焦家成矿带Ⅲ号矿体群成矿特征浅析及其找矿意义
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Metallogenic Characteristics and Prospecting Significance of No.3 Ore Body in Jiaojia Metallogenic Belt
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    摘要:

    焦家成矿带自被发现以来,一直备受关注,现矿体控制深度已超2000m,至今探明金资源储量已超千吨。焦家成矿带为热液型金矿床成矿带,具有明显的蚀变分带现象,通常根据其蚀变分带特征对矿体群进行划分,将下盘蚀变带最外层的黄铁绢英岩化花岗岩带中的矿体划为Ⅲ号矿体群。以往对1000m以上矿体的矿体特征及成因也做了较为详细的总结和剖析,但其深部Ⅲ号矿体群的研究资料较少。该文搜集焦家成矿带中段各矿床的勘查化验资料,针对焦家成矿带浅部、中部及深部的Ⅲ号矿体群的产出状态、矿化类型进行对比研究,分析其矿床成因,根据其宏观和微观特性加上化验结果,结合区内构造等因素对其矿体成因进行浅析,对深部Ⅲ号矿体群产出状态进行推测,指出Ⅲ号矿体群的富集规律及其成矿集中期。认为深部Ⅲ号矿体群内含矿裂隙倾角集中在40°~69°、80°~90°,并且存在大量与主矿体倾向相同或相反的陡倾矿体。黄铁绢英岩化花岗岩带蚀变相对较弱,其矿化以网脉状、细脉状、脉状及团块状为主。

    Abstract:

    Since Jiaojia metallogenic belt was found, it has been highly concerned. In recent years,accompanying with the increased investment on geological exploration,there is a prospecting breakthrough in the deep area of the metallogenic belt (below -1000m),and now there are more than one thousand tons of proved gold resources. The controlled depth is in excess of -2000m. Jiaojia metallogenic belt is a hydrothermal type gold deposit with obvious alteration zoning. Usually, the ore bodies are divided into groups according to the characteristics of the alteration zoning. The ore bodies in beresitization granite alteration belt in the outermost layer in the lower part of the alteration belt are divided into No.Ⅲ ore body group. The alteration of beresitization granite belt is relatively weaker and its mineralization is present as net veined, fine veined, veined and crumby. Characteristics and genesis of the ore bodies in the depth of -1000m have been summarized and analyzed, but there are few researches on the deep areas of No.Ⅲ ore body group. In this paper, the prospecting data of the deposits in the middle part of Jiaojia metallogenic belt have been collected. occurrence forms and mineralization types of No.Ⅲ ore body group in the shallow, middle and deep part of Jiaojia metallogenic belt have been compared and studied, and the genesis of the deposits have been analyzed. According to macroscopic and microscopic characteristics and the test results, combining with structure factors in the area, the genesis and the enrichment regularity of the ore bodies have been analyzed and summarized, and the occurrence of No.Ⅲ ore body group in the deep area has been conducted, the enrichment regularity and the mineralization concentration period of No.Ⅲ ore body group have been pointed out.

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杨真亮,解天赐,刘天鹏,张坤,李瑞翔,王永庆.焦家成矿带Ⅲ号矿体群成矿特征浅析及其找矿意义[J].山东国土资源,2017,33(9):

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  • 在线发布日期: 2017-08-22