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造山带地貌是气候、构造及其相互作用等复杂过程的产物。其中，河流是造山带中发育最为广泛的地貌之一。河流侵蚀过程的控制因素随时间发生改变，但是它们是如何变化仍然不清楚。横跨青藏高原东南部、南部和喜马拉雅山的长江、湄公河、萨尔温河和雅鲁藏布江等大河水系呈现不寻常的几何形态和地貌特征，被认为是构造变形、水系重组以及气候变化的结果。因此，青藏高原和喜马拉雅山的河流是研究构造、气候、地表过程和水系重组之间复杂...
Damming of River Indus during Late Quaternary in Ladakh Region of Trans-Himalaya, NW India：Implications to Lake formation-climate and tectonics
Late Quaternary Holocene Trans Himalaya Indus Palaeolake deposits climate
2014/1/16
Indus river valley basin in Northwest Indian Himalaya is tectonically unstable, exhibiting a complex topography, landscape relief and varied Quaternary sedimentation. A 422 km transact along the Indus...
Modelling Genesis of Intracratonic Chains Related to Tectonics Inheritance: Case Study from Gafsa Basin (Southern Central Tunisia)
Tectonic inheritance Intracratonics chains Fault related fold
2009/12/3
Tectonic inheritance is a concept proved by the importance of tectonic phase’s variation during time. It is related toreactivation in compression of old normal faults. In our study we will focus on Ga...