Abstract The Tianshan and Junggar orogenic collage occupies the southwestern part of the
Central Asian Orogenic Belt and was assembled by collision/accretion of several continental …

We present a review of major gold mineralization events in China and a summary of
metallogenic provinces, deposit types, metallogenic epochs and tectonic settings. Over 200 …

西天山位于中亚造山带的西南缘, 经历了复杂的增生造山过程. 它也是标志塔里木地块北部被动
陆缘与西伯利亚地块南侧宽阔活动陆缘最后拼合的构造带. 根据近年来的研究进展 …

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 …

Biodiversity is unevenly distributed on Earth and hotspots of biodiversity are often
associated with areas that have undergone orogenic activity during recent geological history …

Continental China is a mosaic of numerous tectonic blocks, which amalgamated from
Neoarchean to Cenozoic broadly coeval with the cycles of global supercontinents such as …

The Tian Shan of Central Asia is located in the southwestern part of the Central Asian
Orogenic Belt (CAOB, also known as the Central Asian Orogenic System or CAOS) …

Abstract The Chinese Tianshan belt is a major part of the southern Central Asian Orogenic
Belt, extending westward to Kyrgyzstan and Kazakhstan. Its Paleozoic tectonic evolution …

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 …

Geochemical and geochronological evidence was obtained from granitoids of the South
Tianshan orogen and adjacent regions, which consist of three individual tectonic domains …