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 …

The Asian continent formed during the past 800 my during late Neoproterozoic through
Jurassic closure of the Tethyan ocean basins, followed by late Mesozoic circum-Pacific and …

Epigenetic gold deposits in metamorphic terranes include those of the Precambrian shields
(approx 23,000-25,000 t Au), particularly the Late Archean greenstone belts and …

Metamorphic belts are complex regions where accretion or collision has added to, or
thickened, continental crust. Gold-rich deposits can be formed at all stages of orogen …

The Altaids are an orogenic collage of Neoproterozoic–Paleozoic rocks located in the center
of Eurasia. This collage consists of only three oroclinally bent Neoproterozoic–Early …

Reduced intrusion-related gold systems (RIRGS) are characterized by widespread arrays of
sheeted auriferous quartz veins that preferentially form in the brittle carapace at the top of …

中亚成矿域地质演化的重要特征是: 古生代地壳生长和演化的多阶段性, 多旋回物质的活化-
再活化, 成矿环境的长期性和周期性, 这些特征导致域内成矿物质的多次迁移和聚集 …

Phanerozoic intrusion-related gold deposits have many consistent characteristics such as a
spatial, temporal, and geochemical association with moderately reduced (predominantly …

Abstract The Central Asian supercollage consists of the Baikalides, Timanides, Altaids, and
Mongolides. They are located between the Eastern European, Siberian, Karakum, Tarim …

The Sawayaerdun gold deposit is hosted by Carbonaceous metasediments and is
considered to be the largest Muruntau-type gold deposit in the Chinese Tianshan …