The architecture and mechanics of an orogen can be understood in terms of a system of
collages that are characterized by a complex assemblage of multiple components, but the …

Abstract The Central Asian Orogenic Belt (CAOB) is the largest accretionary orogen in the
world with considerable Phanerozoic juvenile crustal growth. The eastern segment of the …

As one of the largest Phanerozoic orogens in the world, the Central Asian Orogenic Belt
(CAOB) is a natural laboratory for studies of continental dynamics and metallogenesis. This …

本文提出了" 兴蒙陆内造山带" 的新概念(Xing-Meng Intracontinent Orogenic Belt, XMIOB),
从大地构造, 沉积建造, 岩浆作用和变质作用等方面论述了XMIOB 从晚古生代到中生代初的陆内 …

增生型造山带记录复杂的板块汇聚过程, 增生造山作用演化历史漫长, 发育多期次造山作用.
就增生型造山带的特征与复杂性进行简要总结与评述, 并讨论增生造山作用时空分析思路 …

The interplay between continental motions during the assembly of Pangaea and late
Palaeozoic climate change, including severe glaciation and global aridification, remains …

The key to defining the termination of accretion in an accretionary orogen is to recognize the
initial magmatic processes that are generated at the time of ocean closure. We present new …

Initiation of new subduction zones is an integral part of Earth's plate tectonics regime. It is
generally accepted that the negative buoyancy of sufficiently old oceanic lithosphere …

Abstract The Central Asian Orogenic Belt (CAOB) was generated through multiple collisional
and accretionary events in the Paleo-Asian Ocean, a major global ocean that existed from …

A major current debate in Asian tectonics concerns the time of closure of the Paleo‐Asian
Ocean (PAO) and the collision between the Central Asian arcs and the Tarim and North …