黑龙江省完达山萌裂谷演化与铜金找矿  

On the evolution of Heilongjiang Wandashan embryo rift and its relation to gold and copper deposit

作　　者：史瑞民[1] 孙传斌[1] 

机构地区：[1]黑龙江省有色金属地质勘查702队,黑龙江牡丹江157021

出　　处：《吉林地质》2007年第2期23-26,共4页Jilin Geology

摘　　要：本文对完达山地区大地构造认识进行了新的探讨。该区在大陆边缘裂谷的演化及构造-岩浆活动的改造叠加过程中,孕育着铜金矿产的成矿作用。本区铜金矿产的形成与海底火山喷发和喷气作用密切相关。通过对完达山区构造演化及成矿作用的分折,提出了该区铜金矿产新的成矿作用方式及找矿方向。The new approach on tectonic is made in the Wandashan area in this paper. The gold and copper mineralization was associated with evolution of the continental margin rift and tectonomagmatic reformation and superposition in this area, and the forming of gold and copper deposit is very close relation to sea- floor volcanic eruption and exhalation. On the basis of studies on tectonoevolution and metallization, the new ore- forming mechanism and prospecting direction is proposed in the Wandashan area.

关 键 词：大陆边缘裂谷 成矿作用 铜金找矿方向 黑龙江完达山 

分 类 号：P618.41[天文地球—矿床学]