摘要
On the basis of a study of the Muggar Kangri Group-complex and its cover sediments in the central segment of the Bangong Co-Nujiang River suture zone, Tibet, it has been ascertained that the Shamuluo Formation (J3-K1s) consists of sediments of a relict sea basin overlying unconformably on the Muggar Kangri Group-complex. From above, the authors think that the central segment of the Bangong Co-Nujiang River suture zone closed in the Late Jurassic. This provides new evidence for the study of the evolutionary process of the Tethys Ocean.
On the basis of a study of the Muggar Kangri Group-complex and its cover sediments in the central segment of the Bangong Co-Nujiang River suture zone, Tibet, it has been ascertained that the Shamuluo Formation (J3-K1s) consists of sediments of a relict sea basin overlying unconformably on the Muggar Kangri Group-complex. From above, the authors think that the central segment of the Bangong Co-Nujiang River suture zone closed in the Late Jurassic. This provides new evidence for the study of the evolutionary process of the Tethys Ocean.
出处
《地质通报》
CAS
CSCD
北大核心
2004年第2期193-194,共2页
Geological Bulletin of China
基金
中国地质调查局青藏高原1:25万班戈县幅区域地质调查部分成果
