浅析樟村金矿地质特征及找矿方向  

Analysis of geological features and prospecting direction in Chang Cun gold mine

作　　者：肖应龙 李首钢 XIAO Ying-long;LI Shou-gang(Jiangxi nonferrous geology four team,Jingdezhen 333001,China)

机构地区：[1]江西有色地质四队,江西景德镇333001

出　　处：《世界有色金属》2018年第11期63-64,共2页World Nonferrous Metals

摘　　要：普查区位于钦杭成矿带的东段中部,大地构造位置地处扬子板块与华夏板块碰撞结合部,定位于赣东北深大断裂带西缘乐安江-梅林大断裂中,岩浆岩出露比较广,以中酸-酸性岩浆岩为主,侵入期以燕山期为主,岩性自西向东依次分布有石英闪长岩、花岗闪长岩、花岗斑岩、细碧角斑岩。the census area is located in the middle east part of the qinhang metallogenic belt.The tectonic location is located at the collision junction between the Yangzi plate and the Huaxia plate.It is located in the Yue an River Meilin fault in the western margin of the deep fault zone of Northeast Jiangxi Province.The magma and Iwade dew are wide and mainly acid acid magmatic rocks,the main intrusion period is Yanshan period,and the lithology from west to east to the East.The secondary distribution is quartz diorite,granodiorite,granite porphyry and gabbro porphyry.

关 键 词：钦杭成矿带 扬子板块与华夏板块 细碧角斑岩 

分 类 号：P618.51[天文地球—矿床学]