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 …

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

Reduction–oxidation (redox) reactions occur during burial because sediments contain
reactive mixtures of oxidised and reduced components. Diagenetic chemical reactions …

Knowing the original size of Greater India is a fundamental parameter to quantify the amount
of continental lithosphere that was subducted to help form the Tibetan Plateau and to …

The timing, kinematics, and geodynamic evolution of the India-Asia continental collision are
crucial to understanding the geological and geomorphological evolution of the Himalayan …

Pelagic carbonates are deposited far from continents, usually at water depths of 3000–6000
m, at rates below 10 cm/kyr, and are a globally important sediment type. Recent advances …

Chemical remagnetization is a very common phenomenon in sedimentary rocks and
developing a greater understanding of the mechanisms has several benefits. Acquisition of …

Greater India comprises a part of the Indian plate that subducted under Asia to help form the
Tibetan Plateau. Defining the size of the Greater India is thus a key constraint to model the …

The timing and location India–Asia collision is crucial to understanding the evolution of the
Himalayan–Tibetan orogen and global climate change; however, estimates of the timing of …

The characteristic remanent magnetization (ChRM) isolated from Paleogene carbonate
rocks of the Zongpu Formation in Gamba (28.3° N, 88.5° E) of southern Tibet has previously …