摘要
小江断裂带中段的盆地可以划分为三个阶段，即Ｎ２—Ｑ１、Ｑ２末—Ｑ３初和Ｑ３—Ｑ４。这些盆地受小江断裂带左旋走滑运动控制。
The basins in the central part of the Xiaojiang fault zone can be divided into the three stages, from N 2 to Q 1, from late Q 2 to early Q 3 and from Q 3 to Q 4; and these basins are controlled by left-lateral strike slip motion of the Xiaojiang fault zone.
出处
《地震研究》
CSCD
北大核心
1998年第1期58-64,共7页
Journal of Seismological Research
