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 …

Chemical geodynamics is an integrated discipline that studies the geochemical structure
and tectonic evolution of geospheres with the aim of linking tectonic processes to …

内容提要: 印度亚洲碰撞是新生代地球上最为壮观的重大地质事件. 碰撞及碰撞以来,
青藏高原的广大地域发生了与碰撞前截然不同的变形, 地貌, 环境及其深部结构都发生了深刻地 …

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 …

摘要塔里木盆地为环形山链所环绕, 北缘为古亚洲体系的天山弧形山链, 南缘为特提斯体系的西
昆仑-阿尔金弧形山链. 自新元古代晚期以来, 塔里木地块及周缘地区经历了古亚洲洋盆和特提斯 …

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

The initial collision between Indian and Asian continents marked the starting point for
transformation of land-sea thermal contrast, uplift of the Tibet-Himalaya orogen, and climate …

Zircon geochronology and geochemistry are increasingly important for understanding
metamorphic processes, particularly at extreme conditions, but drivers of zircon dissolution …

The Himalayan orogeny, a result of the collision of India and Eurasia, provides direct
evidence of strain accommodation and large-scale rheological behavior of the continental …

In general, Archean rocks exhibit rather ordinary moderate-P-high-T facies series
metamorphism; neither blueschists nor any record of deep continental subduction and return …