论文部分内容阅读
调整构造是伸展型沉积盆地和造山带中普遍存在的构造，它与走向构造一起，控制了沉积盆地或造山带的基本轮廓与内部结构。调整构造横切走向构造，并与之共同控盆、控岩、控矿，并间隔开两侧不同的构造样式。它以长时期、多阶段活动，具有高渗透性为主要特征，是控制矿带展布与矿床就位的重要构造，也是固定成矿预测区与找矿靶区的重要依据之一，本文以鲁西、中亚及乌拉山—大青山地区、兰坪─思茅盆地区及右江盆地区为例，论述了调整构造的基本特征及控矿作用。
Tectonic structures are ubiquitous structures in extensional sedimentary basins and orogenic belts that, together with strike structures, control the basic contours and internal structures of the sedimentary basin or orogenic belt. Adjust the structure of cross-strike structure, and with the common control basin, control of rock, ore control, and spaced apart on both sides of the different structural styles. It is a long-term, multi-stage activity, with high permeability as the main feature is to control the distribution of mineralization and deposit in place an important structure, but also fixed ore prospecting area and prospecting target is one of the important basis for this article to Luxi, Central Asia, Wulashan-Daqingshan area, Lanping-Simao basin area and Youjiang basin area as examples, the basic features of adjustment structure and their ore-controlling effects are discussed.