The Acoje block of the Zambales ophiolite in the Northwest Philippines is a remnant of forearc lithosphere that formed during an Eocene subduction ini......
The lithospheric root underneath the Dabie orogen, which is the key part of the Central Orogen of China, experienced a cycle of thickening during Tria......
The Madurai Block is the largest crustal block in the Southern Granulite Terrane of India, and is composed of a dominantly Neoarchean northern segment......
Permian Erbutu and Kebu Ni-Cu sulfide-bearing mafic-ultramafic intrusions in the central Asian orogenic belt (CAOB) formed in the Andean- style contin......
Compared with the statement of the mantle plume hypothesis for large-scale plus high-volume intraplate magmatism, a series of OIB-like mafic rocks whi......
The Late Jurassic tectonic environment of western part of northern margin of the North China Craton (NNCC) remains poorly understood due to weak magma......
Volcanic arcs usually produce silica-rich magmas that may modify the peridotitic sub-arc mantle, but direct observations on the lithology and geochemi......
While ultrapotassic rocks are generally considered to be derived from a metasomatized mantle source, whether their characteristically high delta O-18 ......
The Singhbhum Craton in eastern India preserves the records of Paleoarchean - Mesoarchean oceanic crust dominated by ultramafic-mafic extrusive rocks ......
Late Paleozoic granitoid rocks hold critical information regarding continental crustal growth and evolution of the Dunhuang Block at the southernmost ......
Understanding the storage and evolution of magma in the Earth's crust is of great significance for the study of igneous rocks. In recent years, the lo......
The Gangdese magmatic belt of southern Tibet preserves important records of the Mesozoic Neo-Tethyan orogeny. Here we investigate a newly identified L......
Magmatic sulfide saturation and dissolution are increasingly thought to play important roles in controlling the behavior of chalcophile metals in arc-......
The tectonothermal evolution of the interior of the vast Central Asian Orogenic Belt (CAOB) is poorly understood. In this study, detailed structural o......
The interaction between ascending carbonic fluids and rocks at shallow depths in orogenic systems plays a crucial role in carbon distribution and flux......
