The large Gangdese metallogenic belt, located in the southern part of the Tibetan Plateau,
hosts a variety of magmatic-hydrothermal ore deposits. Previous works in the area primarily …

The Kunyang phosphate deposit, located on the southwestern margin of the Yangtze Block
in southern China, is hosted by the Lower Cambrian Meishucun Formation. The distribution …

The tectonic and topographic evolution of the southeastern Tibetan Plateau based on low‐
temperature thermochronology data is controversial, especially whether it is tectonically‐or …

The growth and expansion of the southeastern Tibetan Plateau remain contentious.
Positioned as one of the regions characterized by the most robust tectonic activities on the …

Apart from northern and Central China, the fossil record of the latest Miocene and early
Pliocene of Asia are not well documented and the record of South China during this interval …

The timing and mechanism of uplift in the southeastern Tibet Plateau have long been
subjects of debate. The Gongga Shan region, positioned at the convergence of the Songpan …

Abstract The Karakoram Fault Zone displays distinctive topographic and tectonic
characteristics, with intricate river drainage systems. Although there are extensive …

The occurrence of a sharp turn along the upper course of the Yangtze River is referred to as
the “Great Bend” and represents a large-scale drainage reorganization in response to the …

Abstract The Shuiluo River Catchment (SRC) is the front zone of the southeast compression
and uplift of the Tibetan Plateau, with intense tectonic activity. In the basin, a series of …

Abstract The Qilian Shan is situated along the northeastern margin of the Tibetan Plateau,
and has undergone multiple episodes of tectonic deformation since the Paleozoic. Strikingly …