The final collision of the CAOB: Constraint from the zircon U–Pb

The Linxi Formation occupies an extensive area in the eastern Inner Mongolia in the Central Asian Orogenic Belt (CAOB). The Linxi Formation is compose…

Thermochronological constraints on the exhumation history of the

Zircon U-Pb geochronology, Hf isotopes, and geochemistry

Final closure of the Paleo Asian Ocean basin in the early Triassic

Geochemistry and zircon U–Pb–Hf isotopic data for Permo

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Geochemistry and zircon U–Pb–Hf isotopic data for Permo

Frontiers Geochronological Constraint on the Evolution of the

Late Paleozoic Accretionary and Collisional Processes along the

Concordia diagrams of zircon U-Pb dating on the igneous rocks of

Research News----INSTITUTE OF GEOLOGY AND GEOPHYSICS, CHINESE

Backbone of The Americas - Shallow Subduction, Plateau Uplift

Concordia U–Pb diagrams (a) and (c), chondrite‐normalized REE

PDF) Evolution from Oceanic Subduction to Continental Collision: a

Zircon U–Pb and Hf isotopic study of Neoproterozoic granitic

Origin and Palaeozoic reworking of the Central Tianshan Block