The timing of initial collision between India and Asia has remained controversial for half a
century. This paper attempts to review this crucial and hotly debated argument, describing …

A review of the geologic history of the Himalayan-Tibetan orogen suggests that at least 1400
km of north-south shortening has been absorbed by the orogen since the onset of the Indo …

摘要喜马拉雅2 青藏高原造山带的地质历史显示出, 自从约70Ma 印度板块2
亚洲板块开始碰撞以来, 至少有1 360 km 的SN 向缩短量被喜马拉雅2 青藏高原造山带所吸收 …

提要: 运用地体和地体活动论观点, 提出青藏高原结构划分的新方案; 强调青藏高原的形成经历了
新元古代以来长期活动的过程, 青藏高原是一个“非原地” 诸多地体会聚, 拼合以及经历复合碰撞 …

Siliciclastic sedimentary rocks derived from the southern Lhasa terrane, sitting depositionally
upon rocks of the northern Indian passive continental margin, provide an estimate of the age …

The Red River Fault zone (RRF) is the major geological discontinuity that separates South
China from Indochina. Today it corresponds to a great right-lateral fault, following for over …

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 …

During the Mesozoic–Cenozoic, northward Neotethyan subduction and subsequent India–
Asia collision gave rise to the extensive Transhimalayan magmatism that stretches from …

Continental flood basalt eruptions have resulted in sudden and massive accumulations of
basaltic lavas in excess of any contemporary volcanic processes. The largest flood basalt …

Comparing the timing of mass extinctions with the formation age of large igneous provinces
reveals a close correspondence in five cases, but previous claims that all such provinces …