Oceanic basalts reflect the heterogeneities in the earth's mantle, which can be explained by
five mantle end members. The HIMU end member, characterized by high time-integrated μ …

Abstract The (∼ 550–530 Ma) alkaline magmatic suite of the Amram Massif, southern Israel,
was emplaced during the transition from an orogenic to an intra-plate tectonic setting in the …

Potassic volcanism in the western Sichuan and Yunnan Provinces, SE Tibet, forms part of an
extensive magmatic province in the eastern Indo-Asian collision zone during the Paleogene …

Two Late Neoproterozoic post-collisional igneous suites, calc-alkaline (CA) and alkaline–
peralkaline (Alk), widely occur in the northernmost part of the Arabian–Nubian Shield. In …

Mantle melting, which leads to the formation of oceanic and continental crust, together with
crust recycling through plate tectonics, are the primary processes that drive the chemical …

The generation of magmas in the East African Rift System (EARS) is largely the result of
either:(A) melting of easily fusible compositions located within the lithospheric mantle due to …

Ion-probe U–Pb dating of plutonic rocks from the northern Arabian–Nubian Shield in Sinai
and southern Israel constrains the timing of late East African batholithic post-collisional calc …

The early Cretaceous volcanism occurring along the Sulu orogenic belt, east Shandong
Province, demonstrates a bimodal characteristic. The volcanic rocks belong to high-K …

Common geological, geochemical, and geophysical characteristics of continental fragments
of East Gondwana and adjacent oceanic lithosphere define a long‐lived, low‐volume …

The nature of Mesozoic subcontinental lithospheric mantle (SCLM) has been rarely iscussed
in detail even though it might be crucial to understanding of the lithospheric thinning process …