Palaeogene structural evolution of Dongying Depression, Bohai Bay Basin, NE China
Based on the new all-covering 3D seismic data and the drilling-logging data, we established the sequence stratigraphic framework for Dongying Depression and identified two kinds of structural systems in Palaeogene, i.e. the extensional structural system and the transtensional structural system. The...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Chen, Shuguang [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2017 |
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| Rechteinformationen: |
Nutzungsrecht: © 2016 Informa UK Limited, trading as Taylor & Francis Group 2016 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: International geology review - London [u.a.] : Taylor & Francis, 1959, 59(2017), 3, Seite 259-273 |
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| Übergeordnetes Werk: |
volume:59 ; year:2017 ; number:3 ; pages:259-273 |
| Links: |
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| DOI / URN: |
10.1080/00206814.2016.1223559 |
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OLC1987078489 |
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| 520 | |a Based on the new all-covering 3D seismic data and the drilling-logging data, we established the sequence stratigraphic framework for Dongying Depression and identified two kinds of structural systems in Palaeogene, i.e. the extensional structural system and the transtensional structural system. The extensional structural system consists of different normal faults that predominantly trend NE, EW, and NW. The attitudes of the normal faults vary in different tectonic settings. However, the transtensional structural system consists of some strike-slip faults and some normal faults. According to the analysis of the relationships between the faults and the sedimentary sequences of Dongying Depression, we considered that the extensional structural system was developed mainly from the Palaeocene to the middle Eocene, whereas the transtensional structural system was mostly developed from the middle Eocene to the Oligocene. In addition, we found that the structural systems had transformed since 43.5 Ma, when the subduction direction and activity rates of the Pacific Plate changed and the dextral strike-slip movement of the large-scale Tanlu fault zone started from eastern China. The extensional structural deformation was probably derived from the back-arc extension triggered by subduction rollback of the Pacific Plate under the Eurasian Plate, whereas the transtensional structural deformation was probably related to the regional dextral strike-slip movement induced by the subduction of the Pacific Plate and the continents' collision between the Indian Plate and the Eurasian Plate. | ||
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| 650 | 4 | |a transtensional structure | |
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| 650 | 4 | |a Dongying Depression | |
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10.1080/00206814.2016.1223559 doi PQ20170301 (DE-627)OLC1987078489 (DE-599)GBVOLC1987078489 (PRQ)c1549-86c49585e9c606dd04bbbd5e04115c4d87250867a31f1904cbde7bd109b511fe0 (KEY)0015883620170000059000300259palaeogenestructuralevolutionofdongyingdepressionb DE-627 ger DE-627 rakwb eng 550 ZDB Chen, Shuguang verfasserin aut Palaeogene structural evolution of Dongying Depression, Bohai Bay Basin, NE China 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Based on the new all-covering 3D seismic data and the drilling-logging data, we established the sequence stratigraphic framework for Dongying Depression and identified two kinds of structural systems in Palaeogene, i.e. the extensional structural system and the transtensional structural system. The extensional structural system consists of different normal faults that predominantly trend NE, EW, and NW. The attitudes of the normal faults vary in different tectonic settings. However, the transtensional structural system consists of some strike-slip faults and some normal faults. According to the analysis of the relationships between the faults and the sedimentary sequences of Dongying Depression, we considered that the extensional structural system was developed mainly from the Palaeocene to the middle Eocene, whereas the transtensional structural system was mostly developed from the middle Eocene to the Oligocene. In addition, we found that the structural systems had transformed since 43.5 Ma, when the subduction direction and activity rates of the Pacific Plate changed and the dextral strike-slip movement of the large-scale Tanlu fault zone started from eastern China. The extensional structural deformation was probably derived from the back-arc extension triggered by subduction rollback of the Pacific Plate under the Eurasian Plate, whereas the transtensional structural deformation was probably related to the regional dextral strike-slip movement induced by the subduction of the Pacific Plate and the continents' collision between the Indian Plate and the Eurasian Plate. Nutzungsrecht: © 2016 Informa UK Limited, trading as Taylor & Francis Group 2016 structural system extensional structure transtensional structure dynamic background Dongying Depression Liu, Xiaofeng oth Cui, Yongqian oth Zhao, Xianzheng oth Zhang, Jianli oth Enthalten in International geology review London [u.a.] : Taylor & Francis, 1959 59(2017), 3, Seite 259-273 (DE-627)129358800 (DE-600)160473-9 (DE-576)014731126 0020-6814 nnns volume:59 year:2017 number:3 pages:259-273 http://dx.doi.org/10.1080/00206814.2016.1223559 Volltext http://www.tandfonline.com/doi/abs/10.1080/00206814.2016.1223559 http://search.proquest.com/docview/1859445578 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_70 AR 59 2017 3 259-273 |
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10.1080/00206814.2016.1223559 doi PQ20170301 (DE-627)OLC1987078489 (DE-599)GBVOLC1987078489 (PRQ)c1549-86c49585e9c606dd04bbbd5e04115c4d87250867a31f1904cbde7bd109b511fe0 (KEY)0015883620170000059000300259palaeogenestructuralevolutionofdongyingdepressionb DE-627 ger DE-627 rakwb eng 550 ZDB Chen, Shuguang verfasserin aut Palaeogene structural evolution of Dongying Depression, Bohai Bay Basin, NE China 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Based on the new all-covering 3D seismic data and the drilling-logging data, we established the sequence stratigraphic framework for Dongying Depression and identified two kinds of structural systems in Palaeogene, i.e. the extensional structural system and the transtensional structural system. The extensional structural system consists of different normal faults that predominantly trend NE, EW, and NW. The attitudes of the normal faults vary in different tectonic settings. However, the transtensional structural system consists of some strike-slip faults and some normal faults. According to the analysis of the relationships between the faults and the sedimentary sequences of Dongying Depression, we considered that the extensional structural system was developed mainly from the Palaeocene to the middle Eocene, whereas the transtensional structural system was mostly developed from the middle Eocene to the Oligocene. In addition, we found that the structural systems had transformed since 43.5 Ma, when the subduction direction and activity rates of the Pacific Plate changed and the dextral strike-slip movement of the large-scale Tanlu fault zone started from eastern China. The extensional structural deformation was probably derived from the back-arc extension triggered by subduction rollback of the Pacific Plate under the Eurasian Plate, whereas the transtensional structural deformation was probably related to the regional dextral strike-slip movement induced by the subduction of the Pacific Plate and the continents' collision between the Indian Plate and the Eurasian Plate. Nutzungsrecht: © 2016 Informa UK Limited, trading as Taylor & Francis Group 2016 structural system extensional structure transtensional structure dynamic background Dongying Depression Liu, Xiaofeng oth Cui, Yongqian oth Zhao, Xianzheng oth Zhang, Jianli oth Enthalten in International geology review London [u.a.] : Taylor & Francis, 1959 59(2017), 3, Seite 259-273 (DE-627)129358800 (DE-600)160473-9 (DE-576)014731126 0020-6814 nnns volume:59 year:2017 number:3 pages:259-273 http://dx.doi.org/10.1080/00206814.2016.1223559 Volltext http://www.tandfonline.com/doi/abs/10.1080/00206814.2016.1223559 http://search.proquest.com/docview/1859445578 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_70 AR 59 2017 3 259-273 |
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10.1080/00206814.2016.1223559 doi PQ20170301 (DE-627)OLC1987078489 (DE-599)GBVOLC1987078489 (PRQ)c1549-86c49585e9c606dd04bbbd5e04115c4d87250867a31f1904cbde7bd109b511fe0 (KEY)0015883620170000059000300259palaeogenestructuralevolutionofdongyingdepressionb DE-627 ger DE-627 rakwb eng 550 ZDB Chen, Shuguang verfasserin aut Palaeogene structural evolution of Dongying Depression, Bohai Bay Basin, NE China 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Based on the new all-covering 3D seismic data and the drilling-logging data, we established the sequence stratigraphic framework for Dongying Depression and identified two kinds of structural systems in Palaeogene, i.e. the extensional structural system and the transtensional structural system. The extensional structural system consists of different normal faults that predominantly trend NE, EW, and NW. The attitudes of the normal faults vary in different tectonic settings. However, the transtensional structural system consists of some strike-slip faults and some normal faults. According to the analysis of the relationships between the faults and the sedimentary sequences of Dongying Depression, we considered that the extensional structural system was developed mainly from the Palaeocene to the middle Eocene, whereas the transtensional structural system was mostly developed from the middle Eocene to the Oligocene. In addition, we found that the structural systems had transformed since 43.5 Ma, when the subduction direction and activity rates of the Pacific Plate changed and the dextral strike-slip movement of the large-scale Tanlu fault zone started from eastern China. The extensional structural deformation was probably derived from the back-arc extension triggered by subduction rollback of the Pacific Plate under the Eurasian Plate, whereas the transtensional structural deformation was probably related to the regional dextral strike-slip movement induced by the subduction of the Pacific Plate and the continents' collision between the Indian Plate and the Eurasian Plate. Nutzungsrecht: © 2016 Informa UK Limited, trading as Taylor & Francis Group 2016 structural system extensional structure transtensional structure dynamic background Dongying Depression Liu, Xiaofeng oth Cui, Yongqian oth Zhao, Xianzheng oth Zhang, Jianli oth Enthalten in International geology review London [u.a.] : Taylor & Francis, 1959 59(2017), 3, Seite 259-273 (DE-627)129358800 (DE-600)160473-9 (DE-576)014731126 0020-6814 nnns volume:59 year:2017 number:3 pages:259-273 http://dx.doi.org/10.1080/00206814.2016.1223559 Volltext http://www.tandfonline.com/doi/abs/10.1080/00206814.2016.1223559 http://search.proquest.com/docview/1859445578 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_70 AR 59 2017 3 259-273 |
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10.1080/00206814.2016.1223559 doi PQ20170301 (DE-627)OLC1987078489 (DE-599)GBVOLC1987078489 (PRQ)c1549-86c49585e9c606dd04bbbd5e04115c4d87250867a31f1904cbde7bd109b511fe0 (KEY)0015883620170000059000300259palaeogenestructuralevolutionofdongyingdepressionb DE-627 ger DE-627 rakwb eng 550 ZDB Chen, Shuguang verfasserin aut Palaeogene structural evolution of Dongying Depression, Bohai Bay Basin, NE China 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Based on the new all-covering 3D seismic data and the drilling-logging data, we established the sequence stratigraphic framework for Dongying Depression and identified two kinds of structural systems in Palaeogene, i.e. the extensional structural system and the transtensional structural system. The extensional structural system consists of different normal faults that predominantly trend NE, EW, and NW. The attitudes of the normal faults vary in different tectonic settings. However, the transtensional structural system consists of some strike-slip faults and some normal faults. According to the analysis of the relationships between the faults and the sedimentary sequences of Dongying Depression, we considered that the extensional structural system was developed mainly from the Palaeocene to the middle Eocene, whereas the transtensional structural system was mostly developed from the middle Eocene to the Oligocene. In addition, we found that the structural systems had transformed since 43.5 Ma, when the subduction direction and activity rates of the Pacific Plate changed and the dextral strike-slip movement of the large-scale Tanlu fault zone started from eastern China. The extensional structural deformation was probably derived from the back-arc extension triggered by subduction rollback of the Pacific Plate under the Eurasian Plate, whereas the transtensional structural deformation was probably related to the regional dextral strike-slip movement induced by the subduction of the Pacific Plate and the continents' collision between the Indian Plate and the Eurasian Plate. Nutzungsrecht: © 2016 Informa UK Limited, trading as Taylor & Francis Group 2016 structural system extensional structure transtensional structure dynamic background Dongying Depression Liu, Xiaofeng oth Cui, Yongqian oth Zhao, Xianzheng oth Zhang, Jianli oth Enthalten in International geology review London [u.a.] : Taylor & Francis, 1959 59(2017), 3, Seite 259-273 (DE-627)129358800 (DE-600)160473-9 (DE-576)014731126 0020-6814 nnns volume:59 year:2017 number:3 pages:259-273 http://dx.doi.org/10.1080/00206814.2016.1223559 Volltext http://www.tandfonline.com/doi/abs/10.1080/00206814.2016.1223559 http://search.proquest.com/docview/1859445578 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_70 AR 59 2017 3 259-273 |
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10.1080/00206814.2016.1223559 doi PQ20170301 (DE-627)OLC1987078489 (DE-599)GBVOLC1987078489 (PRQ)c1549-86c49585e9c606dd04bbbd5e04115c4d87250867a31f1904cbde7bd109b511fe0 (KEY)0015883620170000059000300259palaeogenestructuralevolutionofdongyingdepressionb DE-627 ger DE-627 rakwb eng 550 ZDB Chen, Shuguang verfasserin aut Palaeogene structural evolution of Dongying Depression, Bohai Bay Basin, NE China 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Based on the new all-covering 3D seismic data and the drilling-logging data, we established the sequence stratigraphic framework for Dongying Depression and identified two kinds of structural systems in Palaeogene, i.e. the extensional structural system and the transtensional structural system. The extensional structural system consists of different normal faults that predominantly trend NE, EW, and NW. The attitudes of the normal faults vary in different tectonic settings. However, the transtensional structural system consists of some strike-slip faults and some normal faults. According to the analysis of the relationships between the faults and the sedimentary sequences of Dongying Depression, we considered that the extensional structural system was developed mainly from the Palaeocene to the middle Eocene, whereas the transtensional structural system was mostly developed from the middle Eocene to the Oligocene. In addition, we found that the structural systems had transformed since 43.5 Ma, when the subduction direction and activity rates of the Pacific Plate changed and the dextral strike-slip movement of the large-scale Tanlu fault zone started from eastern China. The extensional structural deformation was probably derived from the back-arc extension triggered by subduction rollback of the Pacific Plate under the Eurasian Plate, whereas the transtensional structural deformation was probably related to the regional dextral strike-slip movement induced by the subduction of the Pacific Plate and the continents' collision between the Indian Plate and the Eurasian Plate. Nutzungsrecht: © 2016 Informa UK Limited, trading as Taylor & Francis Group 2016 structural system extensional structure transtensional structure dynamic background Dongying Depression Liu, Xiaofeng oth Cui, Yongqian oth Zhao, Xianzheng oth Zhang, Jianli oth Enthalten in International geology review London [u.a.] : Taylor & Francis, 1959 59(2017), 3, Seite 259-273 (DE-627)129358800 (DE-600)160473-9 (DE-576)014731126 0020-6814 nnns volume:59 year:2017 number:3 pages:259-273 http://dx.doi.org/10.1080/00206814.2016.1223559 Volltext http://www.tandfonline.com/doi/abs/10.1080/00206814.2016.1223559 http://search.proquest.com/docview/1859445578 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_70 AR 59 2017 3 259-273 |
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Palaeogene structural evolution of Dongying Depression, Bohai Bay Basin, NE China |
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palaeogene structural evolution of dongying depression, bohai bay basin, ne china |
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Palaeogene structural evolution of Dongying Depression, Bohai Bay Basin, NE China |
| abstract |
Based on the new all-covering 3D seismic data and the drilling-logging data, we established the sequence stratigraphic framework for Dongying Depression and identified two kinds of structural systems in Palaeogene, i.e. the extensional structural system and the transtensional structural system. The extensional structural system consists of different normal faults that predominantly trend NE, EW, and NW. The attitudes of the normal faults vary in different tectonic settings. However, the transtensional structural system consists of some strike-slip faults and some normal faults. According to the analysis of the relationships between the faults and the sedimentary sequences of Dongying Depression, we considered that the extensional structural system was developed mainly from the Palaeocene to the middle Eocene, whereas the transtensional structural system was mostly developed from the middle Eocene to the Oligocene. In addition, we found that the structural systems had transformed since 43.5 Ma, when the subduction direction and activity rates of the Pacific Plate changed and the dextral strike-slip movement of the large-scale Tanlu fault zone started from eastern China. The extensional structural deformation was probably derived from the back-arc extension triggered by subduction rollback of the Pacific Plate under the Eurasian Plate, whereas the transtensional structural deformation was probably related to the regional dextral strike-slip movement induced by the subduction of the Pacific Plate and the continents' collision between the Indian Plate and the Eurasian Plate. |
| abstractGer |
Based on the new all-covering 3D seismic data and the drilling-logging data, we established the sequence stratigraphic framework for Dongying Depression and identified two kinds of structural systems in Palaeogene, i.e. the extensional structural system and the transtensional structural system. The extensional structural system consists of different normal faults that predominantly trend NE, EW, and NW. The attitudes of the normal faults vary in different tectonic settings. However, the transtensional structural system consists of some strike-slip faults and some normal faults. According to the analysis of the relationships between the faults and the sedimentary sequences of Dongying Depression, we considered that the extensional structural system was developed mainly from the Palaeocene to the middle Eocene, whereas the transtensional structural system was mostly developed from the middle Eocene to the Oligocene. In addition, we found that the structural systems had transformed since 43.5 Ma, when the subduction direction and activity rates of the Pacific Plate changed and the dextral strike-slip movement of the large-scale Tanlu fault zone started from eastern China. The extensional structural deformation was probably derived from the back-arc extension triggered by subduction rollback of the Pacific Plate under the Eurasian Plate, whereas the transtensional structural deformation was probably related to the regional dextral strike-slip movement induced by the subduction of the Pacific Plate and the continents' collision between the Indian Plate and the Eurasian Plate. |
| abstract_unstemmed |
Based on the new all-covering 3D seismic data and the drilling-logging data, we established the sequence stratigraphic framework for Dongying Depression and identified two kinds of structural systems in Palaeogene, i.e. the extensional structural system and the transtensional structural system. The extensional structural system consists of different normal faults that predominantly trend NE, EW, and NW. The attitudes of the normal faults vary in different tectonic settings. However, the transtensional structural system consists of some strike-slip faults and some normal faults. According to the analysis of the relationships between the faults and the sedimentary sequences of Dongying Depression, we considered that the extensional structural system was developed mainly from the Palaeocene to the middle Eocene, whereas the transtensional structural system was mostly developed from the middle Eocene to the Oligocene. In addition, we found that the structural systems had transformed since 43.5 Ma, when the subduction direction and activity rates of the Pacific Plate changed and the dextral strike-slip movement of the large-scale Tanlu fault zone started from eastern China. The extensional structural deformation was probably derived from the back-arc extension triggered by subduction rollback of the Pacific Plate under the Eurasian Plate, whereas the transtensional structural deformation was probably related to the regional dextral strike-slip movement induced by the subduction of the Pacific Plate and the continents' collision between the Indian Plate and the Eurasian Plate. |
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Palaeogene structural evolution of Dongying Depression, Bohai Bay Basin, NE China |
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