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南秦岭竹山地区粗面质火山岩地球化学特征、LA-ICP-MS锆石U-Pb年龄及其大地构造意义

万俊 刘成新 杨成 刘万亮 李雄伟 付晓娟 刘虹显

地质通报2016,Vol.35Issue(7):1134-1143,10.
地质通报2016,Vol.35Issue(7):1134-1143,10.

南秦岭竹山地区粗面质火山岩地球化学特征、LA-ICP-MS锆石U-Pb年龄及其大地构造意义

Geochemical characteristics and LA-ICP-MS zircon U-Pb age of the trachytic volcanic rocks in Zhushan area of Southern Qinling Mountains and their significance

万俊 1刘成新 1杨成 1刘万亮 1李雄伟 1付晓娟 2刘虹显3

作者信息

  • 1. 湖北省地质调查院,湖北武汉430034
  • 2. 中国科学院武汉岩土力学研究所,湖北武汉430071
  • 3. 武汉工程科技学院,湖北武汉430200
  • 折叠

摘要

Abstract

Basic rock-trachyte belts, trending in NW-SE direction,are widely distributed in Zhushan area of Southern Qinling Mountains, intruding in Silurian strata. Previous researchers conducted detailed studies focused on basic rocks. Compared with the ba⁃sic rocks, the research on trachytic volcanic rocks seems very insufficient, and hence accurate data forming chronologic data are espe⁃cially lacking. The dating of trachytic volcanic rocks from Zhushan area in Southern Qinling Mountains shows that the trachytic vol⁃canic rocks are alkaline series rocks with relatively high Na2O+K2O. Lithophile elements(Ba, Th, U)and high field strength elements (Nb, Ta)are relatively abundant, but the elements such as Sr, Ti and Yb are relatively poor. Rare earth elements(ΣREE, which are rich in light REE and deficient in heavy REE)are relatively high. Combined with the trace element characteristics, it is shown that the trachytic volcanic rocks were formed in a continental rifting environment. The crystallization of trachytic volcanic rocks took place at 430.6±2.7Ma, as shown by the LA-ICP-MS zircon U-Pb dating of trachytic pyroclastic rocks in Zhushan area. The studies show that a strong cleavage activity occurred in the period of early Silurian and formed a deep water basin with rich siliceous and car⁃ bonaceous rock combination in the Zhushan area of Southern Qinling Mountains. Combined with the discovery of ocean island ba⁃salts as well as island arc and oceanic basalts, the authors hold that this region might have developed a small finite ocean basin after Si⁃lurian, and the ocean basin was probably the eastward extension of the Mianlue Ocean in Southern Qinling Mountains. The study of the geochemical characteristics and zircon U-Pb age of the trachytic volcanic rocks provides an important basis for early Paleozoic tectonic evolution in Zhushan area of Southern Qinling Mountains.

关键词

粗面质火山岩/地球化学/LA-ICP-MS锆石U-Pb定年/竹山地区/南秦岭/勉略洋

Key words

trachytic volcanic rocks/geochemical characteristics/LA-ICP-MS zircon U-Pb age/Zhushan area/Southern Qinling Mountains/Mianlue Ocean

分类

天文与地球科学

引用本文复制引用

万俊,刘成新,杨成,刘万亮,李雄伟,付晓娟,刘虹显..南秦岭竹山地区粗面质火山岩地球化学特征、LA-ICP-MS锆石U-Pb年龄及其大地构造意义[J].地质通报,2016,35(7):1134-1143,10.

基金项目

中国地质调查局项目(编号1212011220508、12120113012800)和湖北省国土资源厅项目 (编号1212011220508、12120113012800)

地质通报

OA北大核心CSCDCSTPCD

1671-2552

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