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 …

Determining the absolute duration of magmatic-hydrothermal events leading to the formation
of porphyry systems (ie, including porphyry copper, skarn, and epithermal deposits) is one of …

Many workers accept a metamorphic model for orogenic gold ore formation, where a gold-
bearing aqueous-carbonic fluid is an inherent product of devolatilization across the …

Understanding the source of metamorphic sulfur is critical to clarifying the complete cycle of
ore genesis, from source to sink, for several mineral deposit types. In this study, a mass …

The Hercynian Tien Shan (Tianshan) orogen formed during Late Palaeozoic collision
between the Karakum–Tarim and the Kazakhstan paleo-continents. In order to constrain …

We re-evaluate the cycling of molybdenum (Mo) and rhenium (Re) in the near-surface
environment. World river average Mo and Re concentrations, initially based on a handful of …

Abstract Major porphyry Cu–Au and Cu–Mo deposits are distributed across almost 5000 km
across central Eurasia, from the Urals Mountains in Russia in the west, to Inner Mongolia in …

天山西段, 从乌兹别克斯坦向东, 经吉尔吉斯斯坦到中国新疆西部, 在中天山及南北缘巨型和世界
级金矿集中产出, 构成世人瞩目的巨型金成矿带, 即“亚洲金腰带”. 为什么能在这个东西延伸近 …

Mineral assemblages formed during hydrothermal alteration reflect the geochemical
composition of ore-forming fluids. Gold is mainly transported in solution as Au–Cl and Au–S …

Multimethod chronology was applied on intrusives bordering the Kyrgyz South Tien Shan
suture (STSs) to decipher the timing of (1) formation and amalgamation of the suturing units …