活化(地洼)构造理论的历史回顾与发展现状(一)——地壳演化及成矿的递进律

来源期刊：中南大学学报(自然科学版)1991年第5期

论文作者：陈国达

文章页码：473 - 479

关键词：地洼学说; 递进说; 成矿

Key words：Diwa Theory; progressive theory; metallogeny

摘    要：本文回顾了地洼学说的形成与发展历程,阐述了其发展现状。在现阶段,地洼学说已逐步发展成为具有五个组成部分和两个衍生学科的比较复杂的大地构造与成矿学理论体系。这里论述了:(1)活化地区(地洼区)的概念——阐述这个构造单元的地质、地球物理及地球化学特征、鉴别标志、时空分布规律和成矿特点;(2)地壳动定转化递进说——阐明地壳构造发展的一般性规律,即动定递进律;(3)递进(地洼)成矿理论——论述地壳中成矿作用演化规律与地壳构造演化规律的关系、构造成矿概念以及多因复成矿床。

Abstract: The writer looks back on the course of the formation and development ofDiwa Theory and expounds its recent developments. At present, Diwa Theory iscomposed of five parts and hast wo derivative disciplines. The paper deals with thefollows: (1) The concept of Activated. Region (Diwa). It expounds the geologic,geophysical and geochenical features, distinguishing criteria, temporal-spatialdistribution regularities, and metallogenic regularities of this new found tectonicelement. (2) Theory of progression with transformation between active and"stable" regions. This theory expounds the general rule of tectonic evolution of the crust, it is called "law of progression" . (3) Progressive (Diwa)netallogenic theory. It expounds the correlation between evolutionary regu-1arities of metallogenesis in the crust and evolutionary regularities of crustal tectonics, concepts of tectonic netallogeny, and polygenetic compound metallogenesis.