Understanding the manner and degree to which topography in active mountain ranges
reflects deformation of the Earth's surface remains a first order goal of tectonic …

The flood distribution and bedrock incision threshold exert important influences on the
erosion efficiency, which can result into a nonlinear scaling between channel steepness …

Convergent orogens exhibit high elevations and relief, features characteristic of active rock
uplift, the latter influencing normalized channel steepness (Ksn). In systems with significant …

Cenozoic extension of the Qinling range-Weihe Graben system has occurred in response to
the uplift and growth of the Tibetan Plateau. Rapid exhumation of the northern Qinling range …

Identification of the planation surfaces (PSs) is key for utilizing them as a reference in
studying the long-term geomorphological evolution of the Upper Yangtze River Basin in the …

Mountains in the US Basin and Range Province are similar in form, yet they have different
histories of deformation and uplift. Unfortunately, chronicling fault slip with techniques like …

Understanding how fault systems interact and transfer strain over seismogenic timescales
(seconds to ka) requires temporal records of past ruptures along adjacent and intersecting …

均衡状态时的基岩河道纵剖面表现为平滑形态, 然而自然界的河道纵剖面常因地球各种内外动力
作用的影响而呈现出以裂点为特征的不均衡状态, 因此不均衡的河道剖面及裂点的特征可以用于 …

The long profile of rivers is widely considered as a recorded of tectonic uplift rate.
Knickpoints form in response to rate changes and faster rates produce steeper channel …

Understanding the degree to which topography of erosional landscapes in active mountain
belts encode the rates and patterns of active deformation in the upper crust is a primary goal …