Normal fault evolution in Lishu Fault Depression, southern Songliao Basin
The formation of the Songliao Basin was affected by multidirectional tectonic stress and various peripheral structural belts, and has a complicated geological structure and basin evolution process. The Lishu Fault Depression in the southern Songliao Basin has the characteristics of superimposed and...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | zho |
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Editorial Office of Petroleum Geology and Experiment
2021-03-01
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| Series: | Shiyou shiyan dizhi |
| Subjects: | |
| Online Access: | https://www.sysydz.net/cn/article/doi/10.11781/sysydz202102288 |
| _version_ | 1797277234126389248 |
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| author | Mingzhe DENG Zongxin ZUO Qi QIU Fan BAI |
| author_facet | Mingzhe DENG Zongxin ZUO Qi QIU Fan BAI |
| author_sort | Mingzhe DENG |
| collection | DOAJ |
| description | The formation of the Songliao Basin was affected by multidirectional tectonic stress and various peripheral structural belts, and has a complicated geological structure and basin evolution process. The Lishu Fault Depression in the southern Songliao Basin has the characteristics of superimposed and complex evolution of multiple tectonic activities, and is a good window to reveal the impacts of the peripheral structural belts and basin tectonic-sedimentary response. Whether strike-slip tectonic activity controls the sedimentary process of the basin is an unsolved problem. Using three-dimensional seismic data to carry out detailed interpretation, combined with fault distance statistics, structural model analysis and other research methods, the extension activities of the Sangshutai and Qinjiatun faults in the Lishu Fault Depression during the Early Cretaceous were studied. The evolution process of the Sangshutai fault was controlled by the nearly east-west extensional tectonic stress. The initial scale of the fault was large, so the Sangshutai fault was less affected by the adjustment of the extension direction. The Qinjiatun fault was controlled by the NEE-SWW extension during the Early Cretaceous Huoshiling period, and by the NE-SW extension during the Early Cretaceous Shahezi period. The regional strike-slip activity in the Early Cretaceous extension in the Lishu Fault Depression caused a change in the extension direction. |
| first_indexed | 2024-03-07T15:45:44Z |
| format | Article |
| id | doaj.art-9c49cc782927484ea10f2f6de02d2b76 |
| institution | Directory Open Access Journal |
| issn | 1001-6112 |
| language | zho |
| last_indexed | 2024-03-07T15:45:44Z |
| publishDate | 2021-03-01 |
| publisher | Editorial Office of Petroleum Geology and Experiment |
| record_format | Article |
| series | Shiyou shiyan dizhi |
| spelling | doaj.art-9c49cc782927484ea10f2f6de02d2b762024-03-05T04:39:43ZzhoEditorial Office of Petroleum Geology and ExperimentShiyou shiyan dizhi1001-61122021-03-0143228829610.11781/sysydz202102288sysydz-43-2-288Normal fault evolution in Lishu Fault Depression, southern Songliao BasinMingzhe DENG0Zongxin ZUO1Qi QIU2Fan BAI3Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, ChinaWuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, ChinaWuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, ChinaSINOPEC Geophysical Research Institute, Nanjing, Jiangsu 211103, ChinaThe formation of the Songliao Basin was affected by multidirectional tectonic stress and various peripheral structural belts, and has a complicated geological structure and basin evolution process. The Lishu Fault Depression in the southern Songliao Basin has the characteristics of superimposed and complex evolution of multiple tectonic activities, and is a good window to reveal the impacts of the peripheral structural belts and basin tectonic-sedimentary response. Whether strike-slip tectonic activity controls the sedimentary process of the basin is an unsolved problem. Using three-dimensional seismic data to carry out detailed interpretation, combined with fault distance statistics, structural model analysis and other research methods, the extension activities of the Sangshutai and Qinjiatun faults in the Lishu Fault Depression during the Early Cretaceous were studied. The evolution process of the Sangshutai fault was controlled by the nearly east-west extensional tectonic stress. The initial scale of the fault was large, so the Sangshutai fault was less affected by the adjustment of the extension direction. The Qinjiatun fault was controlled by the NEE-SWW extension during the Early Cretaceous Huoshiling period, and by the NE-SW extension during the Early Cretaceous Shahezi period. The regional strike-slip activity in the Early Cretaceous extension in the Lishu Fault Depression caused a change in the extension direction.https://www.sysydz.net/cn/article/doi/10.11781/sysydz202102288extension structureearly cretaceouslishu fault depressionsongliao basin |
| spellingShingle | Mingzhe DENG Zongxin ZUO Qi QIU Fan BAI Normal fault evolution in Lishu Fault Depression, southern Songliao Basin Shiyou shiyan dizhi extension structure early cretaceous lishu fault depression songliao basin |
| title | Normal fault evolution in Lishu Fault Depression, southern Songliao Basin |
| title_full | Normal fault evolution in Lishu Fault Depression, southern Songliao Basin |
| title_fullStr | Normal fault evolution in Lishu Fault Depression, southern Songliao Basin |
| title_full_unstemmed | Normal fault evolution in Lishu Fault Depression, southern Songliao Basin |
| title_short | Normal fault evolution in Lishu Fault Depression, southern Songliao Basin |
| title_sort | normal fault evolution in lishu fault depression southern songliao basin |
| topic | extension structure early cretaceous lishu fault depression songliao basin |
| url | https://www.sysydz.net/cn/article/doi/10.11781/sysydz202102288 |
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