雅鲁藏布中新生代深水沉积盆地形成和演化(Ⅰ)——喜马拉雅造山带沉积特征及演化

收稿日期: 1992-11-21

刊出日期: 1993-02-28

FORMATION AND EVOLUTION OF THE MESOZOIC AND CENOZOIC DEEP-WATER SEDIMENTARY BASINS ALONG THE YARLUNG ZANGBO RIVER(Ⅰ): SEDIMENTARY CHARACTERISTICS AND EVOLUTION OF THE HIMAIAYAN OROGENIC ZONE

Received Date: 21 November 1992

Publish Date: 28 February 1993

摘要: 通过对喜马拉雅三叠纪到第三纪区域沉积特征分析,阐明了雅鲁藏布喜马拉雅特提斯造山带从裂谷—被动大陆边缘—前陆盆地的沉积盆地演化史。随着以雅鲁藏布带为代表的喜马拉雅特提斯打开,三叠纪到早侏罗世为特提斯早期裂开的大陆边缘裂谷盆地。早期裂谷中心部位不是现在大陆缝合线的雅鲁藏布一带,而在低分水岭带。晚侏罗世到早白垩世,雅鲁藏布江南测为典型被动大陆边缘,其沉积盆地沉降、海平面变化与沉积作用相吻合。晚白垩世到第三纪为前陆盆地演化阶段,从沉积作用可以识别出晚白垩世晚期为造山第一暮,第三纪初为第二幕。
- 喜马拉雅特提斯 /
- 沉积演化 /
- 被动大陆边缘 /
- 前陆盆地
Abstract: There are similar sedimentary characteristics in the areas from the northern slope of the Himalayas to Lhasa and to Xainza in the Palaeozoic. The Carboniferous-Permian distinctive Gondwana glaciomarine sediments and cold-water faunas indicate that the study area was still then a part of the Indian plate.
- Himalayan Tethys /
- sedimentary evolution /
- passive continental margin /
- foreland basin