地质论评2025，Vol.71Issue(3)：1011-1019,9.DOI:10.16509/j.georeview.2024.10.085
含金刚石的金伯利岩和钾镁煌斑岩研究的科学问题
Scientific questions in the study of diamondiferous kimberlite and lamproites
摘要
Abstract
Besides their economics,geoscientists can study geology in deep mantle through diamondiferous kimberlites or diamondiferous Lamproites,and there have been many advances in this area worldwide.Surface element cycling and geological events in the mantle were discovered through inclusions and fluids contained in diamonds.The C—P—T—PH2Oconditions for determining the origin of mantle magma were determined through DKL mantle xenoliths and xenolith crystals.The scientific research value and economic value of DKL have also driven the discovery of multiple DKL fields in Angola,Russia,India,central Canada,and other regions,thereby promoting deep geological research.This article provides a brief overview of global research achievements in this area.关键词
地幔/金刚石/金伯利岩/钾镁煌斑岩/捕虏体Key words
mantle/diamond/kimberlite/lamproites/xenolith引用本文复制引用
丁毅,肖丙建,侯征,王天意,王玉峰,杜现福,宗传攀..含金刚石的金伯利岩和钾镁煌斑岩研究的科学问题[J].地质论评,2025,71(3):1011-1019,9.基金项目
本文为河北地质大学与山东省地质矿产勘查开发局第七地质大队合作项目的成果. This paper is supported by the cooperation project between Hebei GEO University and the 7th Geological Team of Shandong Geological and Mineral Exploration and Development Bureau （）
