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铜的内生富集,可形成超基性岩铜镍矿床、斑岩铜钼矿床、玄武岩铜矿床、火山岩黄铁矿型铜矿床、矽卡岩多金属铜矿床、各种中低温热液脉铜矿床以及罕见的碱性超基性岩-碳酸岩铜矿化等等.它们有的是相互联系制约的地质-地球化学统一体系的各个侧面,有的是不同阶段、不同位置的构造岩浆活动的产物,是铜的地球化学性质和行为在不同内生作用条件下的表现,因而各有其成矿地球化学机制、伴生矿种和找矿标志.
Copper endogenous enrichment, can form ultramafic rock copper nickel deposit, porphyry copper molybdenum deposit, basalt copper deposit, volcanic pyrite copper deposit, skarn polymetallic copper deposit, all kinds of low temperature Hydrothermal vein-copper deposits, and rare alkaline ultrabasic rocks - carbonate rock mineralization, etc. They have various aspects of a unified geo-geochemical system that are interconnected and constrained, and some are tectonic magmatic activities at different stages and locations Is the product of the geochemical behavior and behavior of copper under different endogenous conditions, and thus each has its own metallogenetic geochemical mechanism, associated minerals and prospecting indicators.