山东省金刚石原生矿地质特征和成矿规律浅析

    A study of metallogenic regularity and geological characteristics of primary diamond deposits in Shandong Province

    • 摘要: 金刚石具有优异的物理化学性能,是新兴产业发展的重要原材料。金刚石是山东省的优势矿种之一,目前对于山东省金刚石原生矿的成矿时代还存在许多争论。通过对山东省金刚石原生矿地质特征进行系统阐述,对其空间分布规律、成矿地质条件、成矿时代等方面进行探讨,总结认为: 山东蒙阴3个金刚石原生矿岩带(常马岩带、西峪岩带和坡里岩带)的中心点相连后,其连线呈一NW向突出的折线,具有方向性、等距性及左列式展布规律; 3个岩带的岩性由南向北含矿性具有南富北贫、中间富两边贫等变化规律; 确定其原生矿属于受超基性岩控制的脉状、管状矿体,成因类型为岩浆型,其侵入时代主要为中生代。通过对其成矿环境、成矿规律和成矿时代进行总结和讨论,为今后金刚石原生矿找矿提供了重要依据。

       

      Abstract: Diamond has excellent physical and chemical properties, which is an important raw material for the development of new industries. The diamond resource is a kind of dominant mineral in Shandong Province, and the study of diamond deposits in Shandong is still under controversy. Through the systematic explanations of diamond deposits in Shandong Province, the authors in this paper discussed the distribution regularity, mineralization geological condition and mineralization age, and summarized the central points of three diamond primary ore belts in Mengyin, which the connecting line is a broken line protruding from the north to the west after connection, with directionality, equidistance and left-column distribution regularity. The lithology of the three rock belts changes from south to north with the regularity of rich in the south and poor in the north, rich in the middle and poor in both sides. It is believed that the shape of the primary diamond deposit in Mengyin area of Shandong Province were veined and tubular, and the genetic type is magmatic, of which the invasion era was mainly in Mesozoic. This research would provide important reference in diamond prospecting, by summarizing the minerogenetic environment, minerogenetic regularity and minerogenetic epoch.

       

    /

    返回文章
    返回