地壳应力状态地质学研究现状和展望

doi:10.11867/j.issn.1001-8166.1992.06.0036

地球科学进展 ›› 1992, Vol. 7 ›› Issue (6): 36 -. doi: 10.11867/j.issn.1001-8166.1992.06.0036

地壳应力状态地质学研究现状和展望

姜刚仁

江苏省地震局 210014

收稿日期:1991-10-16 修回日期:1992-03-16 出版日期:1992-11-01

PRESENT CONDITION AND PROSPECT OF RESEARCH ON CRUSTAL STRESS STATE BY GEOLOGIC METHOD

Jiang Gangren

Seismological Bureau of Jiangsu Province，210014

Received:1991-10-16 Revised:1992-03-16 Online:1992-11-01 Published:1992-11-01

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对研究地壳应力状态的地质学方法作了回顾与展望;指出该方法已经成为研究地壳应力状态的主要方法，并分析了影响该方法发展的三个问题;还指出现代构造遥感地质研究已为地质学方法研究地壳应力状态开辟了新途径。

关键词: 地壳应力状态, 地质学方法, 现代构造, 遥感地质

This article briefly makes a review of present condition and prospect on geologic method studied crustal stress state.
    First,the present arthor points out that geologic method has become a main method studied crustalstress state,after half century straits have involved.
    Secondly ,three factors effected the development of geologic method have been analyzed.
    Thirdly , a research of recent tectonics by remote sensing geology technique is summarized. It suggests that the technique has opened up a new good prospect for geologic method.
      Finally,a new good prospect of geologic method studied crustal stress state has described.

Key words: Crustal stress state , Geologic method, Recent tecto tics , Remote sensing geology technique

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