Dapeng Li

ORCID: 0000-0001-5817-0123
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About
Contact & Profiles
Research Areas
  • Geological and Geochemical Analysis
  • Geochemistry and Geologic Mapping
  • earthquake and tectonic studies
  • High-pressure geophysics and materials
  • Geochemistry and Elemental Analysis
  • Geochemistry and Geochronology of Asian Mineral Deposits
  • Marine and coastal plant biology
  • Machine Learning in Bioinformatics
  • Hydrocarbon exploration and reservoir analysis
  • Geology and Paleoclimatology Research
  • Protein Structure and Dynamics
  • Geomechanics and Mining Engineering
  • Paleontology and Stratigraphy of Fossils
  • Geological Modeling and Analysis
  • Genomics and Phylogenetic Studies
  • RNA and protein synthesis mechanisms
  • Geoscience and Mining Technology
  • Biocrusts and Microbial Ecology
  • Advanced Chemical Sensor Technologies
  • Remote Sensing and Land Use
  • Geological and Geophysical Studies
  • Oceanographic and Atmospheric Processes
  • Chromium effects and bioremediation
  • Bacterial Infections and Vaccines
  • Infectious Diseases and Tuberculosis

Northeast Agricultural University
2025

Shandong Geological Sciences Institute
2014-2024

China University of Geosciences (Beijing)
2014-2024

Ministry of Natural Resources
2014-2024

Shenzhen Third People’s Hospital
2024

China University of Geosciences
2009-2024

Centre de Géosciences
2024

Westlake University
2024

Nanjing University of Posts and Telecommunications
2024

Southern University of Science and Technology
2024

Orbital data indicate that the youngest volcanic units on Moon are basalt lavas in Oceanus Procellarum, a region with high levels of heat-producing elements potassium, thorium, and uranium. The Chang’e-5 mission collected samples these young lunar basalts returned them to Earth for laboratory analysis. We measure an age 1963 ± 57 million years determine their chemical mineralogical compositions. This constrains impact chronology inner Solar System thermal evolution Moon. There is no evidence...

10.1126/science.abl7957 article EN Science 2021-10-21

Abstract The Xing‐Meng Orogenic Belt is the eastern extension of Central Asian that marks boundary between North China Block and Siberian Block. Studies zircon UPb ages Hf isotopic compositions show four clastic sedimentary rock samples from different parts regional stratigraphic sequence were deposited at ages, none earlier than Mid‐ or Early Silurian. Two rocks during after Permian. Almost all zircons are igneous origin. In Silurian Devonian sediments, several modal age peaks, in Permian...

10.1002/gj.1257 article EN Geological Journal 2010-08-03

Identifying the mechanism of gold deposition is important to reveal ore-forming processes and genesis. The giant Dayingezhuang deposit, with 283 tons proven resources, located in northwestern Jiaodong province, China. Pyrite dominant sulfide minerals visible dominates Au resources. Five types pyrite were identified at deposit: (1) Py-1a euhedral grain Co– Ni-rich content; (2) Py-1b subhedral anhedral intermediate rich Co, Ni, As minor Te; (3) Py-2a crystalizes a mass mineral inclusions; (4)...

10.1016/j.oregeorev.2022.104992 article EN cc-by-nc-nd Ore Geology Reviews 2022-06-17

Abstract The Y angla copper deposit ( C u reserves: 1.2 M t) in the J inshajiang– L ancangjiang– N ujiang region hina is spatially associated with inong granitoid. Zircon U – P b dating shows granitoid formed at 234.1 ± to 235.6 a, and KT 2 ore body of yields a molybdenite R e– O s model age 230.9 3.2 a. ages mineralization crystallization are identical within measurement uncertainties, suggesting genitically related I ndosinian

10.1111/rge.12006 article EN Resource Geology 2013-03-27
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