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La-icp-ms zircon u-pb geochronology and petrology of the muchang alkali granite, zhenkang county, western yunnan province, china

文献类型:期刊论文

作者Ye Lin1; Gao Wei1,2; Cheng Zengtao1,2; Yang Yulong1,2; Tao Yan1
刊名Acta geologica sinica-english edition
出版日期2010
卷号84期号:6页码:1488-1499
关键词A-type granite U-pb age Muchang alkali granite Tectonic setting Evolution of tethys in southern sanjiang area
ISSN号1000-9515
DOI10.1111/j.1755-6724.2010.00343.x
通讯作者Ye lin(yelin@vip.gyig.ac.cn)
英文摘要The muchang composite intrusion is located about 14 km southeast of the fengwei town and south of the baoshan-zhenkang block. the rift-related intrusion consists of the early-stage riebeckite nordmarkite in the east and west sides and the discontinuous marginal zone, the late-stage main body of dominant riebeckite granite, and minor aegirine granite. studies on petrological geochemistry and la-icp-ms zircon u-pb dating of the late-stage riebeckite granite, origin and evolution of the muchang alkali granite and the relationship between the granite and the associated skarn-type luziyuan pb-zn deposit are discussed in this paper. the results show that the muchang alkali granites belong to a-type granites, which are characterized by enrichment in al2o3, sio2, total alkali and fe, depletion in mgo and cao contents with high feot/mgo ratios. the ree concentrations are relatively high, exhibiting highly fractionated lree patterns with significantly eu negative anomaly. the muchang granites are obviously enriched in lithophile elements (e.g., rb, k, u and th) and high field strength elements (e.g., zr, hf, nb, y and ga) with high 10000xga/al ratios and depleted in sr, ba, ti, cr and ni, which are similar to those of the a-type granites and quite different from those of s-type and i-type granites. the la-icp-ms zircon dating results of the muchang granite gave a weighted mean age of 266.2 +/- 5.4 ma (2 sigma), suggesting that they were formed in the stage of extension at the end of post-collision at middle permian and the consumption of paleo-tethys ocean took place before 266 ma. it is suggested that the unexposed intermediate-acid intrusive rocks in the luziyuan ore district, which is the "sister" rocks material of the muchang granites and related closely to luziyuan pb-zn mineralization, were the product of middle permian.
WOS关键词A-TYPE GRANITES ; SOUTHEASTERN AUSTRALIA ; PETROGENESIS ; ORIGIN ; AGE ; MAGMAS ; MANTLE ; ROCKS ; DISCRIMINATION ; CONSTRAINTS
WOS研究方向Geology
WOS类目Geosciences, Multidisciplinary
语种英语
WOS记录号WOS:000285753000015
出版者WILEY-BLACKWELL
URI标识http://www.irgrid.ac.cn/handle/1471x/2415268
专题中国科学院大学
通讯作者Ye Lin
作者单位1.Chinese Acad Sci, Inst Geochem, State Key Lab Ore Deposit Geochem, Guiyang 550002, Peoples R China
2.Chinese Acad Sci, Grad Sch, Beijing 100049, Peoples R China
推荐引用方式
GB/T 7714
Ye Lin,Gao Wei,Cheng Zengtao,et al. La-icp-ms zircon u-pb geochronology and petrology of the muchang alkali granite, zhenkang county, western yunnan province, china[J]. Acta geologica sinica-english edition,2010,84(6):1488-1499.
APA Ye Lin,Gao Wei,Cheng Zengtao,Yang Yulong,&Tao Yan.(2010).La-icp-ms zircon u-pb geochronology and petrology of the muchang alkali granite, zhenkang county, western yunnan province, china.Acta geologica sinica-english edition,84(6),1488-1499.
MLA Ye Lin,et al."La-icp-ms zircon u-pb geochronology and petrology of the muchang alkali granite, zhenkang county, western yunnan province, china".Acta geologica sinica-english edition 84.6(2010):1488-1499.

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来源:中国科学院大学

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