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新疆西昆仑塔什库尔干地区珈玛勒厄格勒中酸性侵入岩体及其大地构造意义

赵佳楠 许志琴

西北地质2017,Vol.50Issue(2):1-15,15.
西北地质2017,Vol.50Issue(2):1-15,15.

新疆西昆仑塔什库尔干地区珈玛勒厄格勒中酸性侵入岩体及其大地构造意义

Gamaleegrad Intermediate Intrusive Rock and Its Geotectonic Significance in the Taxkorgan Region of Western Kunlun Orogenic Belt, Xinjiang

赵佳楠 1许志琴2

作者信息

  • 1. 广东省核工业地质局二九一大队,广东 广州 510800
  • 2. 南京大学,江苏 南京 210023
  • 折叠

摘要

Abstract

Gamaleegrad intermediate intrusive rock, located at the southwestern margin of the Tarim Block and the northeast edge of Karakoram continental margin, is composed of calc-alkaline monzogranite series and alkaline granite series, which were formed between late Cambrian and early Ordovician.Based on geochemical analysis, the main elements and trace elements of Gamaleegrad intrusive rock have been studied in detail, as well as the tectonic setting of the intrusive sequence and geodynamic model between plates around the intrusive sequence have been discussed.The results show that the Gamaleegrad intermediate intrusive rock is a combination of monzogranite-granite (MG-G), which is mixed with sub-neutral granitic magma (high Sr, Zr and low Rb) that experienced the crustal remelting in the evolutionary process of intrusive sequence.It mainly belongs to I-type granites, which was formed in continental backarc extensional basin under the condition of subduction collision.Based on physical environment and tectonic setting in the course of magmatic evolution, it is speculated that the formation of these intrusive rock is closely related to subduction collision of Kuda oceanic crust towards Tarim ancient block, indicating the disappearance of Kuda Ocean and the formation of back-arc spreading granite.Meanwhile, it means that the continent-continent collision had taken place between Tarim ancient block and Qaidam ancient block, indicating that both of them were finally converged into Rodinia supercontinent.

关键词

西昆仑造山带/珈玛勒厄格勒中性侵入岩体/地球化学/构造环境/地球动力学

Key words

western Kunlun orogenic belt/Gamaleegrad intermediate intrusive rock/geochemistry/tectonic setting/geodynamics

分类

天文与地球科学

引用本文复制引用

赵佳楠,许志琴..新疆西昆仑塔什库尔干地区珈玛勒厄格勒中酸性侵入岩体及其大地构造意义[J].西北地质,2017,50(2):1-15,15.

基金项目

国家自然科学基金委创新群体项目(40921001),国家自然科学基金"龙门山断裂带晚古生代走滑运动及其成因机制研究"(40702036)资助 (40921001)

西北地质

OA北大核心CSCDCSTPCD

1009-6248

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