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新疆塔木—卡兰古铅锌矿带矿床属于台缘碳酸盐岩容矿的超低温热液成因。矿床赋存于中泥盆统—下石炭统 3个控矿的由碎屑岩与碳酸盐岩组成的古含水层中。角砾岩、矿体均具有复杂的产状。影响矿体产出的主要因素包括碎屑岩 -碳酸盐岩界面、构造、低温热液交代作用以及容矿围岩的岩性。铅锌、铜、铁矿均是统一的成矿系统的一部分 ,锌 (铅 )矿围岩以碳酸盐岩为主 ,铜矿围岩为紫红色碎屑岩 ,铅矿围岩为灰白色碎屑岩。各主要矿床深部及外围均存在较好的找矿前景。
The Tarim-Kalanchu lead-zinc ore belt in Xinjiang belongs to the ultra-low temperature hydrothermal genesis of carbonate ore-bearing in the margin. The deposits occur in three ancient controlled aquifers consisting of clastic rocks and carbonate rocks in the Middle Devonian-Lower Carboniferous. Breccia, ore body has a complex shape. The main factors influencing the ore body output include the clastic-carbonate interface, tectonism, low-temperature hydrothermal metasomatism and the lithology of the host rock. Lead, zinc, copper and iron ore are all part of a unified metallogenic system. The rock mass of the zinc (lead) ore is mainly carbonate rock, the copper ore surrounding rock is fuchsia clastic rock, and the lead rock surrounding rock is gray broken Rocks. There are good prospects for prospecting in the deep and the periphery of all major mineral deposits.