Abstract The East Asian continent records a complex geologic and tectonic history that
involved the amalgamation of several small-to medium-sized blocks from Laurasia or …

The Asian monsoons are triggered by complex interactions between the atmosphere, Asian
and African orography, and the surrounding oceans, resulting in highly seasonal climate …

Convergence between the Indian and Asian plates has reshaped large parts of Asia,
changing regional climate and biodiversity, yet geodynamic models fundamentally diverge …

Based on the marine magnetic anomalies identified in the Argo Abyssal Plain offshore
northwestern Australia, the conceptual continent of Argoland must have rifted off in the Late …

Indian continental subduction can explain Cenozoic crustal deformation, magmatic activity
and uplift of the Tibetan Plateau following the India-Asia collision. In the western Himalayan …

Abstract The Cenozoic India-Eurasia collision has had profound impacts on sha** the
Tibetan plateau, but its early history remains controversial due to uneven availability of …

Abstract The Indo-Burma Ranges form an enigmatic mountain belt, with fragments of
evidence for an early accretionary history (Jurassic Jade belt HP-LT metamorphism; Early …

Understanding the tectonics that gave rise to the formation of Tibet is critical to our
understanding of crustal deformation processes. The unusual geomorphology of the …

Abstract The Burma Terrane is a microplate at the eastern edge of the Tibetan-Himalayan
orogen, the origin of which remains poorly understood. Its basement comprises …

Recent, high quality palaeomagnetic data from the West Burma Terrane (WBT) indicates
rapid northwards translation (> 2000 km) of the terrane, at about the velocity of the Indian …