Silicic magmas play an important role in the formation of continental crust and are
responsible for some of the most hazardous volcanic eruptions on the planet. Low-δ 18 O …

Only some carbonatite–syenite complexes in the world could form carbonatite-related rare
earth element (REE) deposits, which is regarded as the main REE origin. The Miocene …

The mechanisms and processes by which subducted slab interacted with mantle plume
remain controversial, as direct observation of such interaction is difficult to impossible …

Abstract Gebel Abu Dabbab, which is located at 50 km NW of Marsa Alam city, represents an
unique and specialized stock-like felsic intrusion of rare metals and Sn bearing albite …

Neoproterozoic magmatic rocks and detrital zircons with low‐δ18O values were frequently
identified in the Yangtze Block, Madagascar, and India. Here we first report Neoproterozoic …

A 2.61 Ga intraplate magmatism took place locally within the Kursk Domain of the Eastern
Sarmatia forming a volcanic-plutonic association of rhyolites and granites. The zircon Lu-Hf …

Magma mixing commonly takes place between isotopically depleted mafic and enriched
felsic magmas. Here we present isotopic evidence exhibiting the opposite behavior in the …

Water is essential to the formation of intracontinental granites, but its origin remains elusive.
Here we address this scientific problem by analyzing D/H isotopes of apatites, hydrous …

Oceanic arc subduction systems are the loci of substantial recycling of oceanic crust and
production of juvenile arc crust that differentiates to more evolved felsic crust. Inevitably …

The Maoniuping giant rare earth element deposit is genetically related to a Cenozoic
alkaline syenite–carbonatite complex. However, the origin of the alkaline complex and the …