华南早燕山期花岗岩是华南大花岗岩省的重要组成部分,其在强度和广度上都胜于其他时期的花岗岩作用,它不仅与华南多期多阶段的地壳运动和板块构造密切相关,同时也是引起区域内钨等多金属大规模成矿作用的主导因素.前人对华南地区早燕山期花岗岩及其地质演化特征研究由来已久,在前人研究的基础上,以华南早燕山期花岗岩为研究对象,总结华南早燕山构造亚阶段花岗岩的岩石学、岩石地球化学及其时空分布特征,探讨早燕山期各侵入阶段花岗岩的耦合关系及其岩浆演化特点与成因类型,以得出华南早燕山构造亚阶段花岗岩的研究进展,为今后该区花岗岩的研究提供可行性建议.%Southern China early Yanshan period granite is an important part of Southern China great granite province, its effect is better than granite in the strength and breadth of the other period, it not only with the Southern China multi-stage of crustal movement and tectonic plates are closely related, but also the main factor causing the regional tungsten polymetallic mineralization in large scale. The predecessor to the Southern China region in the early Yanshan period granite and its geological evolution of long-standing, this paper based on previous studies, in Southern China early Yanshan period granite as the research object, petrology, geochemistry and its temporal and spatial distribution characteristics of Southern China Yanshan tectonic stage summary of early sub granite, and its coupling relationship between magmatic evolution characteristics and genesis of early the Yanshan period granite intrusion stage, research progress to come to Southern China as early as the Yanshan tectonic sub stage granite, for the future study of granite in this area to provide the feasible advice.
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