华北盆地(北部)中、新生代构造应力场及盆地形成发展机制分析

CENO-MESOZOIC TECTONIC STRESS FIELD OF NORTH CHINA BASIN AND MECHANISM OF FORMATION AND DEVEELOPMENT OF BASIN

庄培仁 徐成彦 吕新媛 张延 候钢 王维襄 韩玉英 陈明佑

Zhuang peiren Xu Chengyang Lü Xingyuan Zhang Yan Hou Gang Wang Weixiang Han Yuying Chen Mingyou

武汉地质学院北京研究生部

Baijing Graduate.School, Wuhan College of Geology

华北盆地(北部)其范围大体相当渤海湾盆地,本文试图通过华北盆地两侧山区构造应力测量,联系盆地地质结构、深部特征和各个时期所处的地球动力学背景,采用有限元法对盆地中、新生代构造应力场进行数值模拟,分析盆地形成发展机制。

This paper discusses and probes the evolution of basin structrues, and analyses the mechnaism of basin subsidence, which depends on the fea-tures of geological structures, geophysics, and those of the deeper crust and the stress variation of the surrounding high land. The knowledge is achieved as follows: I. The both sides of the basin are bounded by the Tanlu Faulting Belt and Taihang Structure Belt whose structures have been complicated and are of large size with secular activities. Since Mesozoic, the two belts have mainly undergone three stages of the stress field evolution. Ⅱ. The three evolutional stages correspond to the three different types of structure mechanisms. 1) Early, Middle Yanshanian, the type of folding faulting basin on the background of intraplate uplift; 2)Late Yanshanian-Early Xishanian, the type of extensional graben-half graben basin under the con dition of intraplate subsidence; and 3)Late Xishanian, the type of de pressing of large scale. The first two types are closely related to the occurrence of oil and gas. Ⅲ. The values from the planar and the vertical basin stress fields are simulated by adopting a program of Limited Element Increment. The re-sults, in one respect,support the thesis that North China Basin has under-gone two different stages of stress fields and indicate: 1) the controll-ing factors of the previously existing faults on the basin; 2) the possible weak parts of rock deformation and damages in shallow strara of the crust; and 3) the critical factors of vertical force coming from deeper crust dur-ing the formation of the basin.

https://doi.org/10.11781/sysydz198503200