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黄铁矿矿床的地质概况塞浦路斯岛的中心由特罗多斯火成杂岩体组成,其边部为层状沉积岩.主要的黄铁矿矿床即产于火成杂岩体与上覆沉积物的接触带上或其附近.最下部的沉积层为佩拉佩德希层,该层局部含有火山碎屑-沉积岩,但总的看来,它以独立的单位发育.主要的黄铁矿矿床与该层密切伴生,据推测,二者具有相同的成因.分类与说明浸染状、块状、脉状、洞穴和(或)空隙
Geological Profile of Pyrite Deposits The center of the island of Cyprus is composed of the Troodos volcanic complex with stratigraphic sedimentary rocks on the margins of the main pyrite deposits occurring in igneous complexes and overlying sediments At or near the contact zone.The lowermost sedimentary layer is the Peramedacht layer, which contains volcaniclastic-sedimentary rocks locally, but in general it develops as a separate unit.The main pyrite deposit Closely associated with this layer, it is speculated that the two have the same genetic causes. Classification and description of disseminated, massive, veins, caves and (or) voids