Transpressional uplift of Wensu Uplift in northern Tarim Basin, NW China: evidence from seismic profiles
The Wensu Uplift is an important structural belt in the northern Tarim Basin, NW China, always regarded as a thrust belt. However, this recognition is not only incompatible with the facts that synthetic and antithetic faults are equally developed in thrusting systems on the seismic profiles, but als...
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| Autor*in: |
Guangyu HE [verfasserIn] Yongqiang ZHAO [verfasserIn] Zewei YAO [verfasserIn] Xiaoli ZHENG [verfasserIn] Sidong XIAO [verfasserIn] Jiwen HUANG [verfasserIn] Cunshan JIA [verfasserIn] Yushuang ZHOU [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Chinesisch |
| Erschienen: |
2020 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
In: Shiyou shiyan dizhi - Editorial Office of Petroleum Geology and Experiment, 2024, 42(2020), 6, Seite 886-891 |
|---|---|
| Übergeordnetes Werk: |
volume:42 ; year:2020 ; number:6 ; pages:886-891 |
| Links: |
|---|
| DOI / URN: |
10.11781/sysydz202006886 |
|---|
| Katalog-ID: |
DOAJ095549811 |
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| 520 | |a The Wensu Uplift is an important structural belt in the northern Tarim Basin, NW China, always regarded as a thrust belt. However, this recognition is not only incompatible with the facts that synthetic and antithetic faults are equally developed in thrusting systems on the seismic profiles, but also contradictory with the changeable thrust directions of the main faults. Based on the high-resolution seismic profiles, strike-slip deformation happened in the Wensu Uplift. It is because: (1) Two large flower structures are developed on seismic profiles; (2) The main strike-slip faults named as the Shajingzi and Gumubiezi faults, which are the main faults of two large flower structures mentioned above, thrust violently southward in the eastern section and northward in the western section, respectively; (3) The pre-Mesozoic units in the Wensu Uplift are ancient Sinian-Cambrian strata, which thrust southward and northward over the Mesozoic-Cenozoic strata in the Awati and Wushi sags, respectively. The strike-slip activities happened during the middle Caledonian (the latest Ordovician), the late Caledonian (the latest Silurian), the early Hercynian (the latest Early-Middle Devonian), the late Hercynian (Late Permian), Indosinian-Yanshan (the latest Triassic and Late Cretaceous) and Himalayan period (Paleogene, Neogene and Quaternary). These results indicate that the Paleozoic is not a uniform tectonic-sedimentary environment in the northern Tarim Basin because of the Wensu Uplift barrier. | ||
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10.11781/sysydz202006886 doi (DE-627)DOAJ095549811 (DE-599)DOAJ51c9a9e326804e2e83a6197e914f069c DE-627 ger DE-627 rakwb chi QC801-809 QE1-996.5 Guangyu HE verfasserin aut Transpressional uplift of Wensu Uplift in northern Tarim Basin, NW China: evidence from seismic profiles 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Wensu Uplift is an important structural belt in the northern Tarim Basin, NW China, always regarded as a thrust belt. However, this recognition is not only incompatible with the facts that synthetic and antithetic faults are equally developed in thrusting systems on the seismic profiles, but also contradictory with the changeable thrust directions of the main faults. Based on the high-resolution seismic profiles, strike-slip deformation happened in the Wensu Uplift. It is because: (1) Two large flower structures are developed on seismic profiles; (2) The main strike-slip faults named as the Shajingzi and Gumubiezi faults, which are the main faults of two large flower structures mentioned above, thrust violently southward in the eastern section and northward in the western section, respectively; (3) The pre-Mesozoic units in the Wensu Uplift are ancient Sinian-Cambrian strata, which thrust southward and northward over the Mesozoic-Cenozoic strata in the Awati and Wushi sags, respectively. The strike-slip activities happened during the middle Caledonian (the latest Ordovician), the late Caledonian (the latest Silurian), the early Hercynian (the latest Early-Middle Devonian), the late Hercynian (Late Permian), Indosinian-Yanshan (the latest Triassic and Late Cretaceous) and Himalayan period (Paleogene, Neogene and Quaternary). These results indicate that the Paleozoic is not a uniform tectonic-sedimentary environment in the northern Tarim Basin because of the Wensu Uplift barrier. strike-slip deformation flower structure paleozoic wensu uplift tarim basin Geophysics. Cosmic physics Geology Yongqiang ZHAO verfasserin aut Zewei YAO verfasserin aut Xiaoli ZHENG verfasserin aut Sidong XIAO verfasserin aut Jiwen HUANG verfasserin aut Cunshan JIA verfasserin aut Yushuang ZHOU verfasserin aut In Shiyou shiyan dizhi Editorial Office of Petroleum Geology and Experiment, 2024 42(2020), 6, Seite 886-891 (DE-627)1681607743 (DE-600)2999009-9 10016112 nnns volume:42 year:2020 number:6 pages:886-891 https://doi.org/10.11781/sysydz202006886 kostenfrei https://doaj.org/article/51c9a9e326804e2e83a6197e914f069c kostenfrei https://www.sysydz.net/cn/article/doi/10.11781/sysydz202006886 kostenfrei https://doaj.org/toc/1001-6112 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_2817 AR 42 2020 6 886-891 |
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10.11781/sysydz202006886 doi (DE-627)DOAJ095549811 (DE-599)DOAJ51c9a9e326804e2e83a6197e914f069c DE-627 ger DE-627 rakwb chi QC801-809 QE1-996.5 Guangyu HE verfasserin aut Transpressional uplift of Wensu Uplift in northern Tarim Basin, NW China: evidence from seismic profiles 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Wensu Uplift is an important structural belt in the northern Tarim Basin, NW China, always regarded as a thrust belt. However, this recognition is not only incompatible with the facts that synthetic and antithetic faults are equally developed in thrusting systems on the seismic profiles, but also contradictory with the changeable thrust directions of the main faults. Based on the high-resolution seismic profiles, strike-slip deformation happened in the Wensu Uplift. It is because: (1) Two large flower structures are developed on seismic profiles; (2) The main strike-slip faults named as the Shajingzi and Gumubiezi faults, which are the main faults of two large flower structures mentioned above, thrust violently southward in the eastern section and northward in the western section, respectively; (3) The pre-Mesozoic units in the Wensu Uplift are ancient Sinian-Cambrian strata, which thrust southward and northward over the Mesozoic-Cenozoic strata in the Awati and Wushi sags, respectively. The strike-slip activities happened during the middle Caledonian (the latest Ordovician), the late Caledonian (the latest Silurian), the early Hercynian (the latest Early-Middle Devonian), the late Hercynian (Late Permian), Indosinian-Yanshan (the latest Triassic and Late Cretaceous) and Himalayan period (Paleogene, Neogene and Quaternary). These results indicate that the Paleozoic is not a uniform tectonic-sedimentary environment in the northern Tarim Basin because of the Wensu Uplift barrier. strike-slip deformation flower structure paleozoic wensu uplift tarim basin Geophysics. Cosmic physics Geology Yongqiang ZHAO verfasserin aut Zewei YAO verfasserin aut Xiaoli ZHENG verfasserin aut Sidong XIAO verfasserin aut Jiwen HUANG verfasserin aut Cunshan JIA verfasserin aut Yushuang ZHOU verfasserin aut In Shiyou shiyan dizhi Editorial Office of Petroleum Geology and Experiment, 2024 42(2020), 6, Seite 886-891 (DE-627)1681607743 (DE-600)2999009-9 10016112 nnns volume:42 year:2020 number:6 pages:886-891 https://doi.org/10.11781/sysydz202006886 kostenfrei https://doaj.org/article/51c9a9e326804e2e83a6197e914f069c kostenfrei https://www.sysydz.net/cn/article/doi/10.11781/sysydz202006886 kostenfrei https://doaj.org/toc/1001-6112 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_2817 AR 42 2020 6 886-891 |
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10.11781/sysydz202006886 doi (DE-627)DOAJ095549811 (DE-599)DOAJ51c9a9e326804e2e83a6197e914f069c DE-627 ger DE-627 rakwb chi QC801-809 QE1-996.5 Guangyu HE verfasserin aut Transpressional uplift of Wensu Uplift in northern Tarim Basin, NW China: evidence from seismic profiles 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Wensu Uplift is an important structural belt in the northern Tarim Basin, NW China, always regarded as a thrust belt. However, this recognition is not only incompatible with the facts that synthetic and antithetic faults are equally developed in thrusting systems on the seismic profiles, but also contradictory with the changeable thrust directions of the main faults. Based on the high-resolution seismic profiles, strike-slip deformation happened in the Wensu Uplift. It is because: (1) Two large flower structures are developed on seismic profiles; (2) The main strike-slip faults named as the Shajingzi and Gumubiezi faults, which are the main faults of two large flower structures mentioned above, thrust violently southward in the eastern section and northward in the western section, respectively; (3) The pre-Mesozoic units in the Wensu Uplift are ancient Sinian-Cambrian strata, which thrust southward and northward over the Mesozoic-Cenozoic strata in the Awati and Wushi sags, respectively. The strike-slip activities happened during the middle Caledonian (the latest Ordovician), the late Caledonian (the latest Silurian), the early Hercynian (the latest Early-Middle Devonian), the late Hercynian (Late Permian), Indosinian-Yanshan (the latest Triassic and Late Cretaceous) and Himalayan period (Paleogene, Neogene and Quaternary). These results indicate that the Paleozoic is not a uniform tectonic-sedimentary environment in the northern Tarim Basin because of the Wensu Uplift barrier. strike-slip deformation flower structure paleozoic wensu uplift tarim basin Geophysics. Cosmic physics Geology Yongqiang ZHAO verfasserin aut Zewei YAO verfasserin aut Xiaoli ZHENG verfasserin aut Sidong XIAO verfasserin aut Jiwen HUANG verfasserin aut Cunshan JIA verfasserin aut Yushuang ZHOU verfasserin aut In Shiyou shiyan dizhi Editorial Office of Petroleum Geology and Experiment, 2024 42(2020), 6, Seite 886-891 (DE-627)1681607743 (DE-600)2999009-9 10016112 nnns volume:42 year:2020 number:6 pages:886-891 https://doi.org/10.11781/sysydz202006886 kostenfrei https://doaj.org/article/51c9a9e326804e2e83a6197e914f069c kostenfrei https://www.sysydz.net/cn/article/doi/10.11781/sysydz202006886 kostenfrei https://doaj.org/toc/1001-6112 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_2817 AR 42 2020 6 886-891 |
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10.11781/sysydz202006886 doi (DE-627)DOAJ095549811 (DE-599)DOAJ51c9a9e326804e2e83a6197e914f069c DE-627 ger DE-627 rakwb chi QC801-809 QE1-996.5 Guangyu HE verfasserin aut Transpressional uplift of Wensu Uplift in northern Tarim Basin, NW China: evidence from seismic profiles 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Wensu Uplift is an important structural belt in the northern Tarim Basin, NW China, always regarded as a thrust belt. However, this recognition is not only incompatible with the facts that synthetic and antithetic faults are equally developed in thrusting systems on the seismic profiles, but also contradictory with the changeable thrust directions of the main faults. Based on the high-resolution seismic profiles, strike-slip deformation happened in the Wensu Uplift. It is because: (1) Two large flower structures are developed on seismic profiles; (2) The main strike-slip faults named as the Shajingzi and Gumubiezi faults, which are the main faults of two large flower structures mentioned above, thrust violently southward in the eastern section and northward in the western section, respectively; (3) The pre-Mesozoic units in the Wensu Uplift are ancient Sinian-Cambrian strata, which thrust southward and northward over the Mesozoic-Cenozoic strata in the Awati and Wushi sags, respectively. The strike-slip activities happened during the middle Caledonian (the latest Ordovician), the late Caledonian (the latest Silurian), the early Hercynian (the latest Early-Middle Devonian), the late Hercynian (Late Permian), Indosinian-Yanshan (the latest Triassic and Late Cretaceous) and Himalayan period (Paleogene, Neogene and Quaternary). These results indicate that the Paleozoic is not a uniform tectonic-sedimentary environment in the northern Tarim Basin because of the Wensu Uplift barrier. strike-slip deformation flower structure paleozoic wensu uplift tarim basin Geophysics. Cosmic physics Geology Yongqiang ZHAO verfasserin aut Zewei YAO verfasserin aut Xiaoli ZHENG verfasserin aut Sidong XIAO verfasserin aut Jiwen HUANG verfasserin aut Cunshan JIA verfasserin aut Yushuang ZHOU verfasserin aut In Shiyou shiyan dizhi Editorial Office of Petroleum Geology and Experiment, 2024 42(2020), 6, Seite 886-891 (DE-627)1681607743 (DE-600)2999009-9 10016112 nnns volume:42 year:2020 number:6 pages:886-891 https://doi.org/10.11781/sysydz202006886 kostenfrei https://doaj.org/article/51c9a9e326804e2e83a6197e914f069c kostenfrei https://www.sysydz.net/cn/article/doi/10.11781/sysydz202006886 kostenfrei https://doaj.org/toc/1001-6112 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_2817 AR 42 2020 6 886-891 |
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10.11781/sysydz202006886 doi (DE-627)DOAJ095549811 (DE-599)DOAJ51c9a9e326804e2e83a6197e914f069c DE-627 ger DE-627 rakwb chi QC801-809 QE1-996.5 Guangyu HE verfasserin aut Transpressional uplift of Wensu Uplift in northern Tarim Basin, NW China: evidence from seismic profiles 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The Wensu Uplift is an important structural belt in the northern Tarim Basin, NW China, always regarded as a thrust belt. However, this recognition is not only incompatible with the facts that synthetic and antithetic faults are equally developed in thrusting systems on the seismic profiles, but also contradictory with the changeable thrust directions of the main faults. Based on the high-resolution seismic profiles, strike-slip deformation happened in the Wensu Uplift. It is because: (1) Two large flower structures are developed on seismic profiles; (2) The main strike-slip faults named as the Shajingzi and Gumubiezi faults, which are the main faults of two large flower structures mentioned above, thrust violently southward in the eastern section and northward in the western section, respectively; (3) The pre-Mesozoic units in the Wensu Uplift are ancient Sinian-Cambrian strata, which thrust southward and northward over the Mesozoic-Cenozoic strata in the Awati and Wushi sags, respectively. The strike-slip activities happened during the middle Caledonian (the latest Ordovician), the late Caledonian (the latest Silurian), the early Hercynian (the latest Early-Middle Devonian), the late Hercynian (Late Permian), Indosinian-Yanshan (the latest Triassic and Late Cretaceous) and Himalayan period (Paleogene, Neogene and Quaternary). These results indicate that the Paleozoic is not a uniform tectonic-sedimentary environment in the northern Tarim Basin because of the Wensu Uplift barrier. strike-slip deformation flower structure paleozoic wensu uplift tarim basin Geophysics. Cosmic physics Geology Yongqiang ZHAO verfasserin aut Zewei YAO verfasserin aut Xiaoli ZHENG verfasserin aut Sidong XIAO verfasserin aut Jiwen HUANG verfasserin aut Cunshan JIA verfasserin aut Yushuang ZHOU verfasserin aut In Shiyou shiyan dizhi Editorial Office of Petroleum Geology and Experiment, 2024 42(2020), 6, Seite 886-891 (DE-627)1681607743 (DE-600)2999009-9 10016112 nnns volume:42 year:2020 number:6 pages:886-891 https://doi.org/10.11781/sysydz202006886 kostenfrei https://doaj.org/article/51c9a9e326804e2e83a6197e914f069c kostenfrei https://www.sysydz.net/cn/article/doi/10.11781/sysydz202006886 kostenfrei https://doaj.org/toc/1001-6112 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_2817 AR 42 2020 6 886-891 |
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QC801-809 QE1-996.5 Transpressional uplift of Wensu Uplift in northern Tarim Basin, NW China: evidence from seismic profiles strike-slip deformation flower structure paleozoic wensu uplift tarim basin |
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transpressional uplift of wensu uplift in northern tarim basin, nw china: evidence from seismic profiles |
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Transpressional uplift of Wensu Uplift in northern Tarim Basin, NW China: evidence from seismic profiles |
| abstract |
The Wensu Uplift is an important structural belt in the northern Tarim Basin, NW China, always regarded as a thrust belt. However, this recognition is not only incompatible with the facts that synthetic and antithetic faults are equally developed in thrusting systems on the seismic profiles, but also contradictory with the changeable thrust directions of the main faults. Based on the high-resolution seismic profiles, strike-slip deformation happened in the Wensu Uplift. It is because: (1) Two large flower structures are developed on seismic profiles; (2) The main strike-slip faults named as the Shajingzi and Gumubiezi faults, which are the main faults of two large flower structures mentioned above, thrust violently southward in the eastern section and northward in the western section, respectively; (3) The pre-Mesozoic units in the Wensu Uplift are ancient Sinian-Cambrian strata, which thrust southward and northward over the Mesozoic-Cenozoic strata in the Awati and Wushi sags, respectively. The strike-slip activities happened during the middle Caledonian (the latest Ordovician), the late Caledonian (the latest Silurian), the early Hercynian (the latest Early-Middle Devonian), the late Hercynian (Late Permian), Indosinian-Yanshan (the latest Triassic and Late Cretaceous) and Himalayan period (Paleogene, Neogene and Quaternary). These results indicate that the Paleozoic is not a uniform tectonic-sedimentary environment in the northern Tarim Basin because of the Wensu Uplift barrier. |
| abstractGer |
The Wensu Uplift is an important structural belt in the northern Tarim Basin, NW China, always regarded as a thrust belt. However, this recognition is not only incompatible with the facts that synthetic and antithetic faults are equally developed in thrusting systems on the seismic profiles, but also contradictory with the changeable thrust directions of the main faults. Based on the high-resolution seismic profiles, strike-slip deformation happened in the Wensu Uplift. It is because: (1) Two large flower structures are developed on seismic profiles; (2) The main strike-slip faults named as the Shajingzi and Gumubiezi faults, which are the main faults of two large flower structures mentioned above, thrust violently southward in the eastern section and northward in the western section, respectively; (3) The pre-Mesozoic units in the Wensu Uplift are ancient Sinian-Cambrian strata, which thrust southward and northward over the Mesozoic-Cenozoic strata in the Awati and Wushi sags, respectively. The strike-slip activities happened during the middle Caledonian (the latest Ordovician), the late Caledonian (the latest Silurian), the early Hercynian (the latest Early-Middle Devonian), the late Hercynian (Late Permian), Indosinian-Yanshan (the latest Triassic and Late Cretaceous) and Himalayan period (Paleogene, Neogene and Quaternary). These results indicate that the Paleozoic is not a uniform tectonic-sedimentary environment in the northern Tarim Basin because of the Wensu Uplift barrier. |
| abstract_unstemmed |
The Wensu Uplift is an important structural belt in the northern Tarim Basin, NW China, always regarded as a thrust belt. However, this recognition is not only incompatible with the facts that synthetic and antithetic faults are equally developed in thrusting systems on the seismic profiles, but also contradictory with the changeable thrust directions of the main faults. Based on the high-resolution seismic profiles, strike-slip deformation happened in the Wensu Uplift. It is because: (1) Two large flower structures are developed on seismic profiles; (2) The main strike-slip faults named as the Shajingzi and Gumubiezi faults, which are the main faults of two large flower structures mentioned above, thrust violently southward in the eastern section and northward in the western section, respectively; (3) The pre-Mesozoic units in the Wensu Uplift are ancient Sinian-Cambrian strata, which thrust southward and northward over the Mesozoic-Cenozoic strata in the Awati and Wushi sags, respectively. The strike-slip activities happened during the middle Caledonian (the latest Ordovician), the late Caledonian (the latest Silurian), the early Hercynian (the latest Early-Middle Devonian), the late Hercynian (Late Permian), Indosinian-Yanshan (the latest Triassic and Late Cretaceous) and Himalayan period (Paleogene, Neogene and Quaternary). These results indicate that the Paleozoic is not a uniform tectonic-sedimentary environment in the northern Tarim Basin because of the Wensu Uplift barrier. |
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Transpressional uplift of Wensu Uplift in northern Tarim Basin, NW China: evidence from seismic profiles |
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