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The Serie Lectures Beidi Lecture Hall started with the First Lecture given by Academician Sun Youhong, President of CUGBApr 22, 2023

On April 22nd the lecture entitled Cherish the Earth, Harmonious Coexistence between Human and Nature was held in China University of Geosciences Beijing as the starting lecture for the series lectures Beidi Lecture Hall on the occasion of the forthcoming 54th Earth Day.

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Seminar on Comprehensive Bilateral Scientific Researches between China and Russia held in CUGB On April 19th, the Sino-Russian bilateral seminar on Baikal Comprehensive scientific research was held in the university.
Teachers from more than 40 universities gathered in CUGB to discuss the development and growth of teachers From April 8th to 9th, the eighth project quarterly meeting sponsored by the Sustainable Development Alliance of the Center for Faculty Development in Colleges and Universities and co-sponsored by CUGB was held on campus in CUGB.
Beijing and Wuhan go hand in hand: University leaders went to China University of Geosciences (Wuhan) for investigation On April 6 leaders of China University of Geosciences (Beijing) went to China University of Geosciences (Wuhan) to make an investigation.

RESEARCH

Geosciences Research

Scientific research is the foundation and source of the vitality of research universities, and the ability of scientific and technological innovation is the concentrated embodiment of the core competitiveness of universities.
Taking inheritance and innovation as its own responsibility, CUGB adapts to the national scientific research management system and operation mechanism, faces the frontier of Geosciences and national strategic needs, and based on the needs of "double first-class" discipline construction and school development, promotes the collaborative innovation of industry university research, promotes the collaborative development of basic research and applied research, continuously enhances the innovation consciousness of teachers and students, and actively seeks new growth points of scientific research development.

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Aug 26, 2025

School of Earth Sciences And Resources

Huixia Ding：Himalayan “S-type” granite generated from I-type sources【PNAS】

Aug 11, 2025

School of Earth Sciences And Resources

Li Tang：Key factors controlling the late Mesozoic diverse porphyry Mo, Cu, and Au mineralization in the Qinling Orogenic Belt, Central China【GSA Bulletin】

Aug 11, 2025

School of Earth Sciences And Resources

Li Tang：Calcium and molybdenum isotopes trace eclogitic crust recycling in formation of unique carbonatite-hosted Mo-REE-U-Nb deposits in orogenic belt【EPSL】

Aug 9, 2025

Institute of Earth Sciences

Zhuang Ma：Nickel isotopic variations in Ni–Cu sulfide deposits: from theoretical predictions to natural observations【GCA】

Huixia Ding：Himalayan “S-type” granite generated from I-type sources【PNAS，2025】

Partial melting of metasedimentary rocks is generally accepted as the source of peraluminous Himalayan leucogranites—they are commonly considered as pure “S-type” (sedimentary source) granites.

Li Tang：Key factors controlling the late Mesozoic diverse porphyry Mo, Cu, and Au mineralization in the Qinling Orogenic Belt, Central China【GSA Bulletin，2025】

The Qinling Orogenic Belt of Central China hosts one of the world-class porphyry Mo belts (proven Mo resource of 8.43 Mt), several porphyry-skarn Cu and Au deposits, and abundant coeval barren granitoid intrusions.

Li Tang：Calcium and molybdenum isotopes trace eclogitic crust recycling in formation of unique carbonatite-hosted Mo-REE-U-Nb deposits in orogenic belt【EPSL，2025】

Carbonatites in orogenic belts provide an exceptional natural laboratory for investigating crust-to-mantle recycling processes and for understanding the fluxes of carbon and other materials in subduction zones.

Zhuang Ma：Nickel isotopic variations in Ni–Cu sulfide deposits: from theoretical predictions to natural observations【GCA，2025】

Extremely light and highly variable δ60/58Ni values have been observed in sulfide-bearing rocks globally, making Ni isotopes a potential tracer for the genesis of magmatic sulfide deposits.