Deepwater fold and thrust belts (DWFTBs) are classified into near-field stress-driven Type 1
systems confined to the sedimentary section, and Type 2 systems deformed by either far …

Paleomagnetic data have long been used to hypothesize that the Cenozoic extrusion of the
Indochina Block along the left-lateral Ailao Shan-Red River fault, as a result of the India-Asia …

Abstract The Indo-Burman mountain ranges mark the boundary between the Indian and
Eurasian plates, north of the Sumatra–Andaman subduction zone. Whether subduction still …

A network of 27 GPS sites was implemented in Iran and northern Oman to measure
displacements in this part of the Alpine–Himalayan mountain belt. We present and interpret …

We derive a detailed horizontal velocity field for the southeast borderland of the Tibetan
Plateau using GPS data collected from the Crustal Motion Observation Network of China …

The Andaman Sea is an active backarc basin lying above and behind the Sunda subduction
zone where convergence between the overriding Southeast Asian plate and the subducting …

Key in understanding the geodynamics governing subduction and orogeny is reconstructing
the paleogeography of 'Greater India', the Indian plate lithosphere that subducted since …

在系统总结前人成果资料基础上, 结合最新的遥感解译与地表调查资料发现,
青藏高原东南缘地壳最新的顺时针旋转运动主要受控于由川滇外弧带和滇西内弧带构成的双弧 …

A unique GPS velocity field that spans the entire Southeast Asia region is presented. It is
based on 10 years (1994–2004) of GPS data at more than 100 sites in Indonesia, Malaysia …

This paper describes geomorphologic evidence for the principal neotectonic features of
Myanmar and its immediate surroundings. We combine this evidence with published …