摘要
笔者在研究有关文献和参加一些学术会议后发现.地洼学说近十余年来进展显著,科研成果累累.被称为当代最有生命力的学科之一,但系统地研究其成长过程尚欠缺.为了促进地球科学的不断发展。总结经验与教训。扩大学科间的交流.本文重点论述了地洼学说产生的历史背景:进展阶段与特点;发展总体趋势;学说的前景和展望等问题.
After studying the related documents and attending some academic conFerences, the author has found that in the past decade diwa theory has been possessing an amazing speed of development and great achievements and is regarded as one of the vitalest sciences, but it still lacks a systematic study of its growing process. In order to promote the constant development of geosciences, sum up the experiences and lessons and enlarge exchanges in sciences, this paper discusses emphatically the historical background of generation, general trend and prospects of diwa theory.
出处
《大地构造与成矿学》
EI
CAS
CSCD
1992年第4期405-409,共5页
Geotectonica et Metallogenia
关键词
地洼学说
地洼
地台活化
phenomenon of activation, activation of platform, diwa region (activizing region), tectono-magmatic activity, theory of progression, hypothesis of mantle creep
