湘南骑田岭锡矿成矿规律探讨

    Exploration on the ore-forming regularities of tin deposits in Qitianling area,southern Hunan

    • 摘要: 骑田岭地区位于炎陵-郴州-蓝山北东向基底构造岩浆岩带中部,是南岭中段多金属成矿带的重要组成部分。现已查明111—333锡资源量101.3×104t,近期又发现了具超大型找矿前景的芙蓉锡矿田。锡矿类型可分为气化高温热液型锡矿、高—中温热液型锡矿、次火山热液型锡矿及冲积型砂锡矿四大类7个亚类,构成了一个较完整的成矿系列。各类锡矿是多次构造-岩浆活动综合作用的产物,燕山早期晚阶段及燕山晚期早阶段是主成矿期。特殊的地质构造背景造就了区内锡矿“带状分布、成群产出、等距展布”的空间分布规律,也展示了巨大的找矿潜力。

       

      Abstract: Qitianling area which located at the middle part of the Yanling-Chenzhou-Lanshan NE-trend-ing tectonomagmatic belt of basement is an important part of polymetallic metallogenic belt in the middle of Nanling region.It is in the area that Furong ore field with prospect of prospecting in super-large tin deposit has been found lately,and the111-333resources of tin have been identified about one million and thirteen thousand tons ;the types of the tin deposits can be divided into four types,the pneumato-hypothermal type,the hypo-mesothermal type,the volcanogenic hydrothermal type and the alluvial type,and seven subtypes,all of which formed nearly a complete metallogenic series.Where,the tin deposit of any type is the product of several times of tectonizations and magmatisms ,its main epoch of mineraliza-tions are at an late stage of early and an early stage of late Yanshanian period;and there are distributive regularities of place on distributing the tin ore among belt,group and being equal distance,for the special geologic structural background,and showed an excellent prospect of prospecting.

       

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