IGGCAS OpenIR  > 岩石圈演化国家重点实验室
Decoding stratigraphic and structural evolution of the Songliao Basin: Implications for late Mesozoic tectonics in NE China
Zhu, Jichang1,3; Feng, Youliang4; Meng, Qing-ren1,2,3; Li, Shihu5; Wu, Guoli1,3; Zhu, Rixiang1,2,3
2020-06-01
Source PublicationJOURNAL OF ASIAN EARTH SCIENCES
ISSN1367-9120
Volume194Pages:14
AbstractAn analysis of the structural styles and sedimentary filling of the Songliao Basin (SB) in the late Mesozoic was carried out based on a detailed interpretation of a large number of 2D and 3D seismic reflection profiles. Using precise stratigraphic chronology, it was established that the SB mainly experienced five stages of evolution in the late Mesozoic, including thermal uplifting in the Late Jurassic, rifting in the Early Cretaceous, symmetrical subsidence early in the early Late Cretaceous, asymmetrical subsidence in the middle Late Cretaceous, and inversion at the end of Cretaceous. The structures contained listric faults and planar domino-style normal faults in the rifting stage; dense normal faults with small throw, as well as negative flower structures in the symmetrical subsidence stage; positive flower structures in the asymmetrical stage; and compression and inversion structures (e.g., angled unconformities and folds) in the inversion stage. Two angular unconformities identified in this area, T-5 and T-02, may reflect orogenic events caused by PaleoAsian Ocean closure and subduction of the Paleo-Pacific Ocean Plate beneath northeastern Asia from SE to NW. The compressive stress of the Yanshanian orogeny in the Yanshan tectonic belt originated from the subduction of the Paleo-Pacific Ocean Plate rather than the closure of the Mongol-Okhotsk Ocean. Although the SB had already been influenced by Paleo-Pacific Ocean Plate subduction in the middle Late Cretaceous, the stress did not cause the inversion of the SB. The SB was affected by Paleo-Pacific Ocean Plate subduction during the deposition of the second member of the Nenjiang Formation in the Upper Cretaceous; however, significant orogenic events and obvious inversion of the SB did not take place until the end of the Late Cretaceous.
KeywordSongliao Basin Late Mesozoic Mongol-Okhotsk Ocean Paleo-Pacific Ocean Plate Yanshanian orgeny
DOI10.1016/j.jseaes.2019.104138
Funding OrganizationNational Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences
WOS KeywordPALEO-ASIAN OCEAN ; EAST GOBI BASIN ; NORTH CHINA ; FAULT ZONE ; SEDIMENTARY ; MONGOLIA ; BELT ; CONSTRAINTS ; ARCHITECTURE ; DEFORMATION
Language英语
Funding ProjectNational Key R&D Program of China[2017YFC0601206] ; National Key R&D Program of China[2016YFC0600406] ; National Natural Science Foundation of China[41688103] ; National Natural Science Foundation of China[41572126] ; National Natural Science Foundation of China[40972151] ; National Natural Science Foundation of China[91114204] ; National Oil & Gas Project of China[2016ZX05006-005] ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences[Z201604]
Funding OrganizationNational Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; National Oil & Gas Project of China ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences ; State Key Laboratory of Lithospheric Evolution of Institute of Geology and Geophysic, Chinese Academy of Sciences
WOS Research AreaGeology
WOS SubjectGeosciences, Multidisciplinary
WOS IDWOS:000538820400009
PublisherPERGAMON-ELSEVIER SCIENCE LTD
Citation statistics
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/96922
Collection岩石圈演化国家重点实验室
Corresponding AuthorFeng, Youliang
Affiliation1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 10029, Peoples R China
4.PetroChina Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China
5.Univ Lancaster, Lancaster Environm Ctr, Lancaster LA1 4YQ, England
First Author AffilicationState Key Laboratory of Lithospheric Evolution
Recommended Citation
GB/T 7714
Zhu, Jichang,Feng, Youliang,Meng, Qing-ren,et al. Decoding stratigraphic and structural evolution of the Songliao Basin: Implications for late Mesozoic tectonics in NE China[J]. JOURNAL OF ASIAN EARTH SCIENCES,2020,194:14.
APA Zhu, Jichang,Feng, Youliang,Meng, Qing-ren,Li, Shihu,Wu, Guoli,&Zhu, Rixiang.(2020).Decoding stratigraphic and structural evolution of the Songliao Basin: Implications for late Mesozoic tectonics in NE China.JOURNAL OF ASIAN EARTH SCIENCES,194,14.
MLA Zhu, Jichang,et al."Decoding stratigraphic and structural evolution of the Songliao Basin: Implications for late Mesozoic tectonics in NE China".JOURNAL OF ASIAN EARTH SCIENCES 194(2020):14.
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