- Geology and Paleoclimatology Research
- Geological and Geochemical Analysis
- earthquake and tectonic studies
- Geological Formations and Processes Exploration
- High-pressure geophysics and materials
- Planetary Science and Exploration
- Marine and environmental studies
Chinese Academy of Geological Sciences
2022-2024
China University of Geosciences (Beijing)
2022
Shanghai Jiao Tong University
2022
Beijing University of Chinese Medicine
2022
Southern University of Science and Technology
2022
Shanghai University
2022
Guangdong Academy of Medical Sciences
2022
University of Chinese Academy of Sciences
2022
Chinese Academy of Agricultural Sciences
2022
Shihezi University
2022
The remnant Comei igneous province in SE Tibet has been recognized as a product of early Kerguelen mantle plume activity. In this paper, we investigate mafic dykes and sills intruded into Lakang Formation the southeastern Tethyan Himalaya. Based on new whole-rock geochemical, Sr-Nd-Pb isotopic SHRIMP zircon U-Pb geochronological data, these rocks can be divided three groups. Group 1 is composed OIB-like with lower εNd(t) (+1.78-+2.55) dated at 124.8 ± 1.7 133.3 1.5 Ma. 2 consists N-MORB-like...
Abstract We carried out a petrological, mineralogical, and geochemical study of fragmental regolith breccia clasts separated from two Chang'e‐5 (CE‐5) soil samples, CE5C0000YJYX03501GP CE5C0400, which provide an opportunity to investigate the compositional change at landing site through time. Fragmental CE‐5‐B3 contains diverse range basaltic mineral fragments, some rare Mg‐suite‐like minerals. Regolith breccias CE‐5‐B006, CE‐5‐B007, CE‐5‐B010‐08, CE‐5‐B010‐09, CE‐5‐B011‐07, CE‐5‐B016‐03...