喜马拉雅阶段
- 网络Himalayan stage
喜马拉雅阶段-
地质分析和剖面复原结果表明，盐推覆构造主要形成于新近纪末期以来的喜马拉雅晚期阶段，现今仍具有强烈的活动性。
According to the geological analysis and cross-section restoration , the salt nappes were mainly formed in the late Himalayan stage since the end of Neogene and are still active intensively at present .
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以雅鲁藏布江带为主洋盆带的特提斯洋，从三叠纪晚期开始消减，经历了印支、燕山、喜马拉雅3个阶段脉动式板块汇聚造山过程。
The Tethyan Ocean with the Yarlung Zangbo belt as the main ocean basin belt began to be sub-ducted in the Late Triassic and experienced a process of pulsatory plate convergence orogeny including the Indosinian , Yanshanian and Himalayan stages .