Detrital zircon trace elements from the Mesozoic Jiyuan Basin, central China and its implication on tectonic transition of the Qinling Orogenic Belt

The Qinling Orogen and the Jiyuan Basin constitute a basin-mountain system during the Early Mesozoic. Therefore, sediments from the Jiyuan Basin can be used to deduce the orogenic process of the Qinling Orogen. This paper attempts to use detrital zircon trace elements with ages ranging from the Late...
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Autor*in:	Wang Min [verfasserIn] Guo Wenfei [verfasserIn] Yang Wentao [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2019

Schlagwörter:	zircon basin-mountain interaction subduction-collision transition mianlve ocean

Übergeordnetes Werk:	In: Open Geosciences - De Gruyter, 2015, 11(2019), 1, Seite 125-139
Übergeordnetes Werk:	volume:11 ; year:2019 ; number:1 ; pages:125-139

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.1515/geo-2019-0011

Katalog-ID:	DOAJ058969977

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allfieldsSound	10.1515/geo-2019-0011 doi (DE-627)DOAJ058969977 (DE-599)DOAJ93c90ad75d5848a2b494aedfedfc8894 DE-627 ger DE-627 rakwb eng QE1-996.5 Wang Min verfasserin aut Detrital zircon trace elements from the Mesozoic Jiyuan Basin, central China and its implication on tectonic transition of the Qinling Orogenic Belt 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Qinling Orogen and the Jiyuan Basin constitute a basin-mountain system during the Early Mesozoic. Therefore, sediments from the Jiyuan Basin can be used to deduce the orogenic process of the Qinling Orogen. This paper attempts to use detrital zircon trace elements with ages ranging from the Late Carboniferous to the Middle Triassic that were obtained from the Jiyuan Basin to discuss the tectonic evolution of Qinling Orogen. On the tectonic setting discriminating diagrams, most grains are concentrated in convergent continental margins/orogenic settings,whereas the remaining samples (268 Ma, 265Ma, 264 Ma and 254Ma) are plotted in anorogenic field. Compared to the Early Paleozoic (400-500Ma) zircons, 306Ma and 281Ma grains represent higher Th/ Nb ratios, which might be related to the Mianlve oceanic crust subduction. The lower Th/Nb ratios containing 268 Ma, 265Ma, 264 Ma and 254Ma grains might indicate lithospheric extension subsequently. The final continent-continent collision between South China and North China blocks took place after the Middle Triassic (242Ma). zircon basin-mountain interaction subduction-collision transition mianlve ocean Geology Guo Wenfei verfasserin aut Yang Wentao verfasserin aut In Open Geosciences De Gruyter, 2015 11(2019), 1, Seite 125-139 (DE-627)804403066 (DE-600)2799881-2 23915447 nnns volume:11 year:2019 number:1 pages:125-139 https://doi.org/10.1515/geo-2019-0011 kostenfrei https://doaj.org/article/93c90ad75d5848a2b494aedfedfc8894 kostenfrei https://doi.org/10.1515/geo-2019-0011 kostenfrei https://doaj.org/toc/2391-5447 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_31 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_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 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 11 2019 1 125-139
language	English
source	In Open Geosciences 11(2019), 1, Seite 125-139 volume:11 year:2019 number:1 pages:125-139
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topic_facet	zircon basin-mountain interaction subduction-collision transition mianlve ocean Geology
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authorswithroles_txt_mv	Wang Min @@aut@@ Guo Wenfei @@aut@@ Yang Wentao @@aut@@
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callnumber-first	Q - Science
author	Wang Min
spellingShingle	Wang Min misc QE1-996.5 misc zircon misc basin-mountain interaction misc subduction-collision transition misc mianlve ocean misc Geology Detrital zircon trace elements from the Mesozoic Jiyuan Basin, central China and its implication on tectonic transition of the Qinling Orogenic Belt
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topic_title	QE1-996.5 Detrital zircon trace elements from the Mesozoic Jiyuan Basin, central China and its implication on tectonic transition of the Qinling Orogenic Belt zircon basin-mountain interaction subduction-collision transition mianlve ocean
topic	misc QE1-996.5 misc zircon misc basin-mountain interaction misc subduction-collision transition misc mianlve ocean misc Geology
topic_unstemmed	misc QE1-996.5 misc zircon misc basin-mountain interaction misc subduction-collision transition misc mianlve ocean misc Geology
topic_browse	misc QE1-996.5 misc zircon misc basin-mountain interaction misc subduction-collision transition misc mianlve ocean misc Geology
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title	Detrital zircon trace elements from the Mesozoic Jiyuan Basin, central China and its implication on tectonic transition of the Qinling Orogenic Belt
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title_full	Detrital zircon trace elements from the Mesozoic Jiyuan Basin, central China and its implication on tectonic transition of the Qinling Orogenic Belt
author_sort	Wang Min
journal	Open Geosciences
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title_sort	detrital zircon trace elements from the mesozoic jiyuan basin, central china and its implication on tectonic transition of the qinling orogenic belt
callnumber	QE1-996.5
title_auth	Detrital zircon trace elements from the Mesozoic Jiyuan Basin, central China and its implication on tectonic transition of the Qinling Orogenic Belt
abstract	The Qinling Orogen and the Jiyuan Basin constitute a basin-mountain system during the Early Mesozoic. Therefore, sediments from the Jiyuan Basin can be used to deduce the orogenic process of the Qinling Orogen. This paper attempts to use detrital zircon trace elements with ages ranging from the Late Carboniferous to the Middle Triassic that were obtained from the Jiyuan Basin to discuss the tectonic evolution of Qinling Orogen. On the tectonic setting discriminating diagrams, most grains are concentrated in convergent continental margins/orogenic settings,whereas the remaining samples (268 Ma, 265Ma, 264 Ma and 254Ma) are plotted in anorogenic field. Compared to the Early Paleozoic (400-500Ma) zircons, 306Ma and 281Ma grains represent higher Th/ Nb ratios, which might be related to the Mianlve oceanic crust subduction. The lower Th/Nb ratios containing 268 Ma, 265Ma, 264 Ma and 254Ma grains might indicate lithospheric extension subsequently. The final continent-continent collision between South China and North China blocks took place after the Middle Triassic (242Ma).
abstractGer	The Qinling Orogen and the Jiyuan Basin constitute a basin-mountain system during the Early Mesozoic. Therefore, sediments from the Jiyuan Basin can be used to deduce the orogenic process of the Qinling Orogen. This paper attempts to use detrital zircon trace elements with ages ranging from the Late Carboniferous to the Middle Triassic that were obtained from the Jiyuan Basin to discuss the tectonic evolution of Qinling Orogen. On the tectonic setting discriminating diagrams, most grains are concentrated in convergent continental margins/orogenic settings,whereas the remaining samples (268 Ma, 265Ma, 264 Ma and 254Ma) are plotted in anorogenic field. Compared to the Early Paleozoic (400-500Ma) zircons, 306Ma and 281Ma grains represent higher Th/ Nb ratios, which might be related to the Mianlve oceanic crust subduction. The lower Th/Nb ratios containing 268 Ma, 265Ma, 264 Ma and 254Ma grains might indicate lithospheric extension subsequently. The final continent-continent collision between South China and North China blocks took place after the Middle Triassic (242Ma).
abstract_unstemmed	The Qinling Orogen and the Jiyuan Basin constitute a basin-mountain system during the Early Mesozoic. Therefore, sediments from the Jiyuan Basin can be used to deduce the orogenic process of the Qinling Orogen. This paper attempts to use detrital zircon trace elements with ages ranging from the Late Carboniferous to the Middle Triassic that were obtained from the Jiyuan Basin to discuss the tectonic evolution of Qinling Orogen. On the tectonic setting discriminating diagrams, most grains are concentrated in convergent continental margins/orogenic settings,whereas the remaining samples (268 Ma, 265Ma, 264 Ma and 254Ma) are plotted in anorogenic field. Compared to the Early Paleozoic (400-500Ma) zircons, 306Ma and 281Ma grains represent higher Th/ Nb ratios, which might be related to the Mianlve oceanic crust subduction. The lower Th/Nb ratios containing 268 Ma, 265Ma, 264 Ma and 254Ma grains might indicate lithospheric extension subsequently. The final continent-continent collision between South China and North China blocks took place after the Middle Triassic (242Ma).
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title_short	Detrital zircon trace elements from the Mesozoic Jiyuan Basin, central China and its implication on tectonic transition of the Qinling Orogenic Belt
url	https://doi.org/10.1515/geo-2019-0011 https://doaj.org/article/93c90ad75d5848a2b494aedfedfc8894 https://doaj.org/toc/2391-5447
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up_date	2024-07-03T21:04:39.603Z
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Detrital zircon trace elements from the Mesozoic Jiyuan Basin, central China and its implication on tectonic transition of the Qinling Orogenic Belt

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