This paper reviews the spatial-temporal distribution, geological and geochemical features,
and geophysical context of diverse types of Cenozoic ore deposits formed during India …

Different hypotheses have been proposed for the origin and pre-Cenozoic evolution of the
Tibetan Plateau as a result of several collision events between a series of Gondwana …

The surface uplift history of the Tibetan Plateau (TP) offers a key testing ground for
evaluating models of collisional tectonics and holds important implications for processes …

Long-standing problems in the geological evolution of the Tibetan–Himalayan orogen
include where the India–Asia convergence was accommodated and how the plateau grew …

The surface uplift of mountain belts is in large part controlled by the effects of crustal
thickening and mantle dynamic processes (eg, lithospheric delamination or slab breakoff) …

Abstract Porphyry Cu deposits in China contain a total resource of~ 47 million tonnes (Mt)
Cu at average grades ranging mostly from 0.2 to 0.7% Cu (most< 0.5% Cu), accounting for …

The time of initial collision between India and Asia has been extremely controversial despite
the fact that it is vital to constraining the orogenesis and subsequent evolution of the …

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 …

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 Lhasa terrane in southern Tibet is composed of Precambrian crystalline basement,
Paleozoic to Mesozoic sedimentary strata and Paleozoic to Cenozoic magmatic rocks. This …