刍议黔中隆起及其形成过程中的均衡沉陷作用  

ON THE CENTRAL GUIZHOU UPLIFT AND THE ISOSTATIC SUBSIDENCE IN THE PROCESS OF ITS FORMATION

作　　者：戴新春[1] 黄友庄[1] 

机构地区：[1]贵州工业大学资源工程系

出　　处：《贵州工业大学学报（自然科学版）》1998年第2期23-26,共4页Journal of Guizhou University of Technology(Natural Science Edition)

摘　　要：地史时期中黔中隆起在曾两次明显的上隆于海平面之上，本文着重论述了红花园期末的这次上隆以及相应的均衡沉陷作用。指出均衡沉陷作用在研究黔中隆起及古构造中是不容忽视的重要因素；而且，均衡沉陷与构造上隆两者间的对立统一，也是控制沉积物质变化的制约因素之一。It is generally thought that the Central Guizhou Uplift was first formed in the end of Ordovician.In this paper,we suppose that the first uplifting happened in the end of the Honghuayuan Age of the Lower Ordovician and that the isostatic subsidence and the tectonic uplifting played an importamt role in the formation and development of the Central Guizhou Uplift.

关 键 词：黔中隆起 奥陶纪 形成过程 均衡沉陷作用 

分 类 号：P542.1[天文地球—构造地质学]