scispace - formally typeset
C

Changgui Gao

Researcher at China University of Geosciences (Wuhan)

Publications -  13
Citations -  7467

Changgui Gao is an academic researcher from China University of Geosciences (Wuhan). The author has contributed to research in topics: Zircon & Eclogite. The author has an hindex of 11, co-authored 13 publications receiving 5909 citations.

Papers
More filters
Journal ArticleDOI

In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard

TL;DR: In this paper, an internal standard-independent calibration strategy for LA-ICP-MS analysis of anhydrous minerals and glasses was described, where the ablation yield correction factor (AYCF) was used to correct the matrix-dependent absolute amount of materials ablated during each run.
Journal ArticleDOI

Continental and Oceanic Crust Recycling-induced Melt^Peridotite Interactions in the Trans-North China Orogen: U^Pb Dating, Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths

TL;DR: In this article, the first finding of continental crust-derived Precambrian zircons in garnet/spinel pyroxenite veins within mantle xenoliths carried by the Neogene Hannuoba basalt in the central zone of the North China Craton (NCC).
Journal ArticleDOI

Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS

TL;DR: In this paper, a protocol was established for simultaneous measurements of zircon U-Pb ages and trace elements by LA-ICP-MS at spot sizes of 16-32?m.
Journal ArticleDOI

In situ U-Pb dating and trace element analysis of zircons in thin sections of eclogite: Refining constraints on the ultra high-pressure metamorphism of the Sulu terrane, China

TL;DR: In this article, two types of zircon grains have been identified in thin sections of a retrograde eclogite from the main hole of the Chinese Continental Scientific Drill project in the Sulu UHP terrane.
Journal ArticleDOI

Melting-induced fluid flow during exhumation of gneisses of the Sulu ultrahigh-pressure terrane

TL;DR: In this paper, a deformed quartz vein is located at the boundary between the host gneiss and the eclogite lens, and a pool of weighted average 206 Pb/ 238 U analyses reveal an age of 219±-3 ǫ (2σ).