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西藏羌塘地体南部多龙增生杂岩早三叠世辉长岩的发现及其地质意义

段瑶瑶 李亚林 段志明

地质通报2016,Vol.35Issue(6):887-893,7.
地质通报2016,Vol.35Issue(6):887-893,7.

西藏羌塘地体南部多龙增生杂岩早三叠世辉长岩的发现及其地质意义

The discovery of the Early Triassic gabbro rocks of the Duolong accretionary complexes in southern Qiangtang terrane of Tibet and its geological significance

段瑶瑶 1李亚林 1段志明2

作者信息

  • 1. 中国地质大学地球科学与资源学院,北京100083
  • 2. 中国地质调查局成都地质调查中心,四川成都610082
  • 折叠

摘要

Abstract

The outcropped Late Triassic-Jurassic accretionary complexes are located along northern Bangong Co-Nujiang suture zone where a large subduction-type Duolong porphyry copper-gold ore concentration area is developed. Bulk-rock major and trace elements, Sr-Nd isotope and LA-ICP-MS zircon U-Pb data are reported for gabbro rocks sampled from the Duolong accretionary complexes. The 206Pb/238U age of zircon in the gabbro analyzed by LA-ICP-MS is 246.0±1.4Ma, which represents the crystallization age of the magma. Na, Mg, LREE and large ion lithophile elements (Ba, U, La and Sr) are concentrated whereas Ti, K and high-field strength elements (Nb and Ta) are deficient. These characteristics suggest that the geochemistry of the gabbro is similar to that of the island arc type basalt. The isotopic compositions of the Sr and Nd ( (87Sr/86Sr)i=0.707605~0.709778, (143Nd/144Nd)i=0.512515~0.512678, and TDM2=0.54~0.99Ga) suggest that gabbro is developed on the arc in an intraplate environment. It is considered that the end of early Triassic igneous activity probably resulted from the northward subduction of the Bangong Co-Nujiang Ocean crust which interacted with the lithospheric mantle material. The discovery and understand ing provide the northward subduction of the Bangong Co-Nujiang ocean crust in early Triassic with important evidence of magma tism.

关键词

LA-ICP-MS锆石U-Pb年龄/地球化学特征/岛弧辉长岩/班公湖-怒江缝合带

Key words

LA-ICP-MS zircon U-Pb ages/geochemical characteristics/island arc gabbro/Bangong Co-Nujiang suture zone

分类

天文与地球科学

引用本文复制引用

段瑶瑶,李亚林,段志明..西藏羌塘地体南部多龙增生杂岩早三叠世辉长岩的发现及其地质意义[J].地质通报,2016,35(6):887-893,7.

基金项目

国家自然科学基金项目(批准号41572188)和中国地质调查局项目 ()

地质通报

OA北大核心CSCDCSTPCD

1671-2552

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