Influence of Mo and Cu additions on the microstructure and mechanical performance of air-hardening ductile forging steels in the context of circular economy

Oguz Gülbay

doi:10.1016/j.msea.2026.150881

Devonian Jinshuikou pegmatites at the northern margin of the Tibetan Plateau: UPb and SmNd constraints on their genetic relationship with regional granitoids

2026-07-06

0

PRE

AI

S

Si-Qi Liu

S

Shao-Yong Jiang *

M

Mostafa Fayek

H

Hui-Min Su

Y

Yu-Ying Che

W

Wei Wang

Q

Qinglin Xia

DOI：10.1016/j.lithos.2026.108707

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• Paleozoic granitic pegmatites occurred in the Jinshuikou area of northern Tibetan Plateau. • Pegmatites and I-type granitoids are both from a crust-mantle mixed source. • Pegmatites are products from intense fractional processes at the magma source. • Pegmatitic magma was preserved in the deep crust for nearly 15 Myr.

Devonian Jinshuikou pegmatites at the northern margin of the Tibetan Plateau: UPb and SmNd constraints on their genetic relationship with regional granitoids

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