班公湖-怒江断裂带的形成——二论大陆地壳层波运动

详细信息

收稿日期: 1998-04-28

ON THE FORMATION OF THE BANGONG-CO-NUJIANG FAULT ZONE

Received Date: 28 April 1998

摘要: 班公湖-怒江断裂带是由4条断层组成的3个巨大弧形断裂带,带中发育晚三叠世至白垩纪沉积地层。自北而南,各断裂带及其南北两盘,有相继隆升的剥蚀带和与之相伴的凹陷沉积带,表明该区地壳曾发生强弱起伏、缓慢交替的层波运动。
- 班公湖-怒江断裂带 /
- 沉积地层 /
- 层波运动
Abstract: The Bangong-Co-Nujiang fault zone consists of four arcuate faults.The zone was subsided successively from north to south to receive sediments derived from the two immediately adjoining uplifted flanks in the late Triassic to the Cretaceous.It was the results of undulated earth's movement.
- Bangong-Co-Nujiang fault zone /
- sedimental bed /
- undulated earth's movement