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Spatio-temporal variation in rock exhumation linked to large-scale shear zones in the southeastern Tibetan Plateau
作者姓名:Yukui GE  Jing LIU-ZENG  Jinyu ZHANG  Wei WANG  Yuntao TIAN  Matthew FOX  Lingsen ZENG  Xiaoming SHEN  Heng WANG  Ze SU  Kejia XIE
作者单位:State Key Laboratory of Earthquake Dynamics;Institute of Surface-Earth System Science;Guangdong Provincial Key Laboratory of Geodynamics and Geohazards;Department of Earth Sciences;Key Laboratory of Deep-Earth Dynamics;Key Laboratory of Crustal Dynamics;Henan Province Non-ferrous Metals Geological Mineral Resources Bureau
基金项目:supported by the National Natural Science Foundation of China(Grant Nos.41761144065,41902213 and 41702223);the State Key Laboratory of Earthquake Dynamics of China(Grant No.LED2016A02);the National Key Research and Development Project of China(Grant No.2016YFC0600310);the Natural Environment Research Council of UK(Grant No.NE/N015479/1)。
摘    要:Crustal-scale shear zones are believed to have played an important role in the tectonic and landscape evolution of orogens. However, the variation of long-term rock exhumation between the interior of shear zones and adjacent regions has not been documented in detail. In this study, we obtained new zircon U-Pb, biotite 40Ar/39Ar, zircon and apatite(U-Th)/He data, and conducted inverse thermal history modeling from two age-elevation profiles(the Pianma and Tu'er profiles) in the southeastern Tibetan Plateau. Our goal is to constrain the exhumation history of the Gaoligong and Chongshan shear zones and adjacent regions, so as to explore the effect of the shear zones on exhumation and their thermal effect on cooling that should not be ignored. Our results suggest that during the interval of 18–11 Ma the exhumation rates of rocks within the Gaoligong shear zone are anomalously high compared with those outside of. The rapid cooling during 18–11 Ma appears to be restricted to the shear zone, likely due to localized thermal effects of shearing and exhumation. After 11 Ma, both the areas within and outside of the shear zones experienced a similar two-stage exhumation history: slower cooling until the early Pliocene, and then a rapid increase in cooling rate since the early Pliocene. Our results indicate a synchronized exhumation but with spatially varied exhumation rates. Our study also highlights the important role of large-scale shear zones in exposing rocks, and thus the importance of the structural context when interpreting thermochronological data in the southeastern margin of the Tibetan Plateau.

关 键 词:Southeastern  TIBETAN  PLATEAU  EXHUMATION  (U-Th)/He  LOW-TEMPERATURE  THERMOCHRONOMETRY  Shear  zone

Spatio-temporal variation in rock exhumation linked to large-scale shear zones in the southeastern Tibetan Plateau
Yukui GE,Jing LIU-ZENG,Jinyu ZHANG,Wei WANG,Yuntao TIAN,Matthew FOX,Lingsen ZENG,Xiaoming SHEN,Heng WANG,Ze SU,Kejia XIE.Spatio-temporal variation in rock exhumation linked to large-scale shear zones in the southeastern Tibetan Plateau[J].Science China Earth Sciences,2020,63(4):512-532.
Authors:Ge  Yukui  Liu-Zeng  Jing  Zhang  Jinyu  Wang  Wei  Tian  Yuntao  Fox  Matthew  Zeng  Lingsen  Shen  Xiaoming  Wang  Heng  Su  Ze  Xie  Kejia
Institution:1.State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing, 100029, China
;2.Institute of Surface-Earth System Science, Tianjin University, Tianjin, 300072, China
;3.Guangdong Provincial Key Laboratory of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou, 510275, China
;4.Department of Earth Sciences, University College London, Gower St., Kings Cross London, WC1E 6BT, UK
;5.Key Laboratory of Deep-Earth Dynamics, Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, 100037, China
;6.Key Laboratory of Crustal Dynamics, Institute of Crustal Dynamics, China Earthquake Administration, Beijing, 100085, China
;7.Henan Province Non-ferrous Metals Geological Mineral Resources Bureau, Zhengzhou, 450016, China
;
Abstract:Science China Earth Sciences - Crustal-scale shear zones are believed to have played an important role in the tectonic and landscape evolution of orogens. However, the variation of long-term rock...
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