Mesozoic structural evolution of the Hangjinqi area in the northern Ordos Basin, North China
This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfac...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Yang, Minghui [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015transfer abstract |
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| Schlagwörter: |
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| Umfang: |
16 |
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| Übergeordnetes Werk: |
Enthalten in: Honesty-Humility and unethical behavior in adolescents: The mediating role of moral disengagement and the moderating role of system justification - Guo, Zhen ELSEVIER, 2021, Amsterdam [u.a.] |
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| Übergeordnetes Werk: |
volume:66 ; year:2015 ; pages:695-710 ; extent:16 |
| Links: |
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| DOI / URN: |
10.1016/j.marpetgeo.2015.07.014 |
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ELV018371345 |
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| 520 | |a This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfaces have been recognized overlying a paleoslope surface (T9) in this area: (1) The Late Carboniferous-Permian and Triassic tectonic sequence (TS-1); sedimentation of the lowest part of this succession is strongly controlled by the Hangjinqi Fault Zone (HFZ), whereas the rest of the sequence indicates much less fault control; (2) the Middle Jurassic tectonic sequence (TS-2); (3) the Late Early Cretaceous tectonic sequence (TS-3); and the TS-2 and TS-3 sequences are more extensive than the TS-1 sequence throughout the Hangjinqi area. The structural framework displayed by the TS-2 sequence is very different from that displayed by the TS-3 sequence. More specifically, the general structure beneath the unconformity (T3) between the Late Jurassic strata and the Early Cretaceous strata consists of an E–W trending transtensional fault system. This resulted from a multi-stage dextral phase, which was caused by oblique subduction of the Paleo-Pacific Plate under the Eurasian Plate and dextral movement of the HFZ, and a subsequent inversion event, which caused significant reverse movement along previous transtensional structures. The study area, which underlies the unconformity (T2) between the Late Jurassic strata and the Early Cretaceous strata, has been deformed since the Late Cretaceous, when tectonic inversion occurred, possibly due to changes in the strike-slip motion, from dextral-to sinistral, of the HFZ. Late Cretaceous erosion was responsible for an important and unequal denudation. The timing of the transition from extension to uplift cannot be determined due to continuous erosion, but this uplift finally marked the end of the structural evolution of the Hanjinqi area and even the Ordos Basin. | ||
| 520 | |a This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfaces have been recognized overlying a paleoslope surface (T9) in this area: (1) The Late Carboniferous-Permian and Triassic tectonic sequence (TS-1); sedimentation of the lowest part of this succession is strongly controlled by the Hangjinqi Fault Zone (HFZ), whereas the rest of the sequence indicates much less fault control; (2) the Middle Jurassic tectonic sequence (TS-2); (3) the Late Early Cretaceous tectonic sequence (TS-3); and the TS-2 and TS-3 sequences are more extensive than the TS-1 sequence throughout the Hangjinqi area. The structural framework displayed by the TS-2 sequence is very different from that displayed by the TS-3 sequence. More specifically, the general structure beneath the unconformity (T3) between the Late Jurassic strata and the Early Cretaceous strata consists of an E–W trending transtensional fault system. This resulted from a multi-stage dextral phase, which was caused by oblique subduction of the Paleo-Pacific Plate under the Eurasian Plate and dextral movement of the HFZ, and a subsequent inversion event, which caused significant reverse movement along previous transtensional structures. The study area, which underlies the unconformity (T2) between the Late Jurassic strata and the Early Cretaceous strata, has been deformed since the Late Cretaceous, when tectonic inversion occurred, possibly due to changes in the strike-slip motion, from dextral-to sinistral, of the HFZ. Late Cretaceous erosion was responsible for an important and unequal denudation. The timing of the transition from extension to uplift cannot be determined due to continuous erosion, but this uplift finally marked the end of the structural evolution of the Hanjinqi area and even the Ordos Basin. | ||
| 650 | 7 | |a Hangjinqi area |2 Elsevier | |
| 650 | 7 | |a Mesozoic |2 Elsevier | |
| 650 | 7 | |a Structural evolution |2 Elsevier | |
| 650 | 7 | |a Ordos Basin |2 Elsevier | |
| 650 | 7 | |a Uplift and erosion |2 Elsevier | |
| 650 | 7 | |a Inversion |2 Elsevier | |
| 700 | 1 | |a Li, Liang |4 oth | |
| 700 | 1 | |a Zhou, Jin |4 oth | |
| 700 | 1 | |a Jia, Huichong |4 oth | |
| 700 | 1 | |a Sun, Xiao |4 oth | |
| 700 | 1 | |a Qu, Xiaoyan |4 oth | |
| 700 | 1 | |a Zhou, Duo |4 oth | |
| 700 | 1 | |a Gong, Ting |4 oth | |
| 700 | 1 | |a Ding, Chao |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |n Elsevier Science |a Guo, Zhen ELSEVIER |t Honesty-Humility and unethical behavior in adolescents: The mediating role of moral disengagement and the moderating role of system justification |d 2021 |g Amsterdam [u.a.] |w (DE-627)ELV006295584 |
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10.1016/j.marpetgeo.2015.07.014 doi GBVA2015008000007.pica (DE-627)ELV018371345 (ELSEVIER)S0264-8172(15)30035-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 44.67 bkl Yang, Minghui verfasserin aut Mesozoic structural evolution of the Hangjinqi area in the northern Ordos Basin, North China 2015transfer abstract 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfaces have been recognized overlying a paleoslope surface (T9) in this area: (1) The Late Carboniferous-Permian and Triassic tectonic sequence (TS-1); sedimentation of the lowest part of this succession is strongly controlled by the Hangjinqi Fault Zone (HFZ), whereas the rest of the sequence indicates much less fault control; (2) the Middle Jurassic tectonic sequence (TS-2); (3) the Late Early Cretaceous tectonic sequence (TS-3); and the TS-2 and TS-3 sequences are more extensive than the TS-1 sequence throughout the Hangjinqi area. The structural framework displayed by the TS-2 sequence is very different from that displayed by the TS-3 sequence. More specifically, the general structure beneath the unconformity (T3) between the Late Jurassic strata and the Early Cretaceous strata consists of an E–W trending transtensional fault system. This resulted from a multi-stage dextral phase, which was caused by oblique subduction of the Paleo-Pacific Plate under the Eurasian Plate and dextral movement of the HFZ, and a subsequent inversion event, which caused significant reverse movement along previous transtensional structures. The study area, which underlies the unconformity (T2) between the Late Jurassic strata and the Early Cretaceous strata, has been deformed since the Late Cretaceous, when tectonic inversion occurred, possibly due to changes in the strike-slip motion, from dextral-to sinistral, of the HFZ. Late Cretaceous erosion was responsible for an important and unequal denudation. The timing of the transition from extension to uplift cannot be determined due to continuous erosion, but this uplift finally marked the end of the structural evolution of the Hanjinqi area and even the Ordos Basin. This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfaces have been recognized overlying a paleoslope surface (T9) in this area: (1) The Late Carboniferous-Permian and Triassic tectonic sequence (TS-1); sedimentation of the lowest part of this succession is strongly controlled by the Hangjinqi Fault Zone (HFZ), whereas the rest of the sequence indicates much less fault control; (2) the Middle Jurassic tectonic sequence (TS-2); (3) the Late Early Cretaceous tectonic sequence (TS-3); and the TS-2 and TS-3 sequences are more extensive than the TS-1 sequence throughout the Hangjinqi area. The structural framework displayed by the TS-2 sequence is very different from that displayed by the TS-3 sequence. More specifically, the general structure beneath the unconformity (T3) between the Late Jurassic strata and the Early Cretaceous strata consists of an E–W trending transtensional fault system. This resulted from a multi-stage dextral phase, which was caused by oblique subduction of the Paleo-Pacific Plate under the Eurasian Plate and dextral movement of the HFZ, and a subsequent inversion event, which caused significant reverse movement along previous transtensional structures. The study area, which underlies the unconformity (T2) between the Late Jurassic strata and the Early Cretaceous strata, has been deformed since the Late Cretaceous, when tectonic inversion occurred, possibly due to changes in the strike-slip motion, from dextral-to sinistral, of the HFZ. Late Cretaceous erosion was responsible for an important and unequal denudation. The timing of the transition from extension to uplift cannot be determined due to continuous erosion, but this uplift finally marked the end of the structural evolution of the Hanjinqi area and even the Ordos Basin. Hangjinqi area Elsevier Mesozoic Elsevier Structural evolution Elsevier Ordos Basin Elsevier Uplift and erosion Elsevier Inversion Elsevier Li, Liang oth Zhou, Jin oth Jia, Huichong oth Sun, Xiao oth Qu, Xiaoyan oth Zhou, Duo oth Gong, Ting oth Ding, Chao oth Enthalten in Elsevier Science Guo, Zhen ELSEVIER Honesty-Humility and unethical behavior in adolescents: The mediating role of moral disengagement and the moderating role of system justification 2021 Amsterdam [u.a.] (DE-627)ELV006295584 volume:66 year:2015 pages:695-710 extent:16 https://doi.org/10.1016/j.marpetgeo.2015.07.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 44.67 Kinderheilkunde VZ AR 66 2015 695-710 16 045F 550 |
| spelling |
10.1016/j.marpetgeo.2015.07.014 doi GBVA2015008000007.pica (DE-627)ELV018371345 (ELSEVIER)S0264-8172(15)30035-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 44.67 bkl Yang, Minghui verfasserin aut Mesozoic structural evolution of the Hangjinqi area in the northern Ordos Basin, North China 2015transfer abstract 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfaces have been recognized overlying a paleoslope surface (T9) in this area: (1) The Late Carboniferous-Permian and Triassic tectonic sequence (TS-1); sedimentation of the lowest part of this succession is strongly controlled by the Hangjinqi Fault Zone (HFZ), whereas the rest of the sequence indicates much less fault control; (2) the Middle Jurassic tectonic sequence (TS-2); (3) the Late Early Cretaceous tectonic sequence (TS-3); and the TS-2 and TS-3 sequences are more extensive than the TS-1 sequence throughout the Hangjinqi area. The structural framework displayed by the TS-2 sequence is very different from that displayed by the TS-3 sequence. More specifically, the general structure beneath the unconformity (T3) between the Late Jurassic strata and the Early Cretaceous strata consists of an E–W trending transtensional fault system. This resulted from a multi-stage dextral phase, which was caused by oblique subduction of the Paleo-Pacific Plate under the Eurasian Plate and dextral movement of the HFZ, and a subsequent inversion event, which caused significant reverse movement along previous transtensional structures. The study area, which underlies the unconformity (T2) between the Late Jurassic strata and the Early Cretaceous strata, has been deformed since the Late Cretaceous, when tectonic inversion occurred, possibly due to changes in the strike-slip motion, from dextral-to sinistral, of the HFZ. Late Cretaceous erosion was responsible for an important and unequal denudation. The timing of the transition from extension to uplift cannot be determined due to continuous erosion, but this uplift finally marked the end of the structural evolution of the Hanjinqi area and even the Ordos Basin. This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfaces have been recognized overlying a paleoslope surface (T9) in this area: (1) The Late Carboniferous-Permian and Triassic tectonic sequence (TS-1); sedimentation of the lowest part of this succession is strongly controlled by the Hangjinqi Fault Zone (HFZ), whereas the rest of the sequence indicates much less fault control; (2) the Middle Jurassic tectonic sequence (TS-2); (3) the Late Early Cretaceous tectonic sequence (TS-3); and the TS-2 and TS-3 sequences are more extensive than the TS-1 sequence throughout the Hangjinqi area. The structural framework displayed by the TS-2 sequence is very different from that displayed by the TS-3 sequence. More specifically, the general structure beneath the unconformity (T3) between the Late Jurassic strata and the Early Cretaceous strata consists of an E–W trending transtensional fault system. This resulted from a multi-stage dextral phase, which was caused by oblique subduction of the Paleo-Pacific Plate under the Eurasian Plate and dextral movement of the HFZ, and a subsequent inversion event, which caused significant reverse movement along previous transtensional structures. The study area, which underlies the unconformity (T2) between the Late Jurassic strata and the Early Cretaceous strata, has been deformed since the Late Cretaceous, when tectonic inversion occurred, possibly due to changes in the strike-slip motion, from dextral-to sinistral, of the HFZ. Late Cretaceous erosion was responsible for an important and unequal denudation. The timing of the transition from extension to uplift cannot be determined due to continuous erosion, but this uplift finally marked the end of the structural evolution of the Hanjinqi area and even the Ordos Basin. Hangjinqi area Elsevier Mesozoic Elsevier Structural evolution Elsevier Ordos Basin Elsevier Uplift and erosion Elsevier Inversion Elsevier Li, Liang oth Zhou, Jin oth Jia, Huichong oth Sun, Xiao oth Qu, Xiaoyan oth Zhou, Duo oth Gong, Ting oth Ding, Chao oth Enthalten in Elsevier Science Guo, Zhen ELSEVIER Honesty-Humility and unethical behavior in adolescents: The mediating role of moral disengagement and the moderating role of system justification 2021 Amsterdam [u.a.] (DE-627)ELV006295584 volume:66 year:2015 pages:695-710 extent:16 https://doi.org/10.1016/j.marpetgeo.2015.07.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 44.67 Kinderheilkunde VZ AR 66 2015 695-710 16 045F 550 |
| allfields_unstemmed |
10.1016/j.marpetgeo.2015.07.014 doi GBVA2015008000007.pica (DE-627)ELV018371345 (ELSEVIER)S0264-8172(15)30035-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 44.67 bkl Yang, Minghui verfasserin aut Mesozoic structural evolution of the Hangjinqi area in the northern Ordos Basin, North China 2015transfer abstract 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfaces have been recognized overlying a paleoslope surface (T9) in this area: (1) The Late Carboniferous-Permian and Triassic tectonic sequence (TS-1); sedimentation of the lowest part of this succession is strongly controlled by the Hangjinqi Fault Zone (HFZ), whereas the rest of the sequence indicates much less fault control; (2) the Middle Jurassic tectonic sequence (TS-2); (3) the Late Early Cretaceous tectonic sequence (TS-3); and the TS-2 and TS-3 sequences are more extensive than the TS-1 sequence throughout the Hangjinqi area. The structural framework displayed by the TS-2 sequence is very different from that displayed by the TS-3 sequence. More specifically, the general structure beneath the unconformity (T3) between the Late Jurassic strata and the Early Cretaceous strata consists of an E–W trending transtensional fault system. This resulted from a multi-stage dextral phase, which was caused by oblique subduction of the Paleo-Pacific Plate under the Eurasian Plate and dextral movement of the HFZ, and a subsequent inversion event, which caused significant reverse movement along previous transtensional structures. The study area, which underlies the unconformity (T2) between the Late Jurassic strata and the Early Cretaceous strata, has been deformed since the Late Cretaceous, when tectonic inversion occurred, possibly due to changes in the strike-slip motion, from dextral-to sinistral, of the HFZ. Late Cretaceous erosion was responsible for an important and unequal denudation. The timing of the transition from extension to uplift cannot be determined due to continuous erosion, but this uplift finally marked the end of the structural evolution of the Hanjinqi area and even the Ordos Basin. This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfaces have been recognized overlying a paleoslope surface (T9) in this area: (1) The Late Carboniferous-Permian and Triassic tectonic sequence (TS-1); sedimentation of the lowest part of this succession is strongly controlled by the Hangjinqi Fault Zone (HFZ), whereas the rest of the sequence indicates much less fault control; (2) the Middle Jurassic tectonic sequence (TS-2); (3) the Late Early Cretaceous tectonic sequence (TS-3); and the TS-2 and TS-3 sequences are more extensive than the TS-1 sequence throughout the Hangjinqi area. The structural framework displayed by the TS-2 sequence is very different from that displayed by the TS-3 sequence. More specifically, the general structure beneath the unconformity (T3) between the Late Jurassic strata and the Early Cretaceous strata consists of an E–W trending transtensional fault system. This resulted from a multi-stage dextral phase, which was caused by oblique subduction of the Paleo-Pacific Plate under the Eurasian Plate and dextral movement of the HFZ, and a subsequent inversion event, which caused significant reverse movement along previous transtensional structures. The study area, which underlies the unconformity (T2) between the Late Jurassic strata and the Early Cretaceous strata, has been deformed since the Late Cretaceous, when tectonic inversion occurred, possibly due to changes in the strike-slip motion, from dextral-to sinistral, of the HFZ. Late Cretaceous erosion was responsible for an important and unequal denudation. The timing of the transition from extension to uplift cannot be determined due to continuous erosion, but this uplift finally marked the end of the structural evolution of the Hanjinqi area and even the Ordos Basin. Hangjinqi area Elsevier Mesozoic Elsevier Structural evolution Elsevier Ordos Basin Elsevier Uplift and erosion Elsevier Inversion Elsevier Li, Liang oth Zhou, Jin oth Jia, Huichong oth Sun, Xiao oth Qu, Xiaoyan oth Zhou, Duo oth Gong, Ting oth Ding, Chao oth Enthalten in Elsevier Science Guo, Zhen ELSEVIER Honesty-Humility and unethical behavior in adolescents: The mediating role of moral disengagement and the moderating role of system justification 2021 Amsterdam [u.a.] (DE-627)ELV006295584 volume:66 year:2015 pages:695-710 extent:16 https://doi.org/10.1016/j.marpetgeo.2015.07.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 44.67 Kinderheilkunde VZ AR 66 2015 695-710 16 045F 550 |
| allfieldsGer |
10.1016/j.marpetgeo.2015.07.014 doi GBVA2015008000007.pica (DE-627)ELV018371345 (ELSEVIER)S0264-8172(15)30035-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 44.67 bkl Yang, Minghui verfasserin aut Mesozoic structural evolution of the Hangjinqi area in the northern Ordos Basin, North China 2015transfer abstract 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfaces have been recognized overlying a paleoslope surface (T9) in this area: (1) The Late Carboniferous-Permian and Triassic tectonic sequence (TS-1); sedimentation of the lowest part of this succession is strongly controlled by the Hangjinqi Fault Zone (HFZ), whereas the rest of the sequence indicates much less fault control; (2) the Middle Jurassic tectonic sequence (TS-2); (3) the Late Early Cretaceous tectonic sequence (TS-3); and the TS-2 and TS-3 sequences are more extensive than the TS-1 sequence throughout the Hangjinqi area. The structural framework displayed by the TS-2 sequence is very different from that displayed by the TS-3 sequence. More specifically, the general structure beneath the unconformity (T3) between the Late Jurassic strata and the Early Cretaceous strata consists of an E–W trending transtensional fault system. This resulted from a multi-stage dextral phase, which was caused by oblique subduction of the Paleo-Pacific Plate under the Eurasian Plate and dextral movement of the HFZ, and a subsequent inversion event, which caused significant reverse movement along previous transtensional structures. The study area, which underlies the unconformity (T2) between the Late Jurassic strata and the Early Cretaceous strata, has been deformed since the Late Cretaceous, when tectonic inversion occurred, possibly due to changes in the strike-slip motion, from dextral-to sinistral, of the HFZ. Late Cretaceous erosion was responsible for an important and unequal denudation. The timing of the transition from extension to uplift cannot be determined due to continuous erosion, but this uplift finally marked the end of the structural evolution of the Hanjinqi area and even the Ordos Basin. This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfaces have been recognized overlying a paleoslope surface (T9) in this area: (1) The Late Carboniferous-Permian and Triassic tectonic sequence (TS-1); sedimentation of the lowest part of this succession is strongly controlled by the Hangjinqi Fault Zone (HFZ), whereas the rest of the sequence indicates much less fault control; (2) the Middle Jurassic tectonic sequence (TS-2); (3) the Late Early Cretaceous tectonic sequence (TS-3); and the TS-2 and TS-3 sequences are more extensive than the TS-1 sequence throughout the Hangjinqi area. The structural framework displayed by the TS-2 sequence is very different from that displayed by the TS-3 sequence. More specifically, the general structure beneath the unconformity (T3) between the Late Jurassic strata and the Early Cretaceous strata consists of an E–W trending transtensional fault system. This resulted from a multi-stage dextral phase, which was caused by oblique subduction of the Paleo-Pacific Plate under the Eurasian Plate and dextral movement of the HFZ, and a subsequent inversion event, which caused significant reverse movement along previous transtensional structures. The study area, which underlies the unconformity (T2) between the Late Jurassic strata and the Early Cretaceous strata, has been deformed since the Late Cretaceous, when tectonic inversion occurred, possibly due to changes in the strike-slip motion, from dextral-to sinistral, of the HFZ. Late Cretaceous erosion was responsible for an important and unequal denudation. The timing of the transition from extension to uplift cannot be determined due to continuous erosion, but this uplift finally marked the end of the structural evolution of the Hanjinqi area and even the Ordos Basin. Hangjinqi area Elsevier Mesozoic Elsevier Structural evolution Elsevier Ordos Basin Elsevier Uplift and erosion Elsevier Inversion Elsevier Li, Liang oth Zhou, Jin oth Jia, Huichong oth Sun, Xiao oth Qu, Xiaoyan oth Zhou, Duo oth Gong, Ting oth Ding, Chao oth Enthalten in Elsevier Science Guo, Zhen ELSEVIER Honesty-Humility and unethical behavior in adolescents: The mediating role of moral disengagement and the moderating role of system justification 2021 Amsterdam [u.a.] (DE-627)ELV006295584 volume:66 year:2015 pages:695-710 extent:16 https://doi.org/10.1016/j.marpetgeo.2015.07.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 44.67 Kinderheilkunde VZ AR 66 2015 695-710 16 045F 550 |
| allfieldsSound |
10.1016/j.marpetgeo.2015.07.014 doi GBVA2015008000007.pica (DE-627)ELV018371345 (ELSEVIER)S0264-8172(15)30035-0 DE-627 ger DE-627 rakwb eng 550 550 DE-600 610 VZ 44.67 bkl Yang, Minghui verfasserin aut Mesozoic structural evolution of the Hangjinqi area in the northern Ordos Basin, North China 2015transfer abstract 16 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfaces have been recognized overlying a paleoslope surface (T9) in this area: (1) The Late Carboniferous-Permian and Triassic tectonic sequence (TS-1); sedimentation of the lowest part of this succession is strongly controlled by the Hangjinqi Fault Zone (HFZ), whereas the rest of the sequence indicates much less fault control; (2) the Middle Jurassic tectonic sequence (TS-2); (3) the Late Early Cretaceous tectonic sequence (TS-3); and the TS-2 and TS-3 sequences are more extensive than the TS-1 sequence throughout the Hangjinqi area. The structural framework displayed by the TS-2 sequence is very different from that displayed by the TS-3 sequence. More specifically, the general structure beneath the unconformity (T3) between the Late Jurassic strata and the Early Cretaceous strata consists of an E–W trending transtensional fault system. This resulted from a multi-stage dextral phase, which was caused by oblique subduction of the Paleo-Pacific Plate under the Eurasian Plate and dextral movement of the HFZ, and a subsequent inversion event, which caused significant reverse movement along previous transtensional structures. The study area, which underlies the unconformity (T2) between the Late Jurassic strata and the Early Cretaceous strata, has been deformed since the Late Cretaceous, when tectonic inversion occurred, possibly due to changes in the strike-slip motion, from dextral-to sinistral, of the HFZ. Late Cretaceous erosion was responsible for an important and unequal denudation. The timing of the transition from extension to uplift cannot be determined due to continuous erosion, but this uplift finally marked the end of the structural evolution of the Hanjinqi area and even the Ordos Basin. This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfaces have been recognized overlying a paleoslope surface (T9) in this area: (1) The Late Carboniferous-Permian and Triassic tectonic sequence (TS-1); sedimentation of the lowest part of this succession is strongly controlled by the Hangjinqi Fault Zone (HFZ), whereas the rest of the sequence indicates much less fault control; (2) the Middle Jurassic tectonic sequence (TS-2); (3) the Late Early Cretaceous tectonic sequence (TS-3); and the TS-2 and TS-3 sequences are more extensive than the TS-1 sequence throughout the Hangjinqi area. The structural framework displayed by the TS-2 sequence is very different from that displayed by the TS-3 sequence. More specifically, the general structure beneath the unconformity (T3) between the Late Jurassic strata and the Early Cretaceous strata consists of an E–W trending transtensional fault system. This resulted from a multi-stage dextral phase, which was caused by oblique subduction of the Paleo-Pacific Plate under the Eurasian Plate and dextral movement of the HFZ, and a subsequent inversion event, which caused significant reverse movement along previous transtensional structures. The study area, which underlies the unconformity (T2) between the Late Jurassic strata and the Early Cretaceous strata, has been deformed since the Late Cretaceous, when tectonic inversion occurred, possibly due to changes in the strike-slip motion, from dextral-to sinistral, of the HFZ. Late Cretaceous erosion was responsible for an important and unequal denudation. The timing of the transition from extension to uplift cannot be determined due to continuous erosion, but this uplift finally marked the end of the structural evolution of the Hanjinqi area and even the Ordos Basin. Hangjinqi area Elsevier Mesozoic Elsevier Structural evolution Elsevier Ordos Basin Elsevier Uplift and erosion Elsevier Inversion Elsevier Li, Liang oth Zhou, Jin oth Jia, Huichong oth Sun, Xiao oth Qu, Xiaoyan oth Zhou, Duo oth Gong, Ting oth Ding, Chao oth Enthalten in Elsevier Science Guo, Zhen ELSEVIER Honesty-Humility and unethical behavior in adolescents: The mediating role of moral disengagement and the moderating role of system justification 2021 Amsterdam [u.a.] (DE-627)ELV006295584 volume:66 year:2015 pages:695-710 extent:16 https://doi.org/10.1016/j.marpetgeo.2015.07.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 44.67 Kinderheilkunde VZ AR 66 2015 695-710 16 045F 550 |
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Mesozoic structural evolution of the Hangjinqi area in the northern Ordos Basin, North China |
| abstract |
This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfaces have been recognized overlying a paleoslope surface (T9) in this area: (1) The Late Carboniferous-Permian and Triassic tectonic sequence (TS-1); sedimentation of the lowest part of this succession is strongly controlled by the Hangjinqi Fault Zone (HFZ), whereas the rest of the sequence indicates much less fault control; (2) the Middle Jurassic tectonic sequence (TS-2); (3) the Late Early Cretaceous tectonic sequence (TS-3); and the TS-2 and TS-3 sequences are more extensive than the TS-1 sequence throughout the Hangjinqi area. The structural framework displayed by the TS-2 sequence is very different from that displayed by the TS-3 sequence. More specifically, the general structure beneath the unconformity (T3) between the Late Jurassic strata and the Early Cretaceous strata consists of an E–W trending transtensional fault system. This resulted from a multi-stage dextral phase, which was caused by oblique subduction of the Paleo-Pacific Plate under the Eurasian Plate and dextral movement of the HFZ, and a subsequent inversion event, which caused significant reverse movement along previous transtensional structures. The study area, which underlies the unconformity (T2) between the Late Jurassic strata and the Early Cretaceous strata, has been deformed since the Late Cretaceous, when tectonic inversion occurred, possibly due to changes in the strike-slip motion, from dextral-to sinistral, of the HFZ. Late Cretaceous erosion was responsible for an important and unequal denudation. The timing of the transition from extension to uplift cannot be determined due to continuous erosion, but this uplift finally marked the end of the structural evolution of the Hanjinqi area and even the Ordos Basin. |
| abstractGer |
This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfaces have been recognized overlying a paleoslope surface (T9) in this area: (1) The Late Carboniferous-Permian and Triassic tectonic sequence (TS-1); sedimentation of the lowest part of this succession is strongly controlled by the Hangjinqi Fault Zone (HFZ), whereas the rest of the sequence indicates much less fault control; (2) the Middle Jurassic tectonic sequence (TS-2); (3) the Late Early Cretaceous tectonic sequence (TS-3); and the TS-2 and TS-3 sequences are more extensive than the TS-1 sequence throughout the Hangjinqi area. The structural framework displayed by the TS-2 sequence is very different from that displayed by the TS-3 sequence. More specifically, the general structure beneath the unconformity (T3) between the Late Jurassic strata and the Early Cretaceous strata consists of an E–W trending transtensional fault system. This resulted from a multi-stage dextral phase, which was caused by oblique subduction of the Paleo-Pacific Plate under the Eurasian Plate and dextral movement of the HFZ, and a subsequent inversion event, which caused significant reverse movement along previous transtensional structures. The study area, which underlies the unconformity (T2) between the Late Jurassic strata and the Early Cretaceous strata, has been deformed since the Late Cretaceous, when tectonic inversion occurred, possibly due to changes in the strike-slip motion, from dextral-to sinistral, of the HFZ. Late Cretaceous erosion was responsible for an important and unequal denudation. The timing of the transition from extension to uplift cannot be determined due to continuous erosion, but this uplift finally marked the end of the structural evolution of the Hanjinqi area and even the Ordos Basin. |
| abstract_unstemmed |
This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfaces have been recognized overlying a paleoslope surface (T9) in this area: (1) The Late Carboniferous-Permian and Triassic tectonic sequence (TS-1); sedimentation of the lowest part of this succession is strongly controlled by the Hangjinqi Fault Zone (HFZ), whereas the rest of the sequence indicates much less fault control; (2) the Middle Jurassic tectonic sequence (TS-2); (3) the Late Early Cretaceous tectonic sequence (TS-3); and the TS-2 and TS-3 sequences are more extensive than the TS-1 sequence throughout the Hangjinqi area. The structural framework displayed by the TS-2 sequence is very different from that displayed by the TS-3 sequence. More specifically, the general structure beneath the unconformity (T3) between the Late Jurassic strata and the Early Cretaceous strata consists of an E–W trending transtensional fault system. This resulted from a multi-stage dextral phase, which was caused by oblique subduction of the Paleo-Pacific Plate under the Eurasian Plate and dextral movement of the HFZ, and a subsequent inversion event, which caused significant reverse movement along previous transtensional structures. The study area, which underlies the unconformity (T2) between the Late Jurassic strata and the Early Cretaceous strata, has been deformed since the Late Cretaceous, when tectonic inversion occurred, possibly due to changes in the strike-slip motion, from dextral-to sinistral, of the HFZ. Late Cretaceous erosion was responsible for an important and unequal denudation. The timing of the transition from extension to uplift cannot be determined due to continuous erosion, but this uplift finally marked the end of the structural evolution of the Hanjinqi area and even the Ordos Basin. |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV018371345</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230625123856.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">180602s2015 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.marpetgeo.2015.07.014</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">GBVA2015008000007.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV018371345</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0264-8172(15)30035-0</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2=" "><subfield code="a">550</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">610</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">44.67</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Yang, Minghui</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Mesozoic structural evolution of the Hangjinqi area in the northern Ordos Basin, North China</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2015transfer abstract</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">16</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfaces have been recognized overlying a paleoslope surface (T9) in this area: (1) The Late Carboniferous-Permian and Triassic tectonic sequence (TS-1); sedimentation of the lowest part of this succession is strongly controlled by the Hangjinqi Fault Zone (HFZ), whereas the rest of the sequence indicates much less fault control; (2) the Middle Jurassic tectonic sequence (TS-2); (3) the Late Early Cretaceous tectonic sequence (TS-3); and the TS-2 and TS-3 sequences are more extensive than the TS-1 sequence throughout the Hangjinqi area. The structural framework displayed by the TS-2 sequence is very different from that displayed by the TS-3 sequence. More specifically, the general structure beneath the unconformity (T3) between the Late Jurassic strata and the Early Cretaceous strata consists of an E–W trending transtensional fault system. This resulted from a multi-stage dextral phase, which was caused by oblique subduction of the Paleo-Pacific Plate under the Eurasian Plate and dextral movement of the HFZ, and a subsequent inversion event, which caused significant reverse movement along previous transtensional structures. The study area, which underlies the unconformity (T2) between the Late Jurassic strata and the Early Cretaceous strata, has been deformed since the Late Cretaceous, when tectonic inversion occurred, possibly due to changes in the strike-slip motion, from dextral-to sinistral, of the HFZ. Late Cretaceous erosion was responsible for an important and unequal denudation. The timing of the transition from extension to uplift cannot be determined due to continuous erosion, but this uplift finally marked the end of the structural evolution of the Hanjinqi area and even the Ordos Basin.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">This study analyzes the structural evolution of the Hangjinqi area in the northern Ordos Basin, based on seismic sections and exploration well data. This area shows excellent examples of the relationship between tectonics and sedimentation. Three tectonic sequences separated by four erosional surfaces have been recognized overlying a paleoslope surface (T9) in this area: (1) The Late Carboniferous-Permian and Triassic tectonic sequence (TS-1); sedimentation of the lowest part of this succession is strongly controlled by the Hangjinqi Fault Zone (HFZ), whereas the rest of the sequence indicates much less fault control; (2) the Middle Jurassic tectonic sequence (TS-2); (3) the Late Early Cretaceous tectonic sequence (TS-3); and the TS-2 and TS-3 sequences are more extensive than the TS-1 sequence throughout the Hangjinqi area. The structural framework displayed by the TS-2 sequence is very different from that displayed by the TS-3 sequence. More specifically, the general structure beneath the unconformity (T3) between the Late Jurassic strata and the Early Cretaceous strata consists of an E–W trending transtensional fault system. This resulted from a multi-stage dextral phase, which was caused by oblique subduction of the Paleo-Pacific Plate under the Eurasian Plate and dextral movement of the HFZ, and a subsequent inversion event, which caused significant reverse movement along previous transtensional structures. The study area, which underlies the unconformity (T2) between the Late Jurassic strata and the Early Cretaceous strata, has been deformed since the Late Cretaceous, when tectonic inversion occurred, possibly due to changes in the strike-slip motion, from dextral-to sinistral, of the HFZ. Late Cretaceous erosion was responsible for an important and unequal denudation. The timing of the transition from extension to uplift cannot be determined due to continuous erosion, but this uplift finally marked the end of the structural evolution of the Hanjinqi area and even the Ordos Basin.</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Hangjinqi area</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Mesozoic</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Structural evolution</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Ordos Basin</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Uplift and erosion</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Inversion</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Li, Liang</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhou, Jin</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Jia, Huichong</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sun, Xiao</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Qu, Xiaoyan</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhou, Duo</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Gong, Ting</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Ding, Chao</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier Science</subfield><subfield code="a">Guo, Zhen ELSEVIER</subfield><subfield code="t">Honesty-Humility and unethical behavior in adolescents: The mediating role of moral disengagement and the moderating role of system justification</subfield><subfield code="d">2021</subfield><subfield code="g">Amsterdam [u.a.]</subfield><subfield code="w">(DE-627)ELV006295584</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:66</subfield><subfield code="g">year:2015</subfield><subfield code="g">pages:695-710</subfield><subfield code="g">extent:16</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.marpetgeo.2015.07.014</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">44.67</subfield><subfield code="j">Kinderheilkunde</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">66</subfield><subfield code="j">2015</subfield><subfield code="h">695-710</subfield><subfield code="g">16</subfield></datafield><datafield tag="953" ind1=" " ind2=" "><subfield code="2">045F</subfield><subfield code="a">550</subfield></datafield></record></collection>
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