Abstract：The bigger river belongs to the deep-great fault belt, the deepgreat fault belts were crossed across the branching faults since the newtectonic, the faulted blocks were cut along the deep-great belt river, the gorge formed in the uplifted blocks, the broad valley floor formed in the settling blocks. All the continuing terrace will not be evolved after paternoster valley. For example, there are no continuing terraces in Yarlung Zangbo River, in An Lin River, et al. The River defleotion was controlled by the fault directive.
收稿日期: 1987-04-25
引用本文:
周中民. 雅鲁藏布中游断裂河谷地貌特征的探讨[J]. , 1987, 26(4): 0-0.
周中民. A DISCUSSION ON THE MIDDLE YARLUNG ZANGBO RIVER PATERNOSTER CHARACTERISTICS. , 1987, 26(4): 0-0.
