Abstract The Cenozoic Himalaya-Tibet orogen is generally regarded as the archetypal
continental collision zone and is often used as an analogue for interpreting ancient orogenic …

In this study, we integrate bedrock datasets, observations of subducted slabs in the mantle,
and plate kinematic constraints to constrain models for the India-Asia collision and the …

Abstract The Izu–Bonin–Mariana (IBM) forearc contains a record of a widespread and short-
lived subduction initiation event in the early Eocene. We present new high-precision ages to …

We report paleomagnetic data showing that an intraoceanic Trans-Tethyan subduction zone
existed south of the Eurasian continent and north of the Indian subcontinent until at least …

位于青藏高原南部的冈底斯岩浆弧是新特提斯大洋岩石圈长期俯冲导致的中生代岩浆作用的
产物, 而且在印度与亚洲大陆碰撞过程中叠加了强烈的新生代岩浆作用, 是世界上典型的复合型 …

The enigmatic geodynamic processes involved in the India-Asia collision shape our
understanding of uplift and deformation of the Tibetan Plateau and the subsequent changes …

Zircon rare earth element (REE) oxy-barometers have been widely used to calculate magma
oxygen fugacity. However, sometimes confusing results are obtained, such as extremely …

The timing of the India‐Asia collision onset, essential to understanding the evolution of the
Himalayan‐Tibetan orogen, has been widely investigated through multidisciplinary …

Abstract The Bengal Basin is a collisional foreland basin in South Asia located at the
juncture of the Eurasian, Indian and Burmese Plates occupying Bangladesh and parts of the …

Magmatic arcs are thought to be the primary sites of modern-day continental crustal growth,
and arc crustal sections provide an exceptional opportunity to directly observe the …