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 …

Laser-ablation ICP mass-spectroscopy has been used to investigate the geochemistry of
sphalerite in a range of nine Zn–Pb deposits in South China. The deposits, which are of …

The ore deposits of the Mesozoic age in South China can be divided into three groups, each
with different metal associations and spatial distributions and each related to major …

Abstract The South China Craton was formed by amalgamation of the Yangtze and
Cathaysia Blocks during the Neoproterozoic. During the Mesozoic, voluminous granitic …

China produces about 450 t Au per year and has government stated in-ground reserves of
approximately 12,000 t Au. Orogenic gold, or gold deposits in metamorphic rocks, and …

Abstract The Southeast Asia region is endowed with a diversity of mineral resources, notably
porphyry-related skarn, epithermal and sediment-hosted/orogenic gold deposits. Formation …

Mineral deposits associated with continental collision are abundant in many orogenic
systems. However, the metallogenesis of collisional orogens is often poorly understood, due …

The mid-Miocene Gangdese orogenic belt in southern Tibet contains porphyry Cu deposits
that developed after the Indian–Asian continental collision in the early Cenozoic. Field work …

South China hosts the most abundant and largest tungsten (W) deposits in the world, being
a famous W metallogenic region. Located at the eastern part of the South China Block …

Zircon rare earth element (REE) oxy-barometers have been widely used to calculate magma
oxygen fugacity. However, sometimes confusing results are obtained, such as extremely …