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Petrogenesis of the Dasuji porphyry Mo deposit at the northern margin of North China Craton: Constrains from geochronology, geochemistry and isotopes characteristics

文献类型：期刊论文

作者Chen, Peiwen1,2,3; Zeng, Qingdong1,2,3; Wang, Yongbin1,2; Zhou, Tiancheng1,2,3; Yu, Bing1,2,3; Chen, Junqi4
刊名LITHOS
出版日期2018-12-01
卷号322页码:87-103
关键词Zircon U-Pb age A-type granite Sr-Nd-Hf-Pb isotopes Magmatic evolution Dasuji porphyry Mo deposit
ISSN号0024-4937
DOI10.1016/j.lithos.2018.10.009
英文摘要The Dasuji porphyry Mo deposit is located at the northern margin of North China Craton. Mo mineralization occurs mainly within the intrusions of alkali feldspar granite, granite porphyry, and quartz porphyry, which yield weighted mean Pb-206/U-238 ages (2 sigma) of 227.6 +/- 1.5, 225.7 +/- 1.5, and 224.3 +/- 1.8 Ma, respectively. These ages are indistinguishable to the molybdenite Re-Os isochron age of 223.9 +/- 1.5 Ma (2 sigma). The Dasuji granites show the petrological, mineralogical, geochemical, and geotectonic characteristics of A-type granites. They exhibit low negative epsilon Nd(t) values (-16.7 to -12.6) with corresponding T-DM2 (Nd) ages of 1705-2000 Ma, variable but mainly negative epsilon Hf(t) values (mostly -21.0 to -7.9) with corresponding T-DM2 (Hf) ages of 1715-2728 Ma, and Pb isotopic compositions indicating that the primary magmas were dominantly derived from partial melting of ancient lower crust. In chondrite- and mantle-normalized trace element diagrams, all the granitic rocks show negative anomalies in Ba, Sr, and Eu, and a positive anomaly in Pb. The ratios of LREE/HREE, and (La/Yb)(N) and delta Eu values decrease from the alkali feldspar granite to the granite porphyry and quartz porphyry. These data are attributed to fractional crystallization processes. Fractionation of feldspar, biotite, and possibly K-feldspar produced the variations in major elements and Rb, Sr and Ba, and the distribution of REE are controlled mainly by fractionation of zircon, allanite, minor apatite, and possibly a small quantity of monazite. Together with the regional geology, the data infer that the Dasuji porphyry Mo deposit formed in a post-collision extensional setting during the Late Triassic. (C) 2018 Elsevier BY. All rights reserved.
WOS关键词A-TYPE GRANITES ; RE-OS AGES ; ASIAN OROGENIC BELT ; INNER-MONGOLIA ; TRACE-ELEMENTS ; CALC-ALKALINE ; GEOLOGICAL CHARACTERISTICS ; MOLYBDENUM DEPOSITS ; BASALTIC MAGMA ; HIGH-PRESSURE
资助项目National Natural Science Foundation of China[41390443] ; National Natural Science Foundation of China[91514301]
WOS研究方向Geochemistry & Geophysics ; Mineralogy
语种英语
WOS记录号WOS:000452817700006
出版者ELSEVIER SCIENCE BV
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/90266]  
专题地质与地球物理研究所_中国科学院矿产资源研究重点实验室
通讯作者Zeng, Qingdong
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China
2.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China
3.Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China
4.Inner Mongolia Zhongxi Min Co Ltd, Wulanchabu 012300, Inner Mongolia, Peoples R China
推荐引用方式
GB/T 7714		 Chen, Peiwen,Zeng, Qingdong,Wang, Yongbin,et al. Petrogenesis of the Dasuji porphyry Mo deposit at the northern margin of North China Craton: Constrains from geochronology, geochemistry and isotopes characteristics[J]. LITHOS,2018,322:87-103.
APA Chen, Peiwen,Zeng, Qingdong,Wang, Yongbin,Zhou, Tiancheng,Yu, Bing,&Chen, Junqi.(2018).Petrogenesis of the Dasuji porphyry Mo deposit at the northern margin of North China Craton: Constrains from geochronology, geochemistry and isotopes characteristics.LITHOS,322,87-103.
MLA Chen, Peiwen,et al."Petrogenesis of the Dasuji porphyry Mo deposit at the northern margin of North China Craton: Constrains from geochronology, geochemistry and isotopes characteristics".LITHOS 322(2018):87-103.

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来源：地质与地球物理研究所

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