The Cretaceous tectonic evolution of South China is characterized by widespread
extensional basin and dome generation, voluminous magma intrusion/eruption and …

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 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 …

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 …

Porphyry copper deposits account for more than 80% of the world's total Cu resources.
However, the formation mechanism and controlling factors of porphyry copper deposits …

Mesozoic mineral deposits in South China include world-class deposits of W, Sn and Sb and
those that provide the major sources of Ta, Cu, Hg, As, Tl, Pb, Zn, Au and Ag for the entire …

Long-term couplings between the subducting and overlying plates are very important to
understanding plate tectonics, in particular intraplate evolutions. Geological records of this …

The Middle–Lower Yangtze River Valley metallogenic belt (YRB), situated along the
northern margin of the Yangtze craton, is characterized by porphyry–skarn–stratabound Cu …

The Furong deposit, located in southern Hunan Province, China, is a newly-discovered giant
tin deposit spatially associated with the A-type Qitianling granite. The petrogenetic link …

The East Qinling–Dabie orogenic belt accommodates the largest Mo ore district in the world.
It contains 8.43 Mt of proven Mo metal reserves which accounts for 66% of the total proven …