Abstract The Phanerozoic record of Southeast Asia preserves the history of opening and
subsequent consumption of the Paleotethyan Ocean and the assembly of continental …

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 …

昌宁-孟连特提斯洋的构造演化及其原特提斯与古特提斯的转换方式一直是青藏高原及邻区基础
地质研究中最热门的科学问题之一. 根据新的地质调查资料, 研究成果并结合分析数据 …

青藏高原古特提斯体系的特征表现为古特提斯洋盆中多条状地体的存在, 多俯冲,
多岛弧增生体系的形成和多地体汇聚, 碰撞造山的动力学环境, 其构架包括4 …

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 …

Abstract The Bangong–Nujiang suture zone (BNSZ) is located in the central Tibetan
Plateau, and represents the relict of the Bangong–Nujiang Tethyan Ocean (BNTO). This …

The elevation of the Tibetan plateau is a revolutionary event in the Earth history, which
resulted in change not only of Cenozoic regional and global climate but also of monsoon …

The Qiangtang metamorphic belt (QMB) in central Tibet is one of the largest and most
recently documented high-pressure (HP) to near-ultrahigh-pressure (near-UHP) belts on …

Abstract The Paleozoic-early Mesozoic geology of Tibet was controlled by the rift-drift,
seafloor spreading and subduction zone tectonics of a Paleo-Tethyan realm, which evolved …