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Meso-Cenozoic Tectonothermal History of Permian Strata, Southwestern Weibei Uplift: Insights from Thermochronology and Geothermometry
  修订日期:2019-04-14  点此下载全文
引用本文:YU Qiang,REN Zhanli,LI Rongxi,TAO Ni,QI Kai,JIANG Cheng,WANG Baojiang.2019.Meso-Cenozoic Tectonothermal History of Permian Strata, Southwestern Weibei Uplift: Insights from Thermochronology and Geothermometry[J].ACTA GEOLOGICA SINICA(English edition),93(6):1647~1661
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DOI:10.1111/1755-6724.14367
作者单位E-mail
YU Qiang 1 The School of Earth Science and Resources, Chang’an University, Xi’an 710054, China 2 Key Laboratory of Western China's Mineral Resources and Geological Engineering, Ministry of Education, Chang'an University, Xi'an 710054, China  
REN Zhanli 3 State Key Laboratory of Continental Dynamics, Northwest University, Xi'an 710069, China 4 Department of Geology, Northwest University, Xi’an, 710069, China renzhanl@nwu.edu.cn 
LI Rongxi 1 The School of Earth Science and Resources, Chang’an University, Xi’an 710054, China 2 Key Laboratory of Western China's Mineral Resources and Geological Engineering, Ministry of Education, Chang'an University, Xi'an 710054, China  
TAO Ni 1 The School of Earth Science and Resources, Chang’an University, Xi’an 710054, China4 Department of Geology, Northwest University, Xi’an, 710069, China  
QI Kai 3 State Key Laboratory of Continental Dynamics, Northwest University, Xi'an 710069, China 4 Department of Geology, Northwest University, Xi’an, 710069, China  
JIANG Cheng 5 State Key Laboratory of Coal Mine Disaster Dynamics and Control, Chongqing University, Chongqing 400030, China 6 State and Local Joint Engineering Laboratory of Methane Drainage in Complex Coal Gas Seam, Chongqing University, Chongqing 400030, China  
WANG Baojiang 7 Research Institute of Yanchang Petroleum (Group) Company Limited, Xi’an, Sichuan, 710075, China  
 
Author NameAffiliationE-mail
YU Qiang 1 The School of Earth Science and Resources, Chang’an University, Xi’an 710054, China 2 Key Laboratory of Western China's Mineral Resources and Geological Engineering, Ministry of Education, Chang'an University, Xi'an 710054, China  
REN Zhanli 3 State Key Laboratory of Continental Dynamics, Northwest University, Xi'an 710069, China 4 Department of Geology, Northwest University, Xi’an, 710069, China renzhanl@nwu.edu.cn 
LI Rongxi 1 The School of Earth Science and Resources, Chang’an University, Xi’an 710054, China 2 Key Laboratory of Western China's Mineral Resources and Geological Engineering, Ministry of Education, Chang'an University, Xi'an 710054, China  
TAO Ni 1 The School of Earth Science and Resources, Chang’an University, Xi’an 710054, China4 Department of Geology, Northwest University, Xi’an, 710069, China  
QI Kai 3 State Key Laboratory of Continental Dynamics, Northwest University, Xi'an 710069, China 4 Department of Geology, Northwest University, Xi’an, 710069, China  
JIANG Cheng 5 State Key Laboratory of Coal Mine Disaster Dynamics and Control, Chongqing University, Chongqing 400030, China 6 State and Local Joint Engineering Laboratory of Methane Drainage in Complex Coal Gas Seam, Chongqing University, Chongqing 400030, China  
WANG Baojiang 7 Research Institute of Yanchang Petroleum (Group) Company Limited, Xi’an, Sichuan, 710075, China  
Abstract:This study provides an integrated interpretation for the Mesozoic - Cenozoic tectonothermal evolutionary history of the Permian strata in the Qishan area of the southwestern Weibei Uplift, Ordos Basin. Apatite fission-track and apatite/zircon (U-Th)/He thermochronometry, bitumen reflectance, thermal conductivity of rocks, paleotemperature recovery, and basin modeling were used to restore the Meso-Cenozoic tectonothermal history of the Permian Strata. The Triassic AFT data have a pooled age of ~180±7 Ma with one age peak and P(χ2)=86%. The average value of corrected apatite (U-Th)/He age of two Permian sandstones is ~168±4 Ma and a zircon (U-Th)/He age from the Cambrian strata is ~231±14 Ma. Bitumen reflectance and maximum paleotemperature of two Ordovician mudstones are 1.81%, 1.57% and ~210°C, ~196°C respectively. After undergoing a rapid subsidence and increasing temperature in Triassic influenced by intrusive rocks in some areas, the Permian strata experienced four cooling-uplift stages after the time when the maximum paleotemperature reached in late Jurassic: (1) A cooling stage (~163 Ma to ~140 Ma) with temperatures ranging from ~132°C to ~53°C and a cooling rate of ~3°C/Ma, an erosion thickness of ~1900 m and an uplift rate of ~82 m/Ma; (2) A cooling stage (~140 Ma to ~52 Ma) with temperatures ranging from ~53°C to ~47°C and a cooling rate less than ~0.1°C /Ma, an erosion thickness of ~300 m and an uplift rate of ~3 m/Ma; (3) (~52 Ma to ~8 Ma) with ~47°C to ~43°C and ~0.1°C /Ma, an erosion thickness of ~500 m and an uplift rate of ~11 m/Ma; (3) (~8 Ma to present ) with ~43°C to ~20°C and ~3°C/Ma, an erosion thickness of ~650 m and an uplift rate of ~81 m/Ma. The tectonothermal evolutionary history of the Qishan area in Triassic was influenced by the interaction of the Qinling Orogeny and the Weibei Uplift, and the south Qishan area had the earliest uplift-cooling time compared to other parts within the Weibei Uplift. The early Eocene at ~52 Ma and the late Miocene at ~8 Ma, as two significant turning points after which both the rate of uplift and the rate of temperature changed rapidly, were two key time for the uplift-cooling history of the Permian strata in the Qishan area of the southwestern Weibei Uplift, Ordos Basin.
keywords:low temperature thermochronology, fission track, (U-Th)/He, basin modeling, cooling history, uplift, Ordos Basin
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