Provenance of Volcanogenic Deposits from the Shanxi Formation of the Daniudi Gas Field, Ordos Basin, and Its Tectonic Implications

Through detailed drill-core description, petrography, cathodoluminescence imaging, and geochemistry analysis, sedimentary deposits with a high content of volcanogenic components (27.6%) were discovered in the Shanxi Formation of the Daniudi Gas Field, Ordos Basin. The volcanogenic components include...
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Autor*in:	Xuejiao Qu [verfasserIn] Qiao Wang [verfasserIn] Dunfan Wang [verfasserIn] Tao Lei [verfasserIn] Hao Chen [verfasserIn] Jia Wang [verfasserIn] Wei Jiang [verfasserIn] Wei Zhang [verfasserIn] Long Luo [verfasserIn] Jianping Liu [verfasserIn] Nan Jiang [verfasserIn] Xuanbo Gao [verfasserIn] Xianfeng Tan [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2023

Schlagwörter:	volcanogenic sedimentary deposits provenance tectonic evolution Shanxi formation Ordos Basin

Übergeordnetes Werk:	In: Minerals - MDPI AG, 2012, 13(2023), 12, p 1546
Übergeordnetes Werk:	volume:13 ; year:2023 ; number:12, p 1546

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.3390/min13121546

Katalog-ID:	DOAJ09882340X

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allfields	10.3390/min13121546 doi (DE-627)DOAJ09882340X (DE-599)DOAJ3022387d3dcc4501a88bb7cdfce22257 DE-627 ger DE-627 rakwb eng QE351-399.2 Xuejiao Qu verfasserin aut Provenance of Volcanogenic Deposits from the Shanxi Formation of the Daniudi Gas Field, Ordos Basin, and Its Tectonic Implications 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Through detailed drill-core description, petrography, cathodoluminescence imaging, and geochemistry analysis, sedimentary deposits with a high content of volcanogenic components (27.6%) were discovered in the Shanxi Formation of the Daniudi Gas Field, Ordos Basin. The volcanogenic components include volcanogenic quartz, lava fragments (dominated by rhyolite fragments), tuff fragments, and tuffaceous matrix. In addition, at least two volcanic ash layers were discovered. Although the metamorphic rocks of the Precambrian succession in the ancient land of Yin Mountain are usually considered the primary source of the Shanxi formation, it is most likely that the volcanogenic components were derived from intermediate-acid volcanic materials that accumulated in the Daqingshan area during the Late Carboniferous to Early Permian. Those volcanogenic components are mainly transported by flowing water rather than by air from origin to basin. In addition, the accumulation of volcanic materials in the Daqingshan area was controlled by volcanic eruptions occurring solely in this area, rather than by the Inner Mongolia Orogenic Belt. Those volcanic eruptions were related to the southward subduction of the Paleo-Asian Ocean Plate beneath the northern margin of the North China Plate in the Late Carboniferous to Early Permian. The active continental margin related to the subduction of the Paleo-Asian Ocean Plate lasted at least until the Early Permian, and the closure of the Paleo-Asian Ocean must have occurred later than the Early Permian. volcanogenic sedimentary deposits provenance tectonic evolution Shanxi formation Ordos Basin Mineralogy Qiao Wang verfasserin aut Dunfan Wang verfasserin aut Tao Lei verfasserin aut Hao Chen verfasserin aut Jia Wang verfasserin aut Wei Jiang verfasserin aut Wei Zhang verfasserin aut Long Luo verfasserin aut Jianping Liu verfasserin aut Nan Jiang verfasserin aut Xuanbo Gao verfasserin aut Xianfeng Tan verfasserin aut In Minerals MDPI AG, 2012 13(2023), 12, p 1546 (DE-627)689132069 (DE-600)2655947-X 2075163X nnns volume:13 year:2023 number:12, p 1546 https://doi.org/10.3390/min13121546 kostenfrei https://doaj.org/article/3022387d3dcc4501a88bb7cdfce22257 kostenfrei https://www.mdpi.com/2075-163X/13/12/1546 kostenfrei https://doaj.org/toc/2075-163X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 13 2023 12, p 1546
spelling	10.3390/min13121546 doi (DE-627)DOAJ09882340X (DE-599)DOAJ3022387d3dcc4501a88bb7cdfce22257 DE-627 ger DE-627 rakwb eng QE351-399.2 Xuejiao Qu verfasserin aut Provenance of Volcanogenic Deposits from the Shanxi Formation of the Daniudi Gas Field, Ordos Basin, and Its Tectonic Implications 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Through detailed drill-core description, petrography, cathodoluminescence imaging, and geochemistry analysis, sedimentary deposits with a high content of volcanogenic components (27.6%) were discovered in the Shanxi Formation of the Daniudi Gas Field, Ordos Basin. The volcanogenic components include volcanogenic quartz, lava fragments (dominated by rhyolite fragments), tuff fragments, and tuffaceous matrix. In addition, at least two volcanic ash layers were discovered. Although the metamorphic rocks of the Precambrian succession in the ancient land of Yin Mountain are usually considered the primary source of the Shanxi formation, it is most likely that the volcanogenic components were derived from intermediate-acid volcanic materials that accumulated in the Daqingshan area during the Late Carboniferous to Early Permian. Those volcanogenic components are mainly transported by flowing water rather than by air from origin to basin. In addition, the accumulation of volcanic materials in the Daqingshan area was controlled by volcanic eruptions occurring solely in this area, rather than by the Inner Mongolia Orogenic Belt. Those volcanic eruptions were related to the southward subduction of the Paleo-Asian Ocean Plate beneath the northern margin of the North China Plate in the Late Carboniferous to Early Permian. The active continental margin related to the subduction of the Paleo-Asian Ocean Plate lasted at least until the Early Permian, and the closure of the Paleo-Asian Ocean must have occurred later than the Early Permian. volcanogenic sedimentary deposits provenance tectonic evolution Shanxi formation Ordos Basin Mineralogy Qiao Wang verfasserin aut Dunfan Wang verfasserin aut Tao Lei verfasserin aut Hao Chen verfasserin aut Jia Wang verfasserin aut Wei Jiang verfasserin aut Wei Zhang verfasserin aut Long Luo verfasserin aut Jianping Liu verfasserin aut Nan Jiang verfasserin aut Xuanbo Gao verfasserin aut Xianfeng Tan verfasserin aut In Minerals MDPI AG, 2012 13(2023), 12, p 1546 (DE-627)689132069 (DE-600)2655947-X 2075163X nnns volume:13 year:2023 number:12, p 1546 https://doi.org/10.3390/min13121546 kostenfrei https://doaj.org/article/3022387d3dcc4501a88bb7cdfce22257 kostenfrei https://www.mdpi.com/2075-163X/13/12/1546 kostenfrei https://doaj.org/toc/2075-163X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 13 2023 12, p 1546
allfields_unstemmed	10.3390/min13121546 doi (DE-627)DOAJ09882340X (DE-599)DOAJ3022387d3dcc4501a88bb7cdfce22257 DE-627 ger DE-627 rakwb eng QE351-399.2 Xuejiao Qu verfasserin aut Provenance of Volcanogenic Deposits from the Shanxi Formation of the Daniudi Gas Field, Ordos Basin, and Its Tectonic Implications 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Through detailed drill-core description, petrography, cathodoluminescence imaging, and geochemistry analysis, sedimentary deposits with a high content of volcanogenic components (27.6%) were discovered in the Shanxi Formation of the Daniudi Gas Field, Ordos Basin. The volcanogenic components include volcanogenic quartz, lava fragments (dominated by rhyolite fragments), tuff fragments, and tuffaceous matrix. In addition, at least two volcanic ash layers were discovered. Although the metamorphic rocks of the Precambrian succession in the ancient land of Yin Mountain are usually considered the primary source of the Shanxi formation, it is most likely that the volcanogenic components were derived from intermediate-acid volcanic materials that accumulated in the Daqingshan area during the Late Carboniferous to Early Permian. Those volcanogenic components are mainly transported by flowing water rather than by air from origin to basin. In addition, the accumulation of volcanic materials in the Daqingshan area was controlled by volcanic eruptions occurring solely in this area, rather than by the Inner Mongolia Orogenic Belt. Those volcanic eruptions were related to the southward subduction of the Paleo-Asian Ocean Plate beneath the northern margin of the North China Plate in the Late Carboniferous to Early Permian. The active continental margin related to the subduction of the Paleo-Asian Ocean Plate lasted at least until the Early Permian, and the closure of the Paleo-Asian Ocean must have occurred later than the Early Permian. volcanogenic sedimentary deposits provenance tectonic evolution Shanxi formation Ordos Basin Mineralogy Qiao Wang verfasserin aut Dunfan Wang verfasserin aut Tao Lei verfasserin aut Hao Chen verfasserin aut Jia Wang verfasserin aut Wei Jiang verfasserin aut Wei Zhang verfasserin aut Long Luo verfasserin aut Jianping Liu verfasserin aut Nan Jiang verfasserin aut Xuanbo Gao verfasserin aut Xianfeng Tan verfasserin aut In Minerals MDPI AG, 2012 13(2023), 12, p 1546 (DE-627)689132069 (DE-600)2655947-X 2075163X nnns volume:13 year:2023 number:12, p 1546 https://doi.org/10.3390/min13121546 kostenfrei https://doaj.org/article/3022387d3dcc4501a88bb7cdfce22257 kostenfrei https://www.mdpi.com/2075-163X/13/12/1546 kostenfrei https://doaj.org/toc/2075-163X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 13 2023 12, p 1546
allfieldsGer	10.3390/min13121546 doi (DE-627)DOAJ09882340X (DE-599)DOAJ3022387d3dcc4501a88bb7cdfce22257 DE-627 ger DE-627 rakwb eng QE351-399.2 Xuejiao Qu verfasserin aut Provenance of Volcanogenic Deposits from the Shanxi Formation of the Daniudi Gas Field, Ordos Basin, and Its Tectonic Implications 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Through detailed drill-core description, petrography, cathodoluminescence imaging, and geochemistry analysis, sedimentary deposits with a high content of volcanogenic components (27.6%) were discovered in the Shanxi Formation of the Daniudi Gas Field, Ordos Basin. The volcanogenic components include volcanogenic quartz, lava fragments (dominated by rhyolite fragments), tuff fragments, and tuffaceous matrix. In addition, at least two volcanic ash layers were discovered. Although the metamorphic rocks of the Precambrian succession in the ancient land of Yin Mountain are usually considered the primary source of the Shanxi formation, it is most likely that the volcanogenic components were derived from intermediate-acid volcanic materials that accumulated in the Daqingshan area during the Late Carboniferous to Early Permian. Those volcanogenic components are mainly transported by flowing water rather than by air from origin to basin. In addition, the accumulation of volcanic materials in the Daqingshan area was controlled by volcanic eruptions occurring solely in this area, rather than by the Inner Mongolia Orogenic Belt. Those volcanic eruptions were related to the southward subduction of the Paleo-Asian Ocean Plate beneath the northern margin of the North China Plate in the Late Carboniferous to Early Permian. The active continental margin related to the subduction of the Paleo-Asian Ocean Plate lasted at least until the Early Permian, and the closure of the Paleo-Asian Ocean must have occurred later than the Early Permian. volcanogenic sedimentary deposits provenance tectonic evolution Shanxi formation Ordos Basin Mineralogy Qiao Wang verfasserin aut Dunfan Wang verfasserin aut Tao Lei verfasserin aut Hao Chen verfasserin aut Jia Wang verfasserin aut Wei Jiang verfasserin aut Wei Zhang verfasserin aut Long Luo verfasserin aut Jianping Liu verfasserin aut Nan Jiang verfasserin aut Xuanbo Gao verfasserin aut Xianfeng Tan verfasserin aut In Minerals MDPI AG, 2012 13(2023), 12, p 1546 (DE-627)689132069 (DE-600)2655947-X 2075163X nnns volume:13 year:2023 number:12, p 1546 https://doi.org/10.3390/min13121546 kostenfrei https://doaj.org/article/3022387d3dcc4501a88bb7cdfce22257 kostenfrei https://www.mdpi.com/2075-163X/13/12/1546 kostenfrei https://doaj.org/toc/2075-163X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 13 2023 12, p 1546
allfieldsSound	10.3390/min13121546 doi (DE-627)DOAJ09882340X (DE-599)DOAJ3022387d3dcc4501a88bb7cdfce22257 DE-627 ger DE-627 rakwb eng QE351-399.2 Xuejiao Qu verfasserin aut Provenance of Volcanogenic Deposits from the Shanxi Formation of the Daniudi Gas Field, Ordos Basin, and Its Tectonic Implications 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Through detailed drill-core description, petrography, cathodoluminescence imaging, and geochemistry analysis, sedimentary deposits with a high content of volcanogenic components (27.6%) were discovered in the Shanxi Formation of the Daniudi Gas Field, Ordos Basin. The volcanogenic components include volcanogenic quartz, lava fragments (dominated by rhyolite fragments), tuff fragments, and tuffaceous matrix. In addition, at least two volcanic ash layers were discovered. Although the metamorphic rocks of the Precambrian succession in the ancient land of Yin Mountain are usually considered the primary source of the Shanxi formation, it is most likely that the volcanogenic components were derived from intermediate-acid volcanic materials that accumulated in the Daqingshan area during the Late Carboniferous to Early Permian. Those volcanogenic components are mainly transported by flowing water rather than by air from origin to basin. In addition, the accumulation of volcanic materials in the Daqingshan area was controlled by volcanic eruptions occurring solely in this area, rather than by the Inner Mongolia Orogenic Belt. Those volcanic eruptions were related to the southward subduction of the Paleo-Asian Ocean Plate beneath the northern margin of the North China Plate in the Late Carboniferous to Early Permian. The active continental margin related to the subduction of the Paleo-Asian Ocean Plate lasted at least until the Early Permian, and the closure of the Paleo-Asian Ocean must have occurred later than the Early Permian. volcanogenic sedimentary deposits provenance tectonic evolution Shanxi formation Ordos Basin Mineralogy Qiao Wang verfasserin aut Dunfan Wang verfasserin aut Tao Lei verfasserin aut Hao Chen verfasserin aut Jia Wang verfasserin aut Wei Jiang verfasserin aut Wei Zhang verfasserin aut Long Luo verfasserin aut Jianping Liu verfasserin aut Nan Jiang verfasserin aut Xuanbo Gao verfasserin aut Xianfeng Tan verfasserin aut In Minerals MDPI AG, 2012 13(2023), 12, p 1546 (DE-627)689132069 (DE-600)2655947-X 2075163X nnns volume:13 year:2023 number:12, p 1546 https://doi.org/10.3390/min13121546 kostenfrei https://doaj.org/article/3022387d3dcc4501a88bb7cdfce22257 kostenfrei https://www.mdpi.com/2075-163X/13/12/1546 kostenfrei https://doaj.org/toc/2075-163X Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4338 GBV_ILN_4367 GBV_ILN_4700 AR 13 2023 12, p 1546
language	English
source	In Minerals 13(2023), 12, p 1546 volume:13 year:2023 number:12, p 1546
sourceStr	In Minerals 13(2023), 12, p 1546 volume:13 year:2023 number:12, p 1546
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	volcanogenic sedimentary deposits provenance tectonic evolution Shanxi formation Ordos Basin Mineralogy
isfreeaccess_bool	true
container_title	Minerals
authorswithroles_txt_mv	Xuejiao Qu @@aut@@ Qiao Wang @@aut@@ Dunfan Wang @@aut@@ Tao Lei @@aut@@ Hao Chen @@aut@@ Jia Wang @@aut@@ Wei Jiang @@aut@@ Wei Zhang @@aut@@ Long Luo @@aut@@ Jianping Liu @@aut@@ Nan Jiang @@aut@@ Xuanbo Gao @@aut@@ Xianfeng Tan @@aut@@
publishDateDaySort_date	2023-01-01T00:00:00Z
hierarchy_top_id	689132069
id	DOAJ09882340X
language_de	englisch
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callnumber-first	Q - Science
author	Xuejiao Qu
spellingShingle	Xuejiao Qu misc QE351-399.2 misc volcanogenic sedimentary deposits misc provenance misc tectonic evolution misc Shanxi formation misc Ordos Basin misc Mineralogy Provenance of Volcanogenic Deposits from the Shanxi Formation of the Daniudi Gas Field, Ordos Basin, and Its Tectonic Implications
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topic_title	QE351-399.2 Provenance of Volcanogenic Deposits from the Shanxi Formation of the Daniudi Gas Field, Ordos Basin, and Its Tectonic Implications volcanogenic sedimentary deposits provenance tectonic evolution Shanxi formation Ordos Basin
topic	misc QE351-399.2 misc volcanogenic sedimentary deposits misc provenance misc tectonic evolution misc Shanxi formation misc Ordos Basin misc Mineralogy
topic_unstemmed	misc QE351-399.2 misc volcanogenic sedimentary deposits misc provenance misc tectonic evolution misc Shanxi formation misc Ordos Basin misc Mineralogy
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title	Provenance of Volcanogenic Deposits from the Shanxi Formation of the Daniudi Gas Field, Ordos Basin, and Its Tectonic Implications
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title_full	Provenance of Volcanogenic Deposits from the Shanxi Formation of the Daniudi Gas Field, Ordos Basin, and Its Tectonic Implications
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author_browse	Xuejiao Qu Qiao Wang Dunfan Wang Tao Lei Hao Chen Jia Wang Wei Jiang Wei Zhang Long Luo Jianping Liu Nan Jiang Xuanbo Gao Xianfeng Tan
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title_sort	provenance of volcanogenic deposits from the shanxi formation of the daniudi gas field, ordos basin, and its tectonic implications
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title_auth	Provenance of Volcanogenic Deposits from the Shanxi Formation of the Daniudi Gas Field, Ordos Basin, and Its Tectonic Implications
abstract	Through detailed drill-core description, petrography, cathodoluminescence imaging, and geochemistry analysis, sedimentary deposits with a high content of volcanogenic components (27.6%) were discovered in the Shanxi Formation of the Daniudi Gas Field, Ordos Basin. The volcanogenic components include volcanogenic quartz, lava fragments (dominated by rhyolite fragments), tuff fragments, and tuffaceous matrix. In addition, at least two volcanic ash layers were discovered. Although the metamorphic rocks of the Precambrian succession in the ancient land of Yin Mountain are usually considered the primary source of the Shanxi formation, it is most likely that the volcanogenic components were derived from intermediate-acid volcanic materials that accumulated in the Daqingshan area during the Late Carboniferous to Early Permian. Those volcanogenic components are mainly transported by flowing water rather than by air from origin to basin. In addition, the accumulation of volcanic materials in the Daqingshan area was controlled by volcanic eruptions occurring solely in this area, rather than by the Inner Mongolia Orogenic Belt. Those volcanic eruptions were related to the southward subduction of the Paleo-Asian Ocean Plate beneath the northern margin of the North China Plate in the Late Carboniferous to Early Permian. The active continental margin related to the subduction of the Paleo-Asian Ocean Plate lasted at least until the Early Permian, and the closure of the Paleo-Asian Ocean must have occurred later than the Early Permian.
abstractGer	Through detailed drill-core description, petrography, cathodoluminescence imaging, and geochemistry analysis, sedimentary deposits with a high content of volcanogenic components (27.6%) were discovered in the Shanxi Formation of the Daniudi Gas Field, Ordos Basin. The volcanogenic components include volcanogenic quartz, lava fragments (dominated by rhyolite fragments), tuff fragments, and tuffaceous matrix. In addition, at least two volcanic ash layers were discovered. Although the metamorphic rocks of the Precambrian succession in the ancient land of Yin Mountain are usually considered the primary source of the Shanxi formation, it is most likely that the volcanogenic components were derived from intermediate-acid volcanic materials that accumulated in the Daqingshan area during the Late Carboniferous to Early Permian. Those volcanogenic components are mainly transported by flowing water rather than by air from origin to basin. In addition, the accumulation of volcanic materials in the Daqingshan area was controlled by volcanic eruptions occurring solely in this area, rather than by the Inner Mongolia Orogenic Belt. Those volcanic eruptions were related to the southward subduction of the Paleo-Asian Ocean Plate beneath the northern margin of the North China Plate in the Late Carboniferous to Early Permian. The active continental margin related to the subduction of the Paleo-Asian Ocean Plate lasted at least until the Early Permian, and the closure of the Paleo-Asian Ocean must have occurred later than the Early Permian.
abstract_unstemmed	Through detailed drill-core description, petrography, cathodoluminescence imaging, and geochemistry analysis, sedimentary deposits with a high content of volcanogenic components (27.6%) were discovered in the Shanxi Formation of the Daniudi Gas Field, Ordos Basin. The volcanogenic components include volcanogenic quartz, lava fragments (dominated by rhyolite fragments), tuff fragments, and tuffaceous matrix. In addition, at least two volcanic ash layers were discovered. Although the metamorphic rocks of the Precambrian succession in the ancient land of Yin Mountain are usually considered the primary source of the Shanxi formation, it is most likely that the volcanogenic components were derived from intermediate-acid volcanic materials that accumulated in the Daqingshan area during the Late Carboniferous to Early Permian. Those volcanogenic components are mainly transported by flowing water rather than by air from origin to basin. In addition, the accumulation of volcanic materials in the Daqingshan area was controlled by volcanic eruptions occurring solely in this area, rather than by the Inner Mongolia Orogenic Belt. Those volcanic eruptions were related to the southward subduction of the Paleo-Asian Ocean Plate beneath the northern margin of the North China Plate in the Late Carboniferous to Early Permian. The active continental margin related to the subduction of the Paleo-Asian Ocean Plate lasted at least until the Early Permian, and the closure of the Paleo-Asian Ocean must have occurred later than the Early Permian.
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container_issue	12, p 1546
title_short	Provenance of Volcanogenic Deposits from the Shanxi Formation of the Daniudi Gas Field, Ordos Basin, and Its Tectonic Implications
url	https://doi.org/10.3390/min13121546 https://doaj.org/article/3022387d3dcc4501a88bb7cdfce22257 https://www.mdpi.com/2075-163X/13/12/1546 https://doaj.org/toc/2075-163X
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