摘要
研究构造运动及构造层特征是查明地壳构造演化历史的重要证据。从福建省目前建立的地层序列分析，自古元古代以来，省内初步可划分出15次构造运动，并分别归属迪口、晋宁、加里东、印支、燕山、喜马拉雅6个构造旋回。文中对前震巳纪地层首次建立构造地层单位，并阐述了各构造运动、构造旋回、构造阶段和构造层、亚构造层的基本特征，较系统地反映了福建省地壳构造演化历史。
Study of the characteristics of tectonic movements and structural layers is of significancein ascertaining the history of the crustal tectonic evolution. As analysing the stratigraphicsequance of Fujian Provine, fifteen tectonic movements since the Proterozic era can be dividedand respectively belong to the six tectonic cycles. The author first established the tectonostratigraphic units for Pre-sinian stata in Fujian Province and made a systematic expositionon the basic characteristics of the tectonic movements, tectonic cycles, tectonic stages, andstructural and sub-structural layers, which systematically reflected the crustal and tectonicevolution of Fujian Province.
出处
《福建地质》
1998年第3期115-130,共16页
Geology of Fujian
关键词
构造地层单位
构造运动
福建
构造层划
tectono-stratigraphic unit, tectonic movement, structural layer, FujianProvince
