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Multi-phase cooling of Early Cretaceous granites on the Jiaodong Peninsula, East China: Evidence from Ar-40/Ar-39 and (U-Th)/He thermochronology

文献类型：期刊论文

作者Wu, Lin1,2,3; Monie, Patrick3; Wang, Fei1,2,4; Lin, Wei1,2; Ji, Wenbin1,2; Yang, Liekun1,2
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2018-07-01
卷号160页码:334-347
关键词Jiaodong Peninsula North China Craton Biotite Ar-40/Ar-39 dating Zircon (U-Th)/He thermochronology Mesozoic granites
ISSN号1367-9120
DOI10.1016/j.jseaes.2017.11.014
文献子类Article
英文摘要The Jiaodong Peninsula at the southeastern periphery of the North China Craton (NCC) has undergone complex changes since the Mesozoic. A striking feature of the NCC is the widespread distribution of Late Mesozoic magmatic rocks, predominantly characterized by granitic intrusions. These igneous plutons are economically important due to their polymetallic mineralization and significant as geodynamic tracers of the regional tectonic evolution. Two representative Early Cretaceous granites (the Yashan and Yuangezhuang plutons) on the Jiaodong Peninsula were selected for multiple-thermochronometer studies to constrain a complete thermal history from their emplacement to near-surface conditions. We obtained biotite Ar-40/Ar-39 ages of two granites on the new generation Argus VI noble gas mass spectrometer. Two biotites registered identical Ar-40/Ar-39 plateau ages of similar to 117 Ma, which are consistent within the error with their zircon U-Pb ages. This suggested that the two granites were emplaced at the same time and cooled rapidly to about 300 degrees C. The single crystal zircon (U-Th)/He (ZHe) dating for the two samples gave weighted mean ages of 93.5 +/- 4.5 Ma and 93.3 +/- 5.0 Ma. Combined with previously published geochronological data and the thermal inversion of the zircon low temperature thermochronological data, three phases of rapid cooling were identified for the two studied plutons: (1) the Early Cretaceous (117-110 Ma); (2) the Late Cretaceous (100-90 Ma); and (3) the Early Tertiary (65-50 Ma). The Early Cretaceous phase of cooling occurred in a regional extensional regime on the NCC characterized by various extensional structures. The Late Cretaceous cooling is consistent with the third episode of the "Yanshan Movement", which caused a regional basin inversion event on the NCC. In comparison to the first two phases of rapid cooling, the Early Tertiary cooling was more gradual. This phase corresponded to a widely developed Eocene rift on the NCC and the reactivation of major boundary faults, such as the giant Tan-Lu Fault Zone and the Taihangshan Fault.
WOS关键词LU FAULT ZONE ; METAMORPHIC CORE COMPLEX ; APATITE FISSION-TRACK ; SULU OROGENIC BELT ; ZIRCON U-PB ; LOW-TEMPERATURE THERMOCHRONOMETRY ; MESOZOIC EXTENSIONAL TECTONICS ; ULTRAHIGH-PRESSURE TERRANE ; COESITE-BEARING ZIRCON ; SOUTHERN TAN-LU
WOS研究方向Geology
语种英语
WOS记录号WOS:000434751500022
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构Chinese Academy of Sciences (CAS) ; Chinese Academy of Sciences (CAS) ; Chinese Academy of Sciences (CAS) ; Chinese Academy of Sciences (CAS) ; Le Centre National de la Recherche Scientifique (CNRS) ; Le Centre National de la Recherche Scientifique (CNRS) ; Le Centre National de la Recherche Scientifique (CNRS) ; Le Centre National de la Recherche Scientifique (CNRS) ; National Natural Science Foundation of China(41503055 ; National Natural Science Foundation of China(41503055 ; National Natural Science Foundation of China(41503055 ; National Natural Science Foundation of China(41503055 ; Ministry of Science and Technology of the People's Republic of China(2016YFC0600109) ; Ministry of Science and Technology of the People's Republic of China(2016YFC0600109) ; Ministry of Science and Technology of the People's Republic of China(2016YFC0600109) ; Ministry of Science and Technology of the People's Republic of China(2016YFC0600109) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDB03020203) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDB03020203) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDB03020203) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDB03020203) ; 41221002 ; 41221002 ; 41221002 ; 41221002 ; 41302114) ; 41302114) ; 41302114) ; 41302114) ; Chinese Academy of Sciences (CAS) ; Chinese Academy of Sciences (CAS) ; Chinese Academy of Sciences (CAS) ; Chinese Academy of Sciences (CAS) ; Le Centre National de la Recherche Scientifique (CNRS) ; Le Centre National de la Recherche Scientifique (CNRS) ; Le Centre National de la Recherche Scientifique (CNRS) ; Le Centre National de la Recherche Scientifique (CNRS) ; National Natural Science Foundation of China(41503055 ; National Natural Science Foundation of China(41503055 ; National Natural Science Foundation of China(41503055 ; National Natural Science Foundation of China(41503055 ; Ministry of Science and Technology of the People's Republic of China(2016YFC0600109) ; Ministry of Science and Technology of the People's Republic of China(2016YFC0600109) ; Ministry of Science and Technology of the People's Republic of China(2016YFC0600109) ; Ministry of Science and Technology of the People's Republic of China(2016YFC0600109) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDB03020203) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDB03020203) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDB03020203) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDB03020203) ; 41221002 ; 41221002 ; 41221002 ; 41221002 ; 41302114) ; 41302114) ; 41302114) ; 41302114) ; Chinese Academy of Sciences (CAS) ; Chinese Academy of Sciences (CAS) ; Chinese Academy of Sciences (CAS) ; Chinese Academy of Sciences (CAS) ; Le Centre National de la Recherche Scientifique (CNRS) ; Le Centre National de la Recherche Scientifique (CNRS) ; Le Centre National de la Recherche Scientifique (CNRS) ; Le Centre National de la Recherche Scientifique (CNRS) ; National Natural Science Foundation of China(41503055 ; National Natural Science Foundation of China(41503055 ; National Natural Science Foundation of China(41503055 ; National Natural Science Foundation of China(41503055 ; Ministry of Science and Technology of the People's Republic of China(2016YFC0600109) ; Ministry of Science and Technology of the People's Republic of China(2016YFC0600109) ; Ministry of Science and Technology of the People's Republic of China(2016YFC0600109) ; Ministry of Science and Technology of the People's Republic of China(2016YFC0600109) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDB03020203) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDB03020203) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDB03020203) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDB03020203) ; 41221002 ; 41221002 ; 41221002 ; 41221002 ; 41302114) ; 41302114) ; 41302114) ; 41302114) ; Chinese Academy of Sciences (CAS) ; Chinese Academy of Sciences (CAS) ; Chinese Academy of Sciences (CAS) ; Chinese Academy of Sciences (CAS) ; Le Centre National de la Recherche Scientifique (CNRS) ; Le Centre National de la Recherche Scientifique (CNRS) ; Le Centre National de la Recherche Scientifique (CNRS) ; Le Centre National de la Recherche Scientifique (CNRS) ; National Natural Science Foundation of China(41503055 ; National Natural Science Foundation of China(41503055 ; National Natural Science Foundation of China(41503055 ; National Natural Science Foundation of China(41503055 ; Ministry of Science and Technology of the People's Republic of China(2016YFC0600109) ; Ministry of Science and Technology of the People's Republic of China(2016YFC0600109) ; Ministry of Science and Technology of the People's Republic of China(2016YFC0600109) ; Ministry of Science and Technology of the People's Republic of China(2016YFC0600109) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDB03020203) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDB03020203) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDB03020203) ; "Strategic Priority Research Program" of the Chinese Academy of Sciences(XDB03020203) ; 41221002 ; 41221002 ; 41221002 ; 41221002 ; 41302114) ; 41302114) ; 41302114) ; 41302114)
源URL[http://ir.iggcas.ac.cn/handle/132A11/88209]  
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Wu, Lin
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Inst Earth Sci, Beijing, Peoples R China
3.Univ Montpellier 2, Geosci Montpellier, UMR CNRS 5243, Pl E Bataillon, F-34095 Montpellier, France
4.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China
推荐引用方式
GB/T 7714		 Wu, Lin,Monie, Patrick,Wang, Fei,et al. Multi-phase cooling of Early Cretaceous granites on the Jiaodong Peninsula, East China: Evidence from Ar-40/Ar-39 and (U-Th)/He thermochronology[J]. JOURNAL OF ASIAN EARTH SCIENCES,2018,160:334-347.
APA Wu, Lin,Monie, Patrick,Wang, Fei,Lin, Wei,Ji, Wenbin,&Yang, Liekun.(2018).Multi-phase cooling of Early Cretaceous granites on the Jiaodong Peninsula, East China: Evidence from Ar-40/Ar-39 and (U-Th)/He thermochronology.JOURNAL OF ASIAN EARTH SCIENCES,160,334-347.
MLA Wu, Lin,et al."Multi-phase cooling of Early Cretaceous granites on the Jiaodong Peninsula, East China: Evidence from Ar-40/Ar-39 and (U-Th)/He thermochronology".JOURNAL OF ASIAN EARTH SCIENCES 160(2018):334-347.

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来源：地质与地球物理研究所

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