To understand the early topographic growth of the Tibetan Plateau and the causes and
effects of climate change in this region, it is important to reconstruct the drainage evolution …

The relative roles of tectonics and climate change in global and regional desertification are
not well constrained. Previous studies have emphasized the role played by climate change …

The evolution of the Sibumasu Terrane forms a principal component in the history of the
Tethys Oceans with the northward movement of Gondwana-derived terranes creating the …

Well-described ribbon continent collision belts, and modern examples, with 2D seismic
coverage, particularly Zealandia, provide analogues for the Permo-Triassic development of …

The late Paleozoic and early Mesozoic Indosinian Orogeny in Southeast Asia was
characterized by subduction in the Paleo-Tethys and collisions among continental blocks …

Devonian–Carboniferous strata in the Hida Gaien belt, Southwest Japan, are characterized
by a change in the dominant lithology from clastic rocks and limestones to volcanic rocks …

Abstract The Tibetan Plateau and its adjacent areas are a typical example for studying the
relationship between plateau uplift, climate change, and surface erosion. It has been argued …

The terranes that form Thailand are key to understanding the palaeogeography of Greater
Gondwana, the Tethys Oceans and the development of present-day Southeast Asia. In …

Continental orogens that involve subduction and collision are important target areas for
studying the growth, stabilization and transformation of Earth's continents. In particular, the …

The Yangtze Block in South China constitutes an important Precambrian landmass in the
present East Asian continent. The Neoproterozoic sedimentary successions of the Hengdan …