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对马山金矿床的研究表明,化探累乘晕异常可作为金矿的找矿标志.累乘晕异常在各类地质体(灰岩、砂岩、岩体、硫铁矿等)上都各有其自身特征,但由于各种地质作用多次活动的影响,常使得累乘晕异常复杂化.然而,在一个地质体上各次成矿作用形成的累乘晕异常具有不同的频率分布特征;在不同的地质体上同一次地质作用显示的累乘晕,其频率分布特征具有同一性.这就在一定程度上为研究成矿作用历史及矿床与构造岩浆活动的关系提供了地球化学信息.
The research on the Mashan gold deposit shows that the cumulative anomalous halo can be used as a prospecting indicator for the gold deposit, and the cumulative motion halo anomaly has its own features on various geological bodies (limestone, sandstone, rock mass, pyrite, etc.) However, due to the influence of multiple activities of various geologic functions, it is often complicated to complicate the multiplicative halo formation. However, the accumulated halo anomaly formed by various metallogenetic events on a geological body has different frequency distribution characteristics; at The same geologic effect on different geologic bodies shows that the frequency distribution features are identical, which provides geochemical information for studying the history of mineralization and the relationship between ore deposits and tectonic magmatism.