibility of reconstructing lithogenetic settings, composition of rocks in provenances, and geodynamic regimes characteristic of the formation of Vendian rocks in the Patom and Nepa–Botuoba sedimentary basins during the late Dal’nyaya Taiga–early Zhuya time and defining interrelations between organic-walled fossils and depositional environments is considered on the basis of the lithogeochemical data. For reconstructing paleogeodynamic depositional settings of sedimentary sequences, several well-known discriminant diagrams, such as $ K_{2} $O/$ Na_{2} $O-$ SiO_{2} $/$ Al_{2} %$ O_{3} $, $ SiO_{2} $-$ K_{2} $O/$ Na_{2} $O, and Th-La-Sc, were used. It is shown that some of them may be used with a variable degree of reliability for reconstructing depositional environments for platformal sedimentary successions composed of both sandstones and fine-grained clastic rocks. The most taxonomically diverse and abundant microfossil assemblages from the Ura and Parsha formations of the Zhuya-Lena area and Nepa–Botuoba anticlinorium, respectively, are confined to structurally and mineralogically immature silty–clayey shelf sediments buried rapidly under new portions of sediments in disoxic environments. Mudstone (dpeaa)DE-He213 Siberian Platform (dpeaa)DE-He213 Active Continental Margin (dpeaa)DE-He213 Passive Continental Margin (dpeaa)DE-He213 Silty Mudstone (dpeaa)DE-He213 Kotova, L. N. verfasserin aut Golubkova, E. Yu. verfasserin aut Ivanovskaya, A. V. verfasserin aut Enthalten in Lithology and mineral resources Moscow : MAIK Nauka/Interperiodica Publ., 2000 50(2015), 4 vom: Juli, Seite 299-310 (DE-627)334711576 (DE-600)2058091-5 1608-3229 nnns volume:50 year:2015 number:4 month:07 pages:299-310 https://dx.doi.org/10.1134/S0024490215040057 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_206 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_2056 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 38.25 ASE 38.50 ASE AR 50 2015 4 07 299-310 |
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Enthalten in Lithology and mineral resources 50(2015), 4 vom: Juli, Seite 299-310 volume:50 year:2015 number:4 month:07 pages:299-310 |
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For reconstructing paleogeodynamic depositional settings of sedimentary sequences, several well-known discriminant diagrams, such as $ K_{2} $O/$ Na_{2} $O-$ SiO_{2} $/$ Al_{2} %$ O_{3} $, $ SiO_{2} $-$ K_{2} $O/$ Na_{2} $O, and Th-La-Sc, were used. It is shown that some of them may be used with a variable degree of reliability for reconstructing depositional environments for platformal sedimentary successions composed of both sandstones and fine-grained clastic rocks. The most taxonomically diverse and abundant microfossil assemblages from the Ura and Parsha formations of the Zhuya-Lena area and Nepa–Botuoba anticlinorium, respectively, are confined to structurally and mineralogically immature silty–clayey shelf sediments buried rapidly under new portions of sediments in disoxic environments.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Mudstone</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Siberian Platform</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Active Continental Margin</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Passive Continental Margin</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Silty Mudstone</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kotova, L. 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Podkovyrov, V. N. |
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Podkovyrov, V. N. ddc 550 bkl 38.25 bkl 38.50 misc Mudstone misc Siberian Platform misc Active Continental Margin misc Passive Continental Margin misc Silty Mudstone Lithogeochemistry of Vendian fine-grained clastic rocks in the Nepa-Zhuya region of the Siberian Platform |
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550 ASE 38.25 bkl 38.50 bkl Lithogeochemistry of Vendian fine-grained clastic rocks in the Nepa-Zhuya region of the Siberian Platform Mudstone (dpeaa)DE-He213 Siberian Platform (dpeaa)DE-He213 Active Continental Margin (dpeaa)DE-He213 Passive Continental Margin (dpeaa)DE-He213 Silty Mudstone (dpeaa)DE-He213 |
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lithogeochemistry of vendian fine-grained clastic rocks in the nepa-zhuya region of the siberian platform |
| title_auth |
Lithogeochemistry of Vendian fine-grained clastic rocks in the Nepa-Zhuya region of the Siberian Platform |
| abstract |
Abstract The possibility of reconstructing lithogenetic settings, composition of rocks in provenances, and geodynamic regimes characteristic of the formation of Vendian rocks in the Patom and Nepa–Botuoba sedimentary basins during the late Dal’nyaya Taiga–early Zhuya time and defining interrelations between organic-walled fossils and depositional environments is considered on the basis of the lithogeochemical data. For reconstructing paleogeodynamic depositional settings of sedimentary sequences, several well-known discriminant diagrams, such as $ K_{2} $O/$ Na_{2} $O-$ SiO_{2} $/$ Al_{2} %$ O_{3} $, $ SiO_{2} $-$ K_{2} $O/$ Na_{2} $O, and Th-La-Sc, were used. It is shown that some of them may be used with a variable degree of reliability for reconstructing depositional environments for platformal sedimentary successions composed of both sandstones and fine-grained clastic rocks. The most taxonomically diverse and abundant microfossil assemblages from the Ura and Parsha formations of the Zhuya-Lena area and Nepa–Botuoba anticlinorium, respectively, are confined to structurally and mineralogically immature silty–clayey shelf sediments buried rapidly under new portions of sediments in disoxic environments. |
| abstractGer |
Abstract The possibility of reconstructing lithogenetic settings, composition of rocks in provenances, and geodynamic regimes characteristic of the formation of Vendian rocks in the Patom and Nepa–Botuoba sedimentary basins during the late Dal’nyaya Taiga–early Zhuya time and defining interrelations between organic-walled fossils and depositional environments is considered on the basis of the lithogeochemical data. For reconstructing paleogeodynamic depositional settings of sedimentary sequences, several well-known discriminant diagrams, such as $ K_{2} $O/$ Na_{2} $O-$ SiO_{2} $/$ Al_{2} %$ O_{3} $, $ SiO_{2} $-$ K_{2} $O/$ Na_{2} $O, and Th-La-Sc, were used. It is shown that some of them may be used with a variable degree of reliability for reconstructing depositional environments for platformal sedimentary successions composed of both sandstones and fine-grained clastic rocks. The most taxonomically diverse and abundant microfossil assemblages from the Ura and Parsha formations of the Zhuya-Lena area and Nepa–Botuoba anticlinorium, respectively, are confined to structurally and mineralogically immature silty–clayey shelf sediments buried rapidly under new portions of sediments in disoxic environments. |
| abstract_unstemmed |
Abstract The possibility of reconstructing lithogenetic settings, composition of rocks in provenances, and geodynamic regimes characteristic of the formation of Vendian rocks in the Patom and Nepa–Botuoba sedimentary basins during the late Dal’nyaya Taiga–early Zhuya time and defining interrelations between organic-walled fossils and depositional environments is considered on the basis of the lithogeochemical data. For reconstructing paleogeodynamic depositional settings of sedimentary sequences, several well-known discriminant diagrams, such as $ K_{2} $O/$ Na_{2} $O-$ SiO_{2} $/$ Al_{2} %$ O_{3} $, $ SiO_{2} $-$ K_{2} $O/$ Na_{2} $O, and Th-La-Sc, were used. It is shown that some of them may be used with a variable degree of reliability for reconstructing depositional environments for platformal sedimentary successions composed of both sandstones and fine-grained clastic rocks. The most taxonomically diverse and abundant microfossil assemblages from the Ura and Parsha formations of the Zhuya-Lena area and Nepa–Botuoba anticlinorium, respectively, are confined to structurally and mineralogically immature silty–clayey shelf sediments buried rapidly under new portions of sediments in disoxic environments. |
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Lithogeochemistry of Vendian fine-grained clastic rocks in the Nepa-Zhuya region of the Siberian Platform |
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https://dx.doi.org/10.1134/S0024490215040057 |
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Kotova, L. N. Golubkova, E. Yu Ivanovskaya, A. V. |
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| score |
7.4003134 |