Hao Yang

ORCID: 0000-0003-0258-636X
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About
Contact & Profiles
Research Areas
  • Geological and Geochemical Analysis
  • Geochemistry and Geologic Mapping
  • Paleontology and Stratigraphy of Fossils
  • High-pressure geophysics and materials
  • earthquake and tectonic studies
  • Geochemistry and Elemental Analysis
  • Geological and Geophysical Studies
  • Geology and Paleoclimatology Research
  • Paleontology and Evolutionary Biology
  • Hydrocarbon exploration and reservoir analysis
  • Marine Biology and Ecology Research
  • Geological Studies and Exploration
  • Mineralogy and Gemology Studies
  • Methane Hydrates and Related Phenomena
  • Plant Diversity and Evolution
  • Geological formations and processes
  • Isotope Analysis in Ecology
  • Geochemistry and Geochronology of Asian Mineral Deposits
  • Evolution and Paleontology Studies
  • Marine and coastal ecosystems
  • Microbial Community Ecology and Physiology
  • Occupational Health and Safety Research
  • Plant and Fungal Species Descriptions
  • Advanced Vision and Imaging
  • Non-Invasive Vital Sign Monitoring

Jilin University
2016-2025

Institute of Geology and Geophysics
2021-2025

Chinese Academy of Sciences
2021-2025

Jilin Medical University
2014-2025

Institute of Hydrobiology
2025

China University of Geosciences (Beijing)
2014-2024

Hebei University of Engineering
2024

China University of Geosciences
2014-2023

Institute of Microelectronics
2022-2023

Ministry of Natural Resources
2019-2022

Research Article| August 01, 2011 Recovery tempo and pattern of marine ecosystems after the end-Permian mass extinction Haijun Song; Song 1State Key Laboratory Biogeology Environmental Geology Ministry Education, China University Geosciences, Wuhan 430074, China2School Earth Environment, Leeds, Leeds LS2 9JT, UK Search for other works by this author on: GSW Google Scholar Paul B. Wignall; Wignall * 2School *E-mails: p.wignall@see.leeds.ac.uk; jntong@cug.edu.cn. Zhong-Qiang Chen; Chen 3School...

10.1130/g32191.1 article EN Geology 2011-07-04

Research Article| May 01, 2010 Cyanobacterial blooms tied to volcanism during the 5 m.y. Permo-Triassic biotic crisis Shucheng Xie; Xie 1State Key Laboratory of Geological Processes and Mineral Resources, China University Geosciences, Wuhan 430074, Search for other works by this author on: GSW Google Scholar Richard D. Pancost; Pancost 2Organic Geochemistry Unit, Bristol Biogeochemistry Centre, School Chemistry, Bristol, Cantock's Close, BS8 1TS UK Yongbiao Wang; Wang 3Key Biogeology...

10.1130/g30769.1 article EN Geology 2010-04-30

Research Article| April 01, 2012 Microbial lipid records of highly alkaline deposits and enhanced aridity associated with significant uplift the Tibetan Plateau in Late Miocene Shucheng Xie; Xie * 1State Key Laboratory Biogeology Environmental Geology, China University Geosciences, Wuhan 430074, China2Organic Geochemistry Unit, Bristol Biogeochemistry Centre Cabot Institute, School Chemistry, Bristol, Cantock's Close, BS8 1TS, UK *E-mail: xiecug@163.com. Search for other works by this author...

10.1130/g32570.1 article EN Geology 2012-02-28

Abstract The carbon (δ13Corg) and nitrogen (δ15N) isotopic compositions of bulk organic matter were analyzed in two high-resolution Permian-Triassic transitional sections containing microbialite south China. results from these shallow-marine show that an abrupt negative shift δ15N, ∼+3‰ to ∼0‰, occurred immediately after the latest Permian mass extinction (LPE) both sections, concurrent with a distinct δ13Corg. persistently low values δ15N suggest that, following LPE, microbial fixation...

10.1130/g32024.1 article EN Geology 2011-05-25

Abstract The Huangzhishan section, 40 km from the well-known Meishan Zhejiang Province, South China, records a carbonate–siliciclastic Permian/Triassic (P/Tr) boundary succession. P/Tr sequences in both sections correlate well with one another, although succession is much thicker at than its equivalent Meishan. transition constrained by Neogondolella yini, N. meishanensis and Hindeodus parvus conodont zones. Of these, between first two zones marks end-Permian mass extinction horizon. base of...

10.1080/08120090903002607 article EN Australian Journal of Earth Sciences 2009-07-14

Abstract Subduction of the Paleo‐Pacific Plate caused widespread Mesozoic magmatism, lithospheric deformation and thinning, mineralization along continental margin East Asia. However, details this subduction process remain unclear. To investigate regional geodynamic evolution processes Plate, we carried out a geochronological, geochemical, Sr‐Nd‐Hf isotopic study Middle‐Late Jurassic adakitic lavas in Hailar Basin, northeast (NE) China. These rocks have relatively high Sr contents (434–877...

10.1029/2019tc005687 article EN Tectonics 2019-11-20
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