中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Petrogenesis of Late Triassic granitoids and their enclaves with implications for post-collisional lithospheric thinning of the Liaodong Peninsula, North China Craton

文献类型:期刊论文

作者Yang, Jin-Hui; Wu, Fu-Yuan; Wilde, Simon A.; Liu, Xiao-Ming
刊名CHEMICAL GEOLOGY
出版日期2007-07-30
卷号242期号:1-2页码:155-175
关键词Mafic microgranular enclaves granite Late Triassic lithospheric thinning North China Craton
ISSN号0009-2541
DOI10.1016/j.chemgeo.2007.03.007
文献子类Article
英文摘要Major and trace element, Sr-, Nd- and Hf-isotope, zircon U-Pb and Hf-isotope data are reported for mafic microgranular enclaves and host granitoids from the Xiuyan pluton in the Liaodong Peninsula of the eastern North China Craton, in order to investigate their sources, petrogenesis and tectonic implications. The zircon U-Pb age of the enclaves (211 I Ma) is identical to that of the host granite (210 +/- 1 Ma), establishing that the mafic and felsic magmas were coeval. The enclaves have high MgO concentrations at low silica contents and positive epsilon(Ht)(t) values. They are enriched in large ion lithophile and light rare earth elements and depleted in high field strength elements, which can be explained as melts derived from a depleted (asthenosphelic) mantle, with some crustal contamination. The host granitoids have high SiO2 contents, variable initial Sr-87/(86) Sr ratios and highly negative epsilon(Nd)(t) and epsilon(Hf) t) values, suggesting they were mainly derived from an ancient crustal source, heated by the input of asthenospheric mantle-derived magmas. Field observations, geochronology, geochemistry, Sr and Nd isotopic and zircon Hf isotopic compositions point to a complex petrogenesis, where asthenospheric mantle- and crust-derived magma mixing was coupled with crystal fractionation, thus explaining the genetic link between enclaves and host rocks. Identification of an asthenospheric mantle component in the Xiuyan granitoids suggests asthenospheric mantle upwelling and decompressional melting of the mantle, indicating that post-collisional lithospheric thinning in the Liaodong Peninsula was initiated in the Late Triassic. (C) 2007 Elsevier B.V. All rights reserved.
WOS关键词SINO-KOREAN CRATON ; U-PB AGES ; COESITE-BEARING ECLOGITES ; HF ISOTOPE COMPOSITION ; SULU OROGENIC BELT ; TECTONIC IMPLICATIONS ; ULTRAHIGH-PRESSURE ; EASTERN CHINA ; TRACE-ELEMENT ; MICROGRANITOID ENCLAVES
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000248433400009
出版者ELSEVIER SCIENCE BV
源URL[http://ir.iggcas.ac.cn/handle/132A11/68160]  
专题中国科学院地质与地球物理研究所
通讯作者Yang, Jin-Hui
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Curtin Univ Technol, Dept Appl Geol, Perth, WA 6845, Australia
3.Nw Univ, State Key Continental Dynam, Xian 750069, Peoples R China
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Yang, Jin-Hui,Wu, Fu-Yuan,Wilde, Simon A.,et al. Petrogenesis of Late Triassic granitoids and their enclaves with implications for post-collisional lithospheric thinning of the Liaodong Peninsula, North China Craton[J]. CHEMICAL GEOLOGY,2007,242(1-2):155-175.
APA Yang, Jin-Hui,Wu, Fu-Yuan,Wilde, Simon A.,&Liu, Xiao-Ming.(2007).Petrogenesis of Late Triassic granitoids and their enclaves with implications for post-collisional lithospheric thinning of the Liaodong Peninsula, North China Craton.CHEMICAL GEOLOGY,242(1-2),155-175.
MLA Yang, Jin-Hui,et al."Petrogenesis of Late Triassic granitoids and their enclaves with implications for post-collisional lithospheric thinning of the Liaodong Peninsula, North China Craton".CHEMICAL GEOLOGY 242.1-2(2007):155-175.

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来源:地质与地球物理研究所

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