中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Zircon U-Pb geochronology, Hf-O isotopes, whole-rock geochemistry of the Dafosi and Jinfosi granite plutons, Gansu Province and geological implications

文献类型:期刊论文

作者Sun BaoLu1,2; Qian Qing1,3; Zhang JianXin4
刊名ACTA PETROLOGICA SINICA
出版日期2017
卷号33期号:10页码:3091-3108
关键词North Qilian Orogen Zoulang Transition Zone Granite Zircon U-pb Age Geochemistry
ISSN号1000-0569
文献子类Article
英文摘要The Dafosi granites from the Zoulang Transition Zone are weakly peraluminous (A/CNK = 1. 03 similar to 1. 06), with high SiO2 (76. 7% similar to 78. 9%), Na2O + K2O (7. 7% similar to 8. 3%), Rb (303 x 10(-6) 383 x 10-6), Nb (32 x 10-6 42 x 10-6) and heavy rare earth element (Yb similar to 8 x 10-6) contents, low MgO (similar to 0. 1%) and CaO (0.5% similar to 0. 6%) contents, high FeOT/MgO (6. 3 similar to 7. 6), Ga/Al (>3 x 10(-4)) and Rb/Ba (3. 0 similar to 6. 2) ratios, as well as large Ba, Sr, Eu and Ti depletions. The Dafosi pluton belongs to A type granite, and was likely derived from a pelitic source with magma temperature above similar to 820 degrees C. Zircon 8180, epsilon(Hf) (t) and two-stage depleted mantle Hf model ages of the Dafosi granites are 7. 8 parts per thousand similar to 8. 6Voc. (ave. 8. 24 +/- 0. 13 parts per thousand),-4. 8 +/- 2.0, and 1540 similar to 1717Ma, respectively. The Jinfosi granites from the northern margin of the North Qilian Orogen are also peraluminous with A/CNK about 1. 0 +/- 1. 1. They have large variations of SiO2 (65. 5% similar to 75. 0%), MgO (0. 6% similar to 2. 2%), Fe2O3 (1. 9% similar to 5. 2%) and TiO2 (0. 3% similar to 0. 8%) abundances. They resemble the Chaidanuo granites from the North Qilian Orogen in major and trace elements, and were likely derived by partial melting of greywacke and amphibolite with magma temperature about 800 similar to 900 degrees C. Zircon delta O-18, epsilon(Hf) (t) and two stage depleted mantle Hf model ages of the Jinfosi granites are 7. 4 parts per thousand -9. 7 parts per thousand (ave. 8. 03 +/- 0. 36 parts per thousand), similar to 0. 5 + 1. 9, and 1289 similar to 1439Ma,respectively. Zircon U-Pb SIMS dating of the Dafosi granite pluton from the Zoulang Transition Zone and the Jinfosi granite pluton from the northern margin of the North Qilian Orogen yielded ages of 426. 1 +/- 2. 8Ma and 424. 0 +/- 1. 6Ma, respectively. The occurrence of coeval magmatic rocks including A-type granite in the adjacent tectonic units indicates that by similar to 425Ma the North Qilian Ocean was already closed and the region was under an extensional regime of post-collisional stage.
WOS关键词A-TYPE GRANITES ; NORTH QILIAN MOUNTAINS ; LACHLAN FOLD BELT ; S-TYPE GRANITES ; NW CHINA ; METASEDIMENTARY ROCKS ; TIBETAN PLATEAU ; OXYGEN-ISOTOPE ; SUBDUCTION INITIATION ; CLASTIC SEDIMENTS
WOS研究方向Geology
语种英语
WOS记录号WOS:000417603000007
出版者SCIENCE PRESS
源URL[http://ir.iggcas.ac.cn/handle/132A11/82364]  
专题中国科学院地质与地球物理研究所
通讯作者Qian Qing
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
4.Chinese Acad Geol Sci, Inst Geol, Beijing 100037, Peoples R China
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GB/T 7714
Sun BaoLu,Qian Qing,Zhang JianXin. Zircon U-Pb geochronology, Hf-O isotopes, whole-rock geochemistry of the Dafosi and Jinfosi granite plutons, Gansu Province and geological implications[J]. ACTA PETROLOGICA SINICA,2017,33(10):3091-3108.
APA Sun BaoLu,Qian Qing,&Zhang JianXin.(2017).Zircon U-Pb geochronology, Hf-O isotopes, whole-rock geochemistry of the Dafosi and Jinfosi granite plutons, Gansu Province and geological implications.ACTA PETROLOGICA SINICA,33(10),3091-3108.
MLA Sun BaoLu,et al."Zircon U-Pb geochronology, Hf-O isotopes, whole-rock geochemistry of the Dafosi and Jinfosi granite plutons, Gansu Province and geological implications".ACTA PETROLOGICA SINICA 33.10(2017):3091-3108.

入库方式: OAI收割

来源:地质与地球物理研究所

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