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Geo-thermochronological analysis reveals transition from transverse to axial detrital inputs during Cretaceous rifting in the Songliao Basin, NE China

文献类型：期刊论文

作者Wang, Nan1,2,3; Zhang, Zhiyong1,5; Malusa, Marco G.3; Zhang, Jien1; Wu, Lin1; Xiang, Dunfeng1,2; Xiao, Wenjiao4
刊名TERRA NOVA
出版日期2023-09-25
页码8
ISSN号0954-4879
关键词AFT thermochronology drainage pattern figure provenance analysis Songliao Basin zircon U-Pb geochronology
DOI10.1111/ter.12682
英文摘要The impact of tectonics, volcanism and climate in controlling temporal and spatial variations in rift-basin sedimentation is still poorly understood. Here, we tackle this issue by the analysis of mid-Cretaceous sediments deposited in the Songliao Basin, northeastern China. We present new zircon U-Pb, apatite fission-track and trace-element data from the northeastern basin, which are discussed within the framework of the published geochronology dataset. Our results reveal a major provenance change from syn-rift tectonic extension to post-rift thermal subsidence at similar to 103 Ma. During the syn-rift stage, the detrital inputs were dominantly from transverse rivers sourced from the surrounding mountains including graben shoulders and volcanoes. During the post-rift stage and coeval thermal subsidence, the basin sedimentation was controlled by coexisting transverse and axial drainage systems sourced from uplifting regions in the south. We conclude that tectonics, not climate, exerted a major control in sediment provenance change in the mid-Cretaceous Songliao Basin.
WOS关键词CONTINENTAL-MARGIN EVOLUTION ; ZIRCON U-PB ; STRUCTURAL CONTROL ; SHAHEZI FORMATION ; SEDIMENTATION ; BOREHOLE ; CLIMATE ; ASIA
资助项目This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments.[41888101] ; This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments.[42230303] ; This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments.[92055213] ; National Natural Science Foundation of China
WOS研究方向Geology
语种英语
出版者WILEY
WOS记录号WOS:001071166000001
资助机构This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments. ; This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments. ; This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments. ; This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments. ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments. ; This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments. ; This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments. ; This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments. ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments. ; This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments. ; This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments. ; This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments. ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments. ; This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments. ; This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments. ; This work was supported by the National Natural Science Foundation of China (grant numbers 41888101, 42230303 and 92055213). Scientific Editor Carlo Doglioni, Associate Editor Vincenzo Stagno and two anonymous are appreciated for their insightful comments. ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/110796]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Zhang, Zhiyong; Malusa, Marco G.
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
2.Univ Chinese Acad Sci, Beijing, Peoples R China
3.Univ Milano Bicocca, Dept Earth & Environm Sci, Milan, Italy
4.Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Xinjiang Res Ctr Mineral Resources, Urumqi, Peoples R China
5.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714		 Wang, Nan,Zhang, Zhiyong,Malusa, Marco G.,et al. Geo-thermochronological analysis reveals transition from transverse to axial detrital inputs during Cretaceous rifting in the Songliao Basin, NE China[J]. TERRA NOVA,2023:8.
APA Wang, Nan.,Zhang, Zhiyong.,Malusa, Marco G..,Zhang, Jien.,Wu, Lin.,...&Xiao, Wenjiao.(2023).Geo-thermochronological analysis reveals transition from transverse to axial detrital inputs during Cretaceous rifting in the Songliao Basin, NE China.TERRA NOVA,8.
MLA Wang, Nan,et al."Geo-thermochronological analysis reveals transition from transverse to axial detrital inputs during Cretaceous rifting in the Songliao Basin, NE China".TERRA NOVA (2023):8.

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