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云南南华地区大龙潭金矿之发现及其矿床地质特征
引用本文:杨伟光,郭远生,王训练,顾雪祥,王根厚.云南南华地区大龙潭金矿之发现及其矿床地质特征[J].地质通报,2006(Z2).
作者姓名:杨伟光  郭远生  王训练  顾雪祥  王根厚
作者单位:云南地质矿产资源股份有限公司,云南地质矿产资源股份有限公司,中国地质大学地球科学与资源学院,中国地质大学地球科学与资源学院,中国地质大学地球科学与资源学院 云南昆明650051,云南昆明650051中国地质大学地球科学与资源学院,北京100083,北京100083,北京100083,北京100083
摘    要:简要报道了在云南省南华县发现的大龙潭金矿床的地质特征。大龙潭金矿主矿体长360m,斜深大于60m。矿体形态呈似层状,局部呈透镜状,形态变化中等。矿体厚度的变化系数为71.2%~149.6%,较稳定;Au品位变化系数为87.5%~218%,较均匀;矿体产于向斜两翼,被断层错动,构造影响程度中等。据以上矿床地质特征将该矿区确定为Ⅱ勘查类型。

关 键 词:金矿床  矿床地质特征  大龙潭  南华县  云南

Discovery of the Dalongtan gold deposit in the Nanhua area,Yunnan,China and its geological characteristics
YANG Wei-guang,GUO Yuan-sheng,WANG Xun-lian,GU Xue-xiang,WANG Gen-hou . Yunnan Geology and Mineral Resources Co. Ltd.,Kunming ,Yunnan,China, . School of Earth Sciences and Mineral Resources,China University of Geosciences,Beijing ,China.Discovery of the Dalongtan gold deposit in the Nanhua area,Yunnan,China and its geological characteristics[J].Geologcal Bulletin OF China,2006(Z2).
Authors:YANG Wei-guang  GUO Yuan-sheng    WANG Xun-lian  GU Xue-xiang  WANG Gen-hou Yunnan Geology and Mineral Resources Co Ltd  Kunming  Yunnan  China  School of Earth Sciences and Mineral Resources  China University of Geosciences  Beijing  China
Institution:YANG Wei-guang1,GUO Yuan-sheng1,2,WANG Xun-lian2,GU Xue-xiang2,WANG Gen-hou2 1. Yunnan Geology and Mineral Resources Co. Ltd.,Kunming 650051,Yunnan,China, 2. School of Earth Sciences and Mineral Resources,China University of Geosciences,Beijing 100083,China
Abstract:The paper briefly reports the geological characteristics of the Dalongtan gold deposit discovered in Nanhua County, Yunnan Province. The main orebody of the deposit is 360 m long with a dip width of >60 m. The orebodies are bed-like in shape and locally lenticular, showing moderate variation in shape. The thickness of the orebodies is relatively uniform, with a variation coefficient of 71.2-149.6%. The gold grade is relatively homogeneous, and its coefficient of variation is 87.5-218%. The orebodies occur in both limbs of a syncline and are disrupted by faults, undergoing moderate structural influence. According to the above-mentioned geological characteristics, the gold district reported here is considered to be of exploration type II.
Keywords:gold deposit  geology of ore deposit  Yunnan  Nanhua County  Dalongtan
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