湖南省煤系石墨成矿规律与找矿方向探讨

Metallogenic law and prospecting direction of coal-based graphite in Hunan Province

  • 摘要: 湖南省侵入岩多,构造较复杂,为系统研究煤系石墨资源成矿规律,在收集现有地质资料的基础上,借鉴国内外煤系石墨矿床的赋存特点,结合湖南省石墨资源的分布特点和开发现状,采用地质调查、生产井调查、采样化验等手段,研究骑田岭岩体和天龙山岩体2个花岗岩体周边现有矿区的矿体地质特征,探讨石墨矿的成因类型和控矿因素。结果表明,研究区石墨矿成因类型为接触变质型,主要控矿因素为岩体的侵位机制、构造作用方式、矿体的形态及变质程度。进而提出了3种石墨赋存模式:兜底式、向斜式、背斜式。提出研究区寻找煤系石墨的突破方向:煤系走向与主压应力方向大致垂直并在岩体附近1.0~1.5 km范围内。

     

    Abstract: There are many intrusive rocks and complex structures in Hunan Province. In order to study the mineralization law of coal-based graphite, on the basis of collecting the existing geological data, drawing on the characteristics of coal-based graphite deposits at home and abroad, combining the distribution characteristics and development status of graphite resources in Hunan Province, using geological surveys, production well surveys, sampling tests, etc., the geological characteristics of the ore bodies in the existing mining areas around the two granite bodies were studied, the genetic type and ore controlling factors of the graphite deposits were explored, the genetic type is contact metamorphism, the main ore controlling factors are the emplacement mechanism of the rock mass, the mode of tectonic action, the shape of the ore body and the degree of metamorphism, furthermore, three modes of graphite occurrence are proposed: pocket bottom type, syncline type and anticline type. The breakthrough direction for graphite exploration was proposed, the strike of organic-rich strata is roughly perpendicular to the direction of the main compressive stress and within 1.0-1.5 km around the rock mass.

     

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