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构造因素是成矿的先决条件,因为,构造运动的动力可促使岩石变质作用的发生,并引起元素的活化迁移,而且构造运动还导致沉积成岩成矿,导致岩浆由深部到地壳上部的运动并成岩成矿。另外,构造运动的结果——构造形迹为矿质的运移提供了通道,为矿质的沉淀提供了场所。 正是基于上述原因,导致了地质工作者对构造与成矿关系的极大兴趣和详细而深入的研究。这项研究的历史粗略分为三个阶段。 第一阶段 着重研究单个构造要素(褶皱断裂、裂隙、接触带)的控矿现象,研究各个构造要素储存矿体的有利部位及其特点。
Tectonics is a prerequisite for metallogenesis because the tectonic movement motivates the metamorphism of rocks and initiates the activation and migration of elements, and the tectonic movement also leads to sedimentary diagenesis and mineralization, leading to the movement of magma from the deep to the upper part of the crust Diagenesis and mineralization. In addition, the result of tectonic movement - tectonic trace provides a channel for mineral migration and provides a place for mineral precipitation. It is for these reasons that led to great interest and detailed and in-depth research by geologists on the relationship between structure and mineralization. The history of this study is roughly divided into three stages. The first stage focuses on the ore-controlling phenomena of single structural elements (fold faults, fissures and contact zones) and studies the favorable parts and characteristics of ore bodies stored by each structural element.