Cretaceous long-distance lithospheric extension and surface response in South China
Lithospheric extension plays a pivotal role in governing the evolution of continents and the birth of oceanic basins on Earth. Despite this, quantifying wide-mode lithospheric extension and its effects on surface uplift remain elusive. The vast (> 800-km-wide) Cretaceous extensional system in Sou...
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| Published in | Earth-science reviews Vol. 243; p. 104496 |
|---|---|
| Main Authors | , , , , , , , |
| Format | Journal Article |
| Language | English |
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Elsevier B.V
01.08.2023
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| Abstract | Lithospheric extension plays a pivotal role in governing the evolution of continents and the birth of oceanic basins on Earth. Despite this, quantifying wide-mode lithospheric extension and its effects on surface uplift remain elusive. The vast (> 800-km-wide) Cretaceous extensional system in South China offers a unique opportunity to study the processes and mechanism(s) of wide-mode extension and their impacts. Here we review the essential constraints from crustal and mantle structures determined from geological, seismic reflection/refraction, and other geophysical data. Our compilation reveals a stratified lithosphere with depth-dependent extension in a magma-poor domain, expressed by normal faulting in the upper crust, ductile stretching in the mid-lower crust, and localized Moho uplift associated with mantle shear zones. From the magma-poor domain to the magma-rich domain, lateral variations in the extensional mode involve increased crustal melting, decreased crust-mantle decoupling, and mantle shear-zone abandonment caused by magmatic underplating. Extension-related strain fields across the South China lithosphere are uniformly NW-SE oriented, indicating vertically coherent deformation. Stress transmission across this coherent system likely occurred via basal traction and localized mantle shearing. Lower-crustal stretching and lithospheric removal accompanied and promoted the tectonic exhumation of extensional domes and mountain ranges. We propose a coupling between slab rollback, mantle flow, and lithospheric extension. Rollback-induced mantle flow likely drove lithospheric extension in South China by imposing shear forces at the lithosphere base.
•We review the deep processes of Cretaceous long-distance extension in South China.•Our data compilation reveals a stratified lithosphere with depth-dependent extension.•We clarified lateral variations in extension modes across the >800-km-wide system.•We propose a coupling between slab rollback, mantle flow, and lithospheric extension. |
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| AbstractList | Lithospheric extension plays a pivotal role in governing the evolution of continents and the birth of oceanic basins on Earth. Despite this, quantifying wide-mode lithospheric extension and its effects on surface uplift remain elusive. The vast (> 800-km-wide) Cretaceous extensional system in South China offers a unique opportunity to study the processes and mechanism(s) of wide-mode extension and their impacts. Here we review the essential constraints from crustal and mantle structures determined from geological, seismic reflection/refraction, and other geophysical data. Our compilation reveals a stratified lithosphere with depth-dependent extension in a magma-poor domain, expressed by normal faulting in the upper crust, ductile stretching in the mid-lower crust, and localized Moho uplift associated with mantle shear zones. From the magma-poor domain to the magma-rich domain, lateral variations in the extensional mode involve increased crustal melting, decreased crust-mantle decoupling, and mantle shear-zone abandonment caused by magmatic underplating. Extension-related strain fields across the South China lithosphere are uniformly NW-SE oriented, indicating vertically coherent deformation. Stress transmission across this coherent system likely occurred via basal traction and localized mantle shearing. Lower-crustal stretching and lithospheric removal accompanied and promoted the tectonic exhumation of extensional domes and mountain ranges. We propose a coupling between slab rollback, mantle flow, and lithospheric extension. Rollback-induced mantle flow likely drove lithospheric extension in South China by imposing shear forces at the lithosphere base.
•We review the deep processes of Cretaceous long-distance extension in South China.•Our data compilation reveals a stratified lithosphere with depth-dependent extension.•We clarified lateral variations in extension modes across the >800-km-wide system.•We propose a coupling between slab rollback, mantle flow, and lithospheric extension. Lithospheric extension plays a pivotal role in governing the evolution of continents and the birth of oceanic basins on Earth. Despite this, quantifying wide-mode lithospheric extension and its effects on surface uplift remain elusive. The vast (> 800-km-wide) Cretaceous extensional system in South China offers a unique opportunity to study the processes and mechanism(s) of wide-mode extension and their impacts. Here we review the essential constraints from crustal and mantle structures determined from geological, seismic reflection/refraction, and other geophysical data. Our compilation reveals a stratified lithosphere with depth-dependent extension in a magma-poor domain, expressed by normal faulting in the upper crust, ductile stretching in the mid-lower crust, and localized Moho uplift associated with mantle shear zones. From the magma-poor domain to the magma-rich domain, lateral variations in the extensional mode involve increased crustal melting, decreased crust-mantle decoupling, and mantle shear-zone abandonment caused by magmatic underplating. Extension-related strain fields across the South China lithosphere are uniformly NW-SE oriented, indicating vertically coherent deformation. Stress transmission across this coherent system likely occurred via basal traction and localized mantle shearing. Lower-crustal stretching and lithospheric removal accompanied and promoted the tectonic exhumation of extensional domes and mountain ranges. We propose a coupling between slab rollback, mantle flow, and lithospheric extension. Rollback-induced mantle flow likely drove lithospheric extension in South China by imposing shear forces at the lithosphere base. |
| ArticleNumber | 104496 |
| Author | Li, Jianhua Dong, Shuwen Clift, Peter D. Johnston, Stephen T. Cawood, Peter A. Zhang, Yueqiao Thybo, Hans Zhao, Guochun |
| Author_xml | – sequence: 1 givenname: Jianhua surname: Li fullname: Li, Jianhua email: lijianhua0301@126.com organization: Institute of Geomechanics, Chinese Academy of Geological Sciences, MNR Key Laboratory of Paleomagnetism and Tectonic Reconstruction, Beijing 100081, China – sequence: 2 givenname: Shuwen surname: Dong fullname: Dong, Shuwen organization: SinoProbe Laboratory, Chinese Academy of Geological Sciences, Beijing 100037, China – sequence: 3 givenname: Peter A. surname: Cawood fullname: Cawood, Peter A. organization: School of Earth, Atmosphere & Environment, Monash University, Melbourne, VIC 3800, Australia – sequence: 4 givenname: Hans surname: Thybo fullname: Thybo, Hans organization: SinoProbe Laboratory, Chinese Academy of Geological Sciences, Beijing 100037, China – sequence: 5 givenname: Peter D. surname: Clift fullname: Clift, Peter D. organization: Department of Earth Sciences, University College London, London WC1E 6BS, UK – sequence: 6 givenname: Stephen T. surname: Johnston fullname: Johnston, Stephen T. organization: Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta, Canada – sequence: 7 givenname: Guochun surname: Zhao fullname: Zhao, Guochun organization: Department of Earth Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong, China – sequence: 8 givenname: Yueqiao surname: Zhang fullname: Zhang, Yueqiao organization: State Key Laboratory for Mineral Deposits Research, Nanjing University, Nanjing 210023, China |
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| Title | Cretaceous long-distance lithospheric extension and surface response in South China |
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