沉积学报2000，Vol.18Issue(3)：445-448,4.
鄂尔多斯盆地早古生代波状构造及其古地理意义
Wave Structre in Paleozoic Era of Ordos Basin and Its Significance in Paleogeography
方国庆 1刘德良 1冯江2
作者信息
- 1. 中国科学技术大学地球与空间科学系合肥 230026
- 2. 中国科学院兰州地质研究所兰州 730000
- 折叠
摘要
Abstract
Undulation is one of the fundamental models of the geological effect , the undulation motion and variation inshape of earth crust is an geologic facts. In this paper, the undulation theory is applied to discuss the structure, de-posit and paleogeography pattern of Paleozoic of Ordos Basin. The units of wave structure of Ordos and its neigb-houring areas are divided as: Yinshan wave trough, Yimeng wave crest, Central wave trough, Weibei wave crest,Qingling wave crest, Alashan wave crest, Helan wave trough, Central doming wave crest, Eastern wave trough andKelan wave crest structure belt. The compound of Central wave trough and Eastern wave trough formed eastern saltdepression. This area has also formed the big center of hydrocabon source that are the most important in under Pa-leozoic group of Ordos Basin. Central doming wave crest structure belt and Central wave trough structure belt wereformed Dinbian compound areas, which make the central doming appear saddle in Dinbian. It also reasonably ex-plains the phenomenon that Central doming is suspended in Dinbian area.关键词
构造沉积古地理波动构造古生代鄂尔多斯盆地Key words
wave structure Paleogeography Early Paleozoic Ordos Basin分类
天文与地球科学引用本文复制引用
方国庆,刘德良,冯江..鄂尔多斯盆地早古生代波状构造及其古地理意义[J].沉积学报,2000,18(3):445-448,4.
