SHRIMP zircon U-Pb age and O isotopic analysis of the dunite from Kudi ophiolite in the West Kunlun,China  

作　　者：Geng-biao Qiao Wen-ming Li Tian-hu Li 

机构地区：[1]Xi’an Center,China Geological Survey,Northwest China Center for Geoscience Innovation,Xi’an 710054,China [2]Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits,Ministry of Natural Resources,Xi’an 710054,China

出　　处：《China Geology》2023年第1期171-173,共3页中国地质（英文）

基　　金：supported by the National Science Foundation of China(41302051);the Natural Science Foundation of Shaanxi Province(2020JM-311);the project of China Geological Survey(DD20221636,DD20221691)。

摘　　要：1.Objective The West Kunlun in Xinjiang is located on the northwestern margin of the Qinghai-Tibet Plateau(Fig.1a)and at the junction of the Paleo-Asian tectonic domain and the Tethys tectonic domain.It serves as an important area for the study on the geologic evolution of the Karakorum-West Kunlun due to its special tectonic position.

关 键 词：TECTONIC KUNLUN ZIRCON 

分 类 号：P597[天文地球—地球化学]