Hongfei Zhang

ORCID: 0000-0002-4659-4241
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About
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Research Areas
  • Geological and Geochemical Analysis
  • earthquake and tectonic studies
  • High-pressure geophysics and materials
  • Geochemistry and Geologic Mapping
  • Geochemistry and Geochronology of Asian Mineral Deposits
  • Geochemistry and Elemental Analysis
  • Recommender Systems and Techniques
  • Geological and Geophysical Studies
  • Topic Modeling
  • Geomechanics and Mining Engineering
  • Single-cell and spatial transcriptomics
  • Gene expression and cancer classification
  • Higher Education and Teaching Methods
  • Computer Graphics and Visualization Techniques
  • Metallurgy and Material Forming
  • Osteoarthritis Treatment and Mechanisms
  • High Temperature Alloys and Creep
  • Geological Studies and Exploration
  • Advanced Vision and Imaging
  • Natural Language Processing Techniques
  • Advanced Graph Neural Networks
  • Hydrocarbon exploration and reservoir analysis
  • Blood donation and transfusion practices
  • Statistical Mechanics and Entropy
  • International Arbitration and Investment Law

China University of Geosciences
2011-2024

Huashan Hospital
2024

Fudan University
2024

Xi'an Jiaotong University
2018-2024

Northeast Forestry University
2024

Tianshui Normal University
2022

Hebei University of Engineering
2022

Chinese PLA General Hospital
2020

Nanchang Institute of Technology
2020

North China University of Science and Technology
2019

Research Article| May 01, 2004 Geochemical, age, and isotopic constraints on the location of Sino–Korean/Yangtze Suture evolution Northern Dabie Complex, east central China Derek L. Bryant; Bryant 1Department Earth Environmental Sciences, Vanderbilt University, Nashville, Tennessee 37235, USA Search for other works by this author on: GSW Google Scholar John C. Ayers; Ayers Shan Gao; Gao 2Faculty University Geosciences, Wuhan 430074, China, Key Laboratory Continental Dynamics, Department...

10.1130/b25302.2 article EN Geological Society of America Bulletin 2004-01-01

An integrated study involving whole-rock and Sr–Nd–Hf isotope geochemistry zircon geochronology trace element combined with detailed field investigation was carried out for the composite Meiwu batholith in West Qinling orogenic belt of central China to probe origins its compositional diversity emplacement history. The is composed quartz diorite, granodiorite biotite granite, abundant mafic magmatic enclaves minor tonalitic granodiorite. crystallization age ∼240–245 Ma. Geochemical isotopic...

10.1093/petrology/egv032 article EN Journal of Petrology 2015-06-01

Dislocation recovery lowering the driving force for recrystallization would be able to suppress latter in Ni-based superalloy single crystals, but was believed unlikely due their low stacking-fault energy. Defying this traditional wisdom, here we show that efficient can realized once γ′-precipitates start dissolve. Our microscopy evidence tracking distribution/configuration of dislocations reveals shifting γ/γ′ interphase boundaries release trapped there, facilitating annihilation and...

10.1080/21663831.2024.2312146 article EN cc-by Materials Research Letters 2024-02-06

With the extensive integration of Internet, social networks and internet things, Internet things has increasingly become a significant research issue. In application scenario, one greatest challenges is how to accurately recommend or match smart objects for users with massive resources. Although variety recommendation algorithms have been employed in this field, they ignore text resources which can effectively improve effect recommendation. paper, object approach named based on topic...

10.1016/j.dcan.2022.04.025 article EN cc-by-nc-nd Digital Communications and Networks 2022-05-06

Abstract A combination of U-Pb zircon ages and geochemical Sr-Nd-Hf isotopic data are presented for the Early Paleozoic granodiorites from Haoquangou Baimawa plutons in order to probe crustal thickness variation eastern North Qilian diachronous evolution orogen. The formed at 436–435 Ma have high Sr/Y ratios (63–117). Elemental combined with modeling comparisons experimental suggest that they were produced melting relatively juvenile mafic rocks thickened lower crust. Together other...

10.1130/l1129.1 article EN cc-by Lithosphere 2019-12-19
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