Petrogenesis and tectonic setting of granite porphyry in Keyouzhongqi area,Inner Mongolia

查看全文 作　　者：WU [1]Qing;YANG [2]Weihong;HE [1]Zhonghua;YANG [1]Deming;MA [1]Rui;WANG [1]Jianguo

机构地区：[1]College of Earth Sciences,Jilin University;[2]Manage Center of Central Geological Exploration Fund,Ministry of Land and Resources

出　　处：《Global Geology》索引2014年第17卷第1期,共10页

摘　　要：The authors studied the geochemistry,zircon U-Pb ages,Hf isotope of the granite porphyry and its petrogenesis and tectonic setting in the studied area. The zircon U-Pb dating indicates the formation of the granite porphyry is in Early Cretaceous( 125. 1 ± 1. 5 Ma). The granite porphyry has high-SiO2and alkali-rich features,which belongs to high-K calc-alkaline series rocks( A / CNK = 0. 95%--1. 25%). The analyses of trace elements show the characteristics of a swallow-shaped REE distribution pattern with enrichment in LREEs and most of LILEs and HFSEs,depletion in Ba,Sr,Nb,P and Ti,and especially strong depletion in Eu,which indicates the granite porphyry belongs to the aluminous A-type granite. Their εHf( t)range from 5. 94 to 8. 80with Hf two-stage model ages( TDM2) of 620 Ma to 803 Ma. Combining with the regional tectonic background,we conclude that the source of the rocks is the new crust materials accreted from depleted mantle in Neoproterozoic and is the product of partial melting of middle and lower crustal rocks,which may be suffered from the dual impact of the subduction of the Palaeo-Pacific Ocean and the closure of the Mongol-Okhotsk Ocean. 关键词：大地构造背景花岗斑岩岩石成因内蒙古科右中旗铝质A型花岗岩锆石U-PB Hf同位素

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Petrogenesis and tectonic setting of granite porphyry in Keyouzhongqi area,Inner Mongolia

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