Lifeng Wang

ORCID: 0000-0003-2361-5772
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About
Contact & Profiles
Research Areas
  • earthquake and tectonic studies
  • Earthquake Detection and Analysis
  • High-pressure geophysics and materials
  • Geophysical and Geoelectrical Methods
  • Seismic Waves and Analysis
  • Seismology and Earthquake Studies
  • Seismic Imaging and Inversion Techniques
  • Geological and Geochemical Analysis
  • Environmental Quality and Pollution
  • Geological and Geophysical Studies
  • Diverse Aspects of Tourism Research
  • Soil Carbon and Nitrogen Dynamics
  • Remote Sensing and Land Use
  • Evaluation Methods in Various Fields
  • Environmental Changes in China
  • Peatlands and Wetlands Ecology
  • Forest Ecology and Biodiversity Studies
  • Environmental and Agricultural Sciences
  • Ecology and Vegetation Dynamics Studies
  • Geoscience and Mining Technology
  • Climate change and permafrost
  • Geophysics and Sensor Technology
  • Agronomic Practices and Intercropping Systems
  • Fire effects on ecosystems
  • Strategic Planning and Analysis

Institute of Geology, China Earthquake Administration
2009-2024

China Earthquake Administration
2014-2024

University of the East
2024

Nanjing Agricultural University
2021-2024

Shanghai Electric (China)
2024

State Grid Nanjing Power Supply Company (China)
2024

China National Petroleum Corporation (China)
2023

Changchun Observatory
2023

Czech Academy of Sciences, Institute of Geology
2023

Sichuan Agricultural University
2019-2022

Abstract The collision between India and Eurasia mobilizes multiple processes of continental tectonics. However, how deformation develops within the lithosphere across Tibetan Plateau is still poorly known a synoptic view missing. Here, we exploit an extensive geodetic observatory to resolve kinematics this diffuse plate boundary arrangement various mechanisms down upper-mantle depths. three-dimensional velocity field compatible with underthrusting below central Himalayas delamination...

10.1038/s43247-023-00815-4 article EN cc-by Communications Earth & Environment 2023-05-12

Abstract A three‐dimensional (3‐D) resistivity model around the 2014 M s 6.5 Ludian earthquake was obtained. The shows that aftershocks were mainly distributed in a shallow inverse L‐shaped conductive angular region surrounded by resistive structures. presences of this zone may be key factor leading to severe damage and surface rupture earthquake. northwest trending local belt along Baogunao‐Xiaohe fault interrupts northeast at Zhaotong‐Lianfeng middle crust, which seismogenic structure main...

10.1002/2016gl071855 article EN Geophysical Research Letters 2017-01-20

Abstract Stress transfer between earthquakes is recognized as a fundamental mechanism governing aftershock sequences. A common approach to relate stress changes seismicity rate the rate‐and‐state constitutive law developed by Dieterich: these elements are foundation of Coulomb‐rate‐and‐state (CRS) models. Despite successes Coulomb hypothesis and formulation, such models perform worse than statistical in an operational forecasting context: one reason that subject large uncertainties intrinsic...

10.1002/2014jb011183 article EN Journal of Geophysical Research Solid Earth 2014-09-23

Abstract Gongga Shan (GGS) is the highest mountain on eastern margin of Tibetan Plateau. However, mechanism for uplift still unclear due to a lack detailed geophysical studies. Inversion an array magnetotelluric data at 120 sites produced 3D resistivity model that revealed GGS massif characterized by high upper crust underlain westward dipping resistor middle crustal depths interpreted as underthrust Yangtze Craton (YC). A thin conductive layer sandwiched between these two zones resistivity....

10.1029/2021gl097394 article EN Geophysical Research Letters 2022-04-22

Abstract Upward shifts of alpine treelines and shrub expansion are occurring under climate change, Abies faxoniana (AF) Rhododendron lapponicum (RL) may become distributed at higher altitudes. How do abiotic factors litter quality modulate the effects soil fauna on carbon release in this context? A field decomposition experiment involving foliar AF RL was conducted along an elevation gradient encompassing coniferous forest, shrubland meadow by using litterbags with different mesh sizes (3...

10.1038/s41598-019-47072-0 article EN cc-by Scientific Reports 2019-07-22

Research Article| November 28, 2017 Seismic and Aseismic Moment Budget Implication for the Potential of Parkfield Segment San Andreas Fault Sylvain Michel; Michel aBullard Laboratories, Department Earth Sciences, University Cambridge, Madingley Road, Cambridge CB3 0EZ, United Kingdom, Sylvain_michel@live.freAlso at Geology Planetary California Institute Technology, 1200 E. Boulevard, Pasadena, 91125. Search other works by this author on: GSW Google Scholar Jean‐Philippe Avouac; Avouac...

10.1785/0120160290 article EN Bulletin of the Seismological Society of America 2017-11-28

Thermal instabilities below the seismogenic zone by shear heating and temperature-weakening friction drive slow slip, tremors.

10.1126/sciadv.abb2057 article EN cc-by-nc Science Advances 2020-09-04

Both aftershocks and geodetically measured postseismic displacements are important markers of the stress relaxation process following large earthquakes. Postseismic can be related to creep‐like in vicinity coseismic rupture by means inversion methods. However, results slip inversions typically non‐unique subject uncertainties. Therefore, we explore possibility improve mechanical constraints. In particular, take into account physical understanding that deformation is stress‐driven, occurs...

10.1029/2011jb009017 article EN Journal of Geophysical Research Atmospheres 2012-06-08

SUMMARY Very clear coseismic electric and magnetic signals accompanying seismic waves were observed during the 2017 Mw 6.5 Jiuzhaigou earthquake, which took place in western China. In order to understand generation mechanism of these signals, we simulate responses this specific earthquake based on three mechanisms, namely, electrokinetic effect, motional induction effect rotation coil-type magnetometer. We conduct simulations using a point source model realistic layered earth compare data...

10.1093/gji/ggaa374 article EN Geophysical Journal International 2020-08-07

Abstract We propose a numerical method for calculating exact all‐time apparent resistivity time‐domain transient electromagnetic method. According to the behaviour of kernel function Y' ( Z ) ∂B z /∂T , can be distinguished into early‐time > 1.6), transition point = 1.6) and late‐time < stages central loop configuration. First resisitivities are calculated using earlytime expressions then curve is founded by combining two over point. Although Y B single valued, there also 1.6 should...

10.1002/cjg2.419 article EN Chinese Journal of Geophysics 2003-09-01
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