As prototypes of crust-derived remelted S-type granite, Himalayan leucogranites have
considerable relevance in crustal evolution and associated metallogeny. However, given …

For quartz-rich tectonites two types of deformation thermometer are currently commonly
employed: 1) The quartz c-axis fabric opening-angle thermometer that provides an estimate …

The Himalayan-Tibetan orogen culminated during the Cenozoic India--Asia collision, but its
geological framework and initial growth were fundamentally the result of multiple, previous …

A range of ages have been proposed for the timing of India‐Asia collision; the range to some
extent reflects different definitions of collision and methods used to date it. In this paper we …

The Himalayan leucogranites are critical for understanding the geodynamic process of
Himalayan orogenesis. In this article, we present petrological, geochronological and …

The Xiaru dome is located in the middle section of the North Himalayan Gneiss Domes belt
in southern Tibet. The leucogranite, which crops out in the core of the Xiaru dome, is a …

The presence of hot, weak crust is a central component of recent hypotheses that seek to
explain the evolution of continent-continent collisions, and in particular may play an …

Out-of-sequence deformation in the Himalaya has been caused mainly by thrusting. Out-of-
sequence thrusts, usually north-to NE-dipping foreshear planes, occur inside the Sub …

自从印度-欧亚大陆碰撞以来, 伴随着构造演化和温度-压力-成分(PTX) 的变化,
喜马拉雅造山带中下地壳变质岩发生不同类型的部分熔融反应, 形成性质各异的过铝质花岗岩 …

Himalayan leucogranites provide some of the best examples in the world of highly felsic and
strongly peraluminous granites, and they have been paid special attention with regard to …