Although the axial and dominant geocentric character of the Earth's magnetic field means
that paleolongitude is indeterminate, paleomagnetism is otherwise the only truly quantitative …

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 Sanjiang region in SE Tibet Plateau and NW Yunnan is known to have formed by
amalgamation of Gondwana-derived continental blocks and arc terranes as a result of …

The Qinghai-Tibet Plateau, composed of several continental slivers within the eastern
Tethyan domain, is one of the pivotal sites to examine to better understand the theory of …

Sundaland, the continental core of SE Asia, is a heterogeneous collage of continental blocks
and volcanic arcs bounded by narrow suture zones that represent the remnants of ancient …

An early Paleozoic ophiolitic mélange has recently been documented in the west Gangma
Co area, north-central Tibetan Plateau. It is composed of serpentinite, isotropic and …

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

High-pressure (HP)/low-temperature (LT) metamorphic rocks, such as eclogite and
blueschist, are generally regarded as an indicator of subduction-zone metamorphism …

Ophiolite plays a key role in identifying paleo-ocean and paleo-plate and rebuilding the
evolutionary history of ancient orogen. Mafic–ultramafic rocks are distributed in a broadly E …

A∼ 500km-long high-pressure metamorphic belt occurs in the Qiangtang Block of northern
Tibet. The occurrence of high-pressure metamorphic rocks (eclogite and blueschist) has a …