Fan Yang

ORCID: 0000-0002-1518-2527
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About
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Research Areas
  • Geological and Geochemical Analysis
  • Geochemistry and Geologic Mapping
  • earthquake and tectonic studies
  • High-pressure geophysics and materials
  • Hydrocarbon exploration and reservoir analysis
  • Crystallization and Solubility Studies
  • X-ray Diffraction in Crystallography
  • Geochemistry and Elemental Analysis
  • Geological and Geophysical Studies
  • Electric and Hybrid Vehicle Technologies
  • Remote-Sensing Image Classification
  • Advanced Battery Technologies Research
  • Geological Modeling and Analysis
  • Heavy metals in environment
  • Soil Carbon and Nitrogen Dynamics
  • Soil Geostatistics and Mapping
  • Geological Studies and Exploration
  • Seismic Imaging and Inversion Techniques
  • Paleontology and Stratigraphy of Fossils
  • Mineral Processing and Grinding
  • Electric Vehicles and Infrastructure
  • Clay minerals and soil interactions
  • Mine drainage and remediation techniques
  • Soil Management and Crop Yield
  • Microbial Community Ecology and Physiology

Lanzhou University
2019-2025

Qinghai University
2025

State Key Laboratory of Plateau Ecology and Agriculture
2025

Dalian University of Technology
2019-2024

Northwestern Polytechnical University
2023-2024

China University of Petroleum, Beijing
2018-2024

Chinese Academy of Geological Sciences
2016-2024

China University of Geosciences (Beijing)
2015-2024

The University of Adelaide
2018-2024

Shanghai University
2023-2024

Abstract The margin of NE China, a part the West Pacific metallogenic belt, contains innumerable low-sulphidation mineral deposits. Gold deposits in this region can be classified into three distinct types based on geology and ore paragenesis: (1) epithermal silver–gold deposits, (2) tellurium–gold (3) Ores formed during late Early Cretaceous early Late reflect periods: Fuxin Stage at 115.98 ± 0.89 Ma, Quantou 107.2 0.6 Ma or <103 Qingshankou Yaojiajie < 97 88.2 1.4 Ma. is dominated by...

10.1080/00206814.2012.729658 article EN International Geology Review 2012-11-01

The Qinling Orogen in Central China records the history of a complex geological evolution and tectonic transition from compression to extension during Late Mesozoic, with concomitant voluminous granitoids formation. In this study, we present results petrological, geochemical, zircon U-Pb-Lu-Hf isotopic studies on Lengshui felsic dykes Luanchuan region East Orogen. We also compile published geochronological, Hf data contour maps. newly obtained age yield two group ages at ∼145 Ma 140 for...

10.1016/j.gsf.2019.03.003 article EN cc-by-nc-nd Geoscience Frontiers 2019-03-23

Abstract Cities play a fundamental role in policy decision-making processes, necessitating the availability of city-level population projections to better understand future dynamics and facilitate research across various domains, including urban planning, shrinking cities, GHG emission projections, GDP disaster risk mitigation, public health assessment. However, current absence for China is significant gap knowledge. Moreover, aggregating grid-level city level introduces substantial errors...

10.1038/s41597-023-02735-6 article EN cc-by Scientific Data 2023-11-17

Molybdenum (Mo) is an important globally strategic metal and mostly occurs as molybdenite (MoS2) in diverse Mo deposits. The Yuku ore field includes multiple porphyry-skarn deposits forms significant world-class cluster the Qinling molybdenum belt, central China. Previous studies on were largely related to its genesis, did not highlight post-mineralization modifications that are formulate prospecting strategies. exhumation preservation processes of through tectonic events also remain poorly...

10.1016/j.oregeorev.2024.105973 article EN cc-by-nc-nd Ore Geology Reviews 2024-03-11

ABSTRACT As one of the most sensitive and fragile alpine ecosystems in Qilian Mountains, meadow holds significant scientific importance understanding changes characteristics soil bacterial community response to altitude aspect variations. In our study, we analyzed composition, diversity, function communities meadows at different altitudes aspects their relationship with environmental factors. Our results indicate that orientation significantly influences diversity index composition...

10.1002/ece3.70769 article EN cc-by Ecology and Evolution 2025-01-01

With the rapid development of analytical techniques, especially in situ Lu-Hf, Rb-Sr, U-Pb, fission-track and (U-Th)/He dating garnet, zircon, apatite other accessory minerals, several important geological issues have been successfully resolved or re-determined past decade [...]

10.3390/min15020169 article EN Minerals 2025-02-11

The Hongdonggou Pb-Zn polymetallic ore deposit, located in the southwestern part of Luanchuan Mo-W-Pb-Zn-Ag mineralization Henan Province, China, is an important East Qinling metallogenic belt. orebodies which are vein, bedded and lenticular, mainly hosted syenite porphyry, formed within carbonate clastic rocks Yuku Qiumugou formations partially. genesis deposit has previously been argued to be hydrothermal-vein type or skarn-hydrothermal type. In this study, we report results Rb-Sr isotopic...

10.1016/j.gsf.2016.06.001 article EN cc-by-nc-nd Geoscience Frontiers 2016-06-23

The Qinling orogenic belt is a complex subduction–accretion–collision orogen that welded the North China Craton and Yangtze during final continental collision in Triassic. Xiong'ershan area, located east Qinling, exposes typical Triassic syenite pluton several contemporaneous Mo, Au, Cu deposits. aegirine–augite syenites from Mogou are characterized by alkalic to peralkalic (total alkali Na 2 O + K = 13.95–14.63 wt.%, CaO 0.06–2.87 wt.%), shoshonitic features (K 11.86–14.34 wt.%). Zircon...

10.1002/gj.3166 article EN Geological Journal 2018-03-05

The continental margin of Northeast China, an important part the margin-related West Pacific metallogenic belt, hosts numerous types gold-dominated mineral deposits. Based on ore deposit geology and isotopic dating, we have classified hydrothermal gold–copper deposits in this region into four distinct types: (1) gold-rich porphyry copper deposits, (2) porphyry-like (3) medium-sulphidation epithermal copper–gold (4) high-sulphidation gold These formed during stages or periods, at 123.6 ± 2.5...

10.1080/00206814.2012.695472 article EN International Geology Review 2012-06-21
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