Hu Wang

ORCID: 0000-0001-5663-7981
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About
Contact & Profiles
Research Areas
  • earthquake and tectonic studies
  • Geological and Geochemical Analysis
  • High-pressure geophysics and materials
  • Geology and Paleoclimatology Research
  • Remote Sensing and Land Use
  • Seismology and Earthquake Studies
  • Seismic Waves and Analysis
  • Seismic Imaging and Inversion Techniques
  • Hydrocarbon exploration and reservoir analysis
  • Earthquake Detection and Analysis
  • GNSS positioning and interference
  • Geochemistry and Geologic Mapping
  • Landslides and related hazards
  • Geomechanics and Mining Engineering
  • Geological and Geophysical Studies
  • Geoscience and Mining Technology
  • Ionosphere and magnetosphere dynamics
  • Marine and coastal ecosystems
  • Environmental Changes in China
  • Cancer-related molecular mechanisms research
  • Inertial Sensor and Navigation
  • Geological Studies and Exploration
  • Environmental Quality and Pollution
  • Color perception and design
  • Methane Hydrates and Related Phenomena

Southwest Jiaotong University
2017-2025

Xinjiang University
2015-2024

Chinese Academy of Surveying and Mapping
2013-2024

Tongji University
2009-2023

Henan Normal University
2023

China University of Geosciences
2020-2022

Dalian Maritime University
2022

Chengdu University of Technology
2021

Yanshan University
2020

Xi'an University of Science and Technology
2020

Compared with marine facies shale strata, lacustrine strata are more complicated in geological conditions, and thus difficult to explore develop. To realize economic exploration development of oil, the regularities accumulation high yield retained movable petroleum should be understood first. In this work, taking Kong 2 Member Sha 3 Paleogene Huanghua depression Bohai Bay Basin as examples, based on previous joint analysis results over ten thousand core samples latest oil testing, production...

10.1016/s1876-3804(20)60106-9 article EN cc-by-nc-nd Petroleum Exploration and Development 2020-10-01

Underwater compressed air energy storage was developed from its terrestrial counterpart. It has also evolved to underwater natural gas and hydrogen in recent years. UWCGES is a promising technology for the marine environment subsequently of significant interest attention. However, it still immature. In this study, latest progress both academic industrial fields summarized. Additionally, challenges facing emerging are analyzed. The pros cons provided differentiated variant. Technical,...

10.3390/app12189361 article EN cc-by Applied Sciences 2022-09-18

Abstract The coseismic surface ruptures associated with large earthquakes contribute to severe damage near-fault buildings through fault deformation. However, previous studies simplified geological conditions and were based mainly on numerical physical simulations. In other words, the scarcity of earthquakes, especially for active thrust faults, limits understanding mechanisms building near faults. Herein, study selected 2008 Mw7.9 Wenchuan earthquake as an example. Based compass...

10.2113/2025/lithosphere_2024_207 article EN cc-by Lithosphere 2025-01-21

Late Quaternary rupture behavior of large earthquakes along the Yingxiu-Beichuan fault and Longmen Shan zone has been focus geoscientists since 2008 Wenchuan earthquake. However, most studies have concentrated on southern segment from Yingxiu to Beichuan. Here we opened trenches used borehole drilling in Guixi Pingxi northern (north Beichuan) with following paleoseismic results: (1) Trenches at reveal that least one event occurred prior earthquake ages 770–955 A.D. 665–1030 determined two...

10.1002/2014tc003649 article EN Tectonics 2014-10-28

The growth mechanisms of the southeastern Tibetan Plateau are debated between models Oligocene shortening and lateral extrusion coherent crustal blocks versus Late Miocene flow low-viscosity lower crust. To test these models, we examine brittle deformation north-striking Anninghe fault, which has been acting as a left-lateral strike-slip fault since time, using structural bedrock low-temperature thermochronologic methods. Different from previous interpretations motion, our observations...

10.1080/00206814.2020.1858354 article EN International Geology Review 2020-12-30

Historical and instrumental records of large earthquakes within the southeastern region Tibetan Plateau appeared to show an irregular complex behaviour in seismic activity over a relatively short-time period. However, whether this kind earthquake can be extrapolated long-time periods is not well addressed. Herein, we present about 8000 yr record using palaeoseismological techniques from Zemuhe fault (ZMHF) assess complexity faulting Plateau. The ZMHF along with Anninghe (ANHF) Xiaojiang...

10.1093/gji/ggs095 article EN Geophysical Journal International 2013-01-30

The 2008 Mw 7.9 Wenchuan earthquake occurred along the middle and northern segments of Longmen Shan fault zone at eastern margin Tibetan Plateau. Five years later, 2013 6.6 Lushan ruptured a section southern segment zone, leaving 50-km-long seismic gap between seismogenic structures two earthquakes. In our study, we use trenching calibrated radiocarbon age models to assess rupture behavior over multiple At least paleoseismic events were identified with constraints A.D. 1350–1830 525–760...

10.1130/l373.1 article EN Lithosphere 2014-10-19

Abstract Most active block boundary faults within the Tibetan plateau have been thought of as Holocene active, and are able to produce large earthquakes. However, it is unknown whether Jiali fault (JLF) has seismically in Holocene, which currently hampers efforts undertake meaningful seismic hazard assessments near southeastern part plateau. In this study, shown that JLF indeed ruptured during evidenced from geological, paleoseismic, radiocarbon dating investigations. Specifically, at least...

10.1785/0220190371 article EN Seismological Research Letters 2020-04-01

Denudational history inferred from bedrock low-temperature thermochronological data provides significant constraint to tectonic models for explaining the growth of Tibetan Plateau. Here, we present new apatite fission-track ages Luoji Shan, bounded by Anninghe and Zemuhe faults in southeastern Cooling vary c. 5 13 Ma bottom top a vertical profile. The age–elevation relationship can be interpreted as either (1) phase river incision at rate 0.16 km −1 or (2) denudation 0.40 between 10 Ma,...

10.1144/jgs2017-005 article EN Journal of the Geological Society 2017-05-15

Abstract Microfracture density in fault damage zones can reflect spatial variability that decays intensity as a function of distance from the fault, which is crucial understanding mechanical, seismological, and fluid-flow properties system. However, few studies explored characteristics fracture between two sides active dip-slip faults due to rare field observations. Here, we measured modeled microfractures across an thrust associated with 2008 Mw 7.9 Wenchuan earthquake Longmen Shan, eastern...

10.2113/2024/lithosphere_2023_193 article EN cc-by Lithosphere 2024-01-19

Abstract The central North China Craton (NCC) acts as a transition zone between the stable western and reworked eastern NCC. It is characterized by high seismic activity experienced volcanic with small magma volumes. To assess dynamic processes of NCC, particularly in marked intense differential tectonic deformation, we have obtained 3‐D radial anisotropic model crust uppermost mantle via joint inversion Love‐ Rayleigh‐wave dispersion curves ellipticity measurements. Compared to models...

10.1029/2023jb028358 article EN Journal of Geophysical Research Solid Earth 2024-11-30

Breast cancer is one of the most prevalent cancers in women worldwide. Through regulation many coding and non-coding target genes, oestrogen (E2 or 17β-oestradiol) its nuclear receptor ERα play important roles breast development progression. Despite astounding advances our understanding oestrogen-regulated genes over past decades, knowledge on targets has just begun to expand. Here we leverage epigenomic approaches systematically analyse long RNAs (lncRNAs). Similar ERα, transcription...

10.1080/15476286.2020.1777769 article EN RNA Biology 2020-06-07
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