华南燕山期橄榄玄粗岩系岩石研究主要进展  

Research Progress and Main Problems of Yanshan Epoch Shoshonite Series Rock of South China

作　　者：胡倩倩 

机构地区：[1]东华理工大学地球科学学院,南昌330013

出　　处：《能源研究与管理》2017年第4期66-70,共5页Energy Research and Management

基　　金：国家自然科学基金项目(41563001)

摘　　要：华南燕山期橄榄玄粗岩系是区别于拉斑玄武岩系和钙碱性岩系的一组具有特殊性质的岩石组合,其在成因岩石学和区域构造演化研究中具有特殊的意义,并与金属成矿作用关系密切,前人对华南地区燕山期橄榄玄粗岩及其地质演化特征研究由来已久,在前人研究的基础上,以华南燕山期橄榄玄粗岩为研究对象及存在的主要问题,总结华南燕山期橄榄玄粗岩的矿物学、岩石地球化学及其地球化学特征,探讨燕山期橄榄玄粗岩的构造环境和地质证据,以得出华南燕山期橄榄玄粗岩的研究进展,为今后该区橄榄玄粗岩的研究提供可行性建议。South China Yanshan epoch shoshonite series is different from tholeiite series and calc-alkaline rock series combination of a set of characteristics to features of rocks, the formation lithology and tectonic evolution in the study has special significance, and closely related to metal minerlization, predecessors to shoshonite in Yanshan epoch in south China and its characteristics of geological evolution research has a long history, the purpose of this paper is to, on the basis of predecessors＇ research in south China Yanshan epoch shoshonite as the research object and the main problems, summarize south Yanshan shoshonite mineralogy, rock geochemistry and geochemical characteristics, discusses the structure of the Yanshan epoch shoshonite environment and geological evidence, to come to south china, the research progress of Yanshan epoch shoshonite research in the area for the future to provide feasible suggestions.

关 键 词：研究进展 华南 橄榄玄粗岩 

分 类 号：P588.14[天文地球—岩石学]