Granite is one of the most important components of the continental crust on our Earth; it thus
has been an enduring studied subject in geology. According to present knowledge, granite …

Regolith-hosted rare earth element (REE) deposits, also called ion-adsorption or weathered
crust elution-deposited REE deposits are distributed over Jiangxi, Guangdong, Fujian …

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 Phanerozoic tectonic regimes of the South China Block (SCB) hold a key to
understanding of its geodynamic evolution with respect to formation of numerous mineral …

Tungsten and Sn deposits in China are widely distributed in the South China block (ie,
Yangtze craton-Cathaysian block), Himalaya, Tibetan, Sanjiang, Kunlun, Qilian, Qinling …

The Asian continent consists of many continental blocks that assembled during the
Phanerozoic, accompanied by widespread granitoids. By compiling a series of digital maps …

Abstract The early Paleozoic Wuyi-Yunkai orogen in South China is a major orogenic belt in
East Asia that formed at a similar time as the classic Caledonian orogeny in Europe. Despite …

The basic tectonic framework of continental East Asia was produced by a series of nearly
contemporaneous orogenic events in the late Middle Jurassic to Early Cretaceous …

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 …

As a major component of continental crust, granites have been served as the most important
subject in geology. Based on advancements obtained during past decades, this paper …