Majoritic Garnets:Key Clues to Kimberlite Formation in South China  

作　　者：Yuhua Zhu William L.Griffin Ruidong Yang Junbo Gao Lei Wang Yuren Zeng Jianshu Chen Miaoling He Hongjuan Rao Yonggang Li Jiawei Zhang 

机构地区：[1]College of Resources and Environmental Engineering,Guizhou University,Guiyang,550025,China [2]Key Laboratory of Karst Georesources and Environment,Ministry of Education,Guizhou University,Guiyang,550025,China [3]Guizhou Geological Survey,Bureau of Geology and Mineral Exploration and Development of Guizhou Province,Guiyang,550081,China [4]CCFS/GEMOC ARC Centre of Excellence,Department of Earth and Environmental Sciences,Macquarie University,Sydney,2109,Australia [5]Wuhan Center,China Geological Survey(Central South China Innovation Center for Geosciences),Wuhan,430205,China [6]101 Geological Team,Bureau of Geology and Mineral Exploration and Development of Guizhou Province,Kaili,556000,China

出　　处：《Journal of Earth Science》2024年第6期2133-2137,共5页地球科学学刊（英文版）

基　　金：supported by the National Natural Science Foundation of China(Nos.41963006,42363006);the Geological Research Project of the Bureau of Geology and Mineral Exploration and Development of Guizhou Province(Nos.QDKKH[2020]26,QDKKH[2024]6,QDKKH[2023]1)。

摘　　要：Kimberlite,which is the primary host rock for diamonds,originates from the deepest sources of all the mantle-derived magmas(Giuliani et al.,2023;Foley et al.,2019).This feature provides a vital perspective to explore Earth's internal structure and evolution.The first primary diamond deposit discovered in China was the East No.1 kimberlite pluton(D1)in Maping(26°56′08″N,108°17′07″E),located on the southeastern margin of the Yangtze Craton(Figure 1).

关 键 词：evolution MAGMA southeastern 

分 类 号：P619.241[天文地球—矿床学]