Yi‐Gang Xu

ORCID: 0000-0002-9531-7208
Publications
Citations
Views
---
Saved
---
About
Contact & Profiles
Research Areas
  • Geological and Geochemical Analysis
  • earthquake and tectonic studies
  • High-pressure geophysics and materials
  • Geochemistry and Geologic Mapping
  • Geological and Geophysical Studies
  • Geochemistry and Elemental Analysis
  • Geology and Paleoclimatology Research
  • Paleontology and Stratigraphy of Fossils
  • Geochemistry and Geochronology of Asian Mineral Deposits
  • Hydrocarbon exploration and reservoir analysis
  • Astro and Planetary Science
  • Planetary Science and Exploration
  • Methane Hydrates and Related Phenomena
  • Geological Studies and Exploration
  • Isotope Analysis in Ecology
  • Space Science and Extraterrestrial Life
  • Geological formations and processes
  • Groundwater and Isotope Geochemistry
  • Radioactive element chemistry and processing
  • Seismic Imaging and Inversion Techniques
  • Geomagnetism and Paleomagnetism Studies
  • Seismology and Earthquake Studies
  • Geoscience and Mining Technology
  • Plant Ecology and Soil Science
  • Space Exploration and Technology

Guangzhou Institute of Geochemistry
2016-2025

Chinese Academy of Sciences
2016-2025

University of Chinese Academy of Sciences
2019-2025

First Affiliated Hospital of Dalian Medical University
2025

Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)
2021-2024

Hubei University of Automotive Technology
2024

Chinese Academy of Medical Sciences & Peking Union Medical College
2024

East China University of Technology
2024

Université Paris Cité
1996-2022

Royal Holloway University of London
1996-2018

10.1016/s1464-1895(01)00124-7 article EN Physics and Chemistry of the Earth Part A Solid Earth and Geodesy 2001-01-01

The North China Craton (NCC) was originally formed by the amalgamation of eastern and western blocks along an orogenic belt at ∼1.9 Ga. After cratonization, NCC essentially stable until Mesozoic, when intense felsic magmatism related mineralization, deformation, pull-apart basins, exhumation deep crust widely occurred, indicative destruction or decratonization. Accompanying this significant removal cratonic keel lithospheric transformation, whereby thick (∼200 km) refractory Archean...

10.1146/annurev-earth-053018-060342 article EN Annual Review of Earth and Planetary Sciences 2018-12-14

Research Article| October 01, 2004 Geologic, geochemical, and geophysical consequences of plume involvement in the Emeishan flood-basalt province Yi-Gang Xu; Xu 1Guangzhou Institute Geochemistry, Chinese Academy Sciences, 510640 Guangzhou, China Search for other works by this author on: GSW Google Scholar Bin He; He Sun-Lin Chung; Chung 2Department Geosciences, National Taiwan University, Taipei 10699, Martin A. Menzies; Menzies 3Department Geology, Royal Holloway University London, Egham,...

10.1130/g20602.1 article EN Geology 2004-01-01
Coming Soon ...