The spatial-temporal distribution of the Triassic post-collision-related and arc-related plutons in the Korean Peninsula is key to unraveling the posi......
The formation of Meso-Neoarchean metagranitoids from the Wuhe complex (WC), southeastern margin of the North China Craton (NCC) and the nature of Meso......
Crust-mantle interaction is essential to the evolution of continental crust, but its type and mechanism remain controversial in continental collision ......
The petrogenesis of silicic igneous rocks is a key aspect in the formation of the continental crust. Whether magma fractional crystallization is a mai......
The Central subprovince of the Borborema Province (NE Brazil) is characterized by a voluminous and diversified late-Neoproterozoic magmatism (ca. 640 ......
Essential mechanisms for the geochemical diversity observed in a silicic igneous rock association, which is of paramount importance for understanding ......
Most Cretaceous igneous rocks in the northeastern North China Cratons (NCC) and southeastern South China Cratons (SCC) in Northeast Asia are interpret......
A suite of lavas from northwest Mull, British Palaeocene Igneous Province, exhibit major and trace element characteristics that are best explained by ......
Ridge subduction is an inevitable process during the evolution history of a vanished ocean. Due to its special characteristics, such as buoyant densit......
The Luobusa ophiolite in the southeastern Tibet holds the largest chromitite resource in China. These rocks present an ideal opportunity to study the ......
Cenozoic post-collisional potassic igneous suites with compositions varying from mafic to felsic members are widespread in western Yunnan, China, but ......
The eastern Blacksea magmatic arc (EBMA) in the eastern Sakarya Zone (ESZ) provides an excellent opportunity to investigate birth of an extensional in......
The Neo-Tethys oceanic slab rollback and ridge subduction are two competing geodynamic processes responsible for the early stage of late Cretaceous ma......
Differentiation processes governing the transformation of the mantle-derived primitive arc melts into more evolved, intermediate to felsic composition......
A suite of kimberlite-hosted mantle xenoliths from the Catalao region, southwestern margin of the Sao Francisco Craton (SFC), Brazil, consists of spin......
