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西藏南木林县罗扎地区早白垩世流纹岩锆石 U-Pb 年龄及地球化学特征

刘伟 李奋其 杨晓勇 袁四化

中国地质2012,Vol.39Issue(5):1151-1161,11.
中国地质2012,Vol.39Issue(5):1151-1161,11.

西藏南木林县罗扎地区早白垩世流纹岩锆石 U-Pb 年龄及地球化学特征

Zircon U-Pb age and geochemistry of Early Cretaceous rhyolite in Luozha area of Namling County, Tibet

刘伟 1李奋其 2杨晓勇 2袁四化1

作者信息

  • 1. 中国科学技术大学地球和空间科学学院,安徽合肥,230026
  • 2. 中国地质调查局成都地质调查中心,四川成都,610081
  • 折叠

摘要

Abstract

The authors studied the nearly EW —trending volcanic rocks in vast areas of northern Luozha zone along the Gangdise arc—ridge fault—uplift zone, obtained the LA—ICP—MS zircon age of 129.8±1.4 Ma, and proved for the first time the existence of Early Cretaceous volcanic rocks in the Gangdise arc—ridge fault—uplift zone. The volcanic rocks are characterized by high SiO2, K2O and K2O/Na2O values, the enrichment of LILEs (Rb, Ba, Th and U) and the depletion of Nb, Ta and Ti. Their cobweb curve is on the whole the same as that of the upper crust and the acidic volcanic rocks owing to crustal remelting of Zenong Group of the Gangdise zone at 110 Ma. These data indicate that the volcanic rocks might be the remelting products resulting from the dehydration of crustal materials. According to the environmental discrimination diagrams of trace elements, the authors consider that they are arc volcanic rocks. In combination with the tectonic background of Early Cretaceous period, it is thought that they were most likely associated with northward subduction of the Yarlung Zangbo River oceanic crust.

关键词

早白垩世/冈底斯弧背断隆带/U-Pb年龄/LA-ICP-MS/流纹岩/锆石

Key words

Early Cretaceous/ Gangdise arc—ridge fault—uplift zone/U—Pb age, LA—ICP—MS, rhyolite/zircon

分类

天文与地球科学

引用本文复制引用

刘伟,李奋其,杨晓勇,袁四化..西藏南木林县罗扎地区早白垩世流纹岩锆石 U-Pb 年龄及地球化学特征[J].中国地质,2012,39(5):1151-1161,11.

基金项目

国家自然科学基金项目(41090372)和国土资源大调查项目(1212010818016)联合资助. (41090372)

中国地质

OA北大核心CSCDCSTPCD

1000-3657

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