The history of the South China Craton and the constituent Yangtze and Cathaysia blocks are
directly linked to Earth's Phanerozoic and Precambrian record of supercontinent assembly …

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

From the formation of Rodinia at the end of the Mesoproterozoic to the commencement of
Pangea breakup at the end of the Paleozoic, the South China craton first formed and then …

Variations in continental volcanic arc emissions have the potential to control atmospheric
carbon dioxide (CO2) levels and climate change on multimillion-year time scales. Here we …

Detrital zircon data have recently become available from many different portions of the
Tibetan–Himalayan orogen. This study uses 13,441 new or existing U‐Pb ages of zircon …

This review paper presents a set of revised global palaeogeographic maps for the 825–540
Ma interval using the latest palaeomagnetic data, along with lithological information for …

The U-Pb age and Hf isotope data on detrital zircons from Paleozoic metasedimentary rocks
in the Lhasa terrane (Tibet) define a distinctive age population of ca. 1170 Ma with εHf (t) …

Zircon U‐Pb geochronological data on over 900 zircon grains for Cambrian to Silurian
sandstone samples from the South China Block constrain the pre‐Devonian tectonic setting …

Detrital zircons from samples of Palaeozoic to Mesozoic sedimentary rocks have been
collected in Malaysia, Thailand, Laos, Vietnam, Cambodia and China, dated by the LA …