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西藏崩纳藏布砂金矿地质特征及找矿方向
引用本文:邹依林,李蒙文,葛良胜,张学军,李振华.西藏崩纳藏布砂金矿地质特征及找矿方向[J].黄金地质,2002,8(2):8-14.
作者姓名:邹依林  李蒙文  葛良胜  张学军  李振华
作者单位:1. 武警黄金地质研究所,河北,廊坊,065000
2. 武警黄金第二总队,河北,廊坊,065000
摘    要:通过对区域地质背景、第四纪典型地貌及矿床地质特征等的研究,发现崩纳藏布砂金矿具有成矿时代新、成矿期短、物质来源多样性等特点。成矿过程明显具有2个阶段:早期可能与斑岩型铜-金-多金属矿床有关,含Au配合物近距离活化、迁移,在适宜的地方堆积成矿;晚期在原地吸收侧向补给的第四系含Au沉积物,次生富集成为富矿。

关 键 词:矿金矿  地质特征  找矿方向  西藏  表生富集  成矿时代  空间分布
文章编号:1006-558X(2002)02-0008-07

Geological features of gold placer and prospecting guide in Bengnazangbu, Tibet
ZOU Yi lin ,LI Meng wen ,GE Liang Sheng ,ZHANG Xue jun ,LI Zhen hua.Geological features of gold placer and prospecting guide in Bengnazangbu, Tibet[J].Gold Geology,2002,8(2):8-14.
Authors:ZOU Yi lin  LI Meng wen  GE Liang Sheng  ZHANG Xue jun  LI Zhen hua
Institution:ZOU Yi lin 1,LI Meng wen 2,GE Liang Sheng 1,ZHANG Xue jun 1,LI Zhen hua 1
Abstract:Characters with new metallogenic epoch and short mineralization period and multiple mass sources are discovered by studing regional geolegic setting and geomorphologic landscope of Quatenary system and geological featues of mineral deposit in the gold placer of Bengnazangbu. The ore forming process can be diveded into two stages obviously. In the early course, it may be related with porphyry Cu Au multimetallic ore deposit, complexes of gold bearing transport and activate in short distance, pile up and form ore in the sure places. In the later course, it absorbed lateral feeder sediments of Quaternary system in the same places, enriched and formed rich ore finally.
Keywords:gold placer  geological feature of deposit  propecting guide  Tibet
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