Hongwei Yin

ORCID: 0000-0003-1766-4287
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About
Contact & Profiles
Research Areas
  • earthquake and tectonic studies
  • Geological and Geochemical Analysis
  • Hydrocarbon exploration and reservoir analysis
  • Geological and Geophysical Studies
  • Protein Degradation and Inhibitors
  • Chromatin Remodeling and Cancer
  • Cancer Mechanisms and Therapy
  • Melanoma and MAPK Pathways
  • Geological formations and processes
  • High-pressure geophysics and materials
  • Seismic Imaging and Inversion Techniques
  • Geology and Paleoclimatology Research
  • Synthetic Aperture Radar (SAR) Applications and Techniques
  • Geological Studies and Exploration
  • Click Chemistry and Applications
  • Landslides and related hazards
  • RNA regulation and disease
  • Geochemistry and Geologic Mapping
  • Geochemistry and Elemental Analysis
  • Geomagnetism and Paleomagnetism Studies
  • Peptidase Inhibition and Analysis
  • Computational Drug Discovery Methods
  • Methane Hydrates and Related Phenomena
  • Cryospheric studies and observations
  • Cutaneous Melanoma Detection and Management

Nanjing University
2015-2024

Anhui University of Science and Technology
2022-2024

Southwest Petroleum University
2013-2023

Gansu Great Wall Electrical and Electronics Engineering Research Institute
2023

St. Vincent's Hospital
2023

Changhai Hospital
2022-2023

Second Military Medical University
2022-2023

Sichuan University
2023

China Academy of Engineering Physics
2023

Huzhou University
2023

Abstract To understand the effects of substantial topographic relief on deformation localization in seismically active mountains, like Longmen Shan thrust belt eastern Tibet, sandbox experiments were performed based framework critical taper theory. First, a reference experiment revealed that angle was 12° for our experimental materials. Subsequently, different proto wedges (subcritical (6° angle), (12°), and supercritical (20°)) introduced to cover range natural relief, we used two setups:...

10.1002/2016jb013013 article EN Journal of Geophysical Research Solid Earth 2016-05-27

In this article, we present in situ U–Pb and Lu–Hf isotope data for Upper Triassic detritus the Sichuan region of northwestern South China, which was a foreland basin during Late Triassic. The aim is to determine provenance sediments constrain evolution surrounding mountain belts. age detrital zircons generally show populations at 2.4–2.6 Ga, 1.7–1.9 710–860 Ma, 410–460 210–300 Ma. By fitting zircon into tectonic, sedimentologic, palaeographic framework, propose that north Yangtze Block...

10.1080/00206814.2015.1027967 article EN International Geology Review 2015-05-14

Metal-organic frameworks (MOFs) have attracted significant research interest for supercapacitor applications due to their high-tunable conductivity and structure's pore size. In this work, we report a facile one-step hydrothermal method synthesize nickel-based metal-organic (MOF) using organic linker 4,4'-biphenyl dicarboxylic acid (BPDC) high-performance supercapacitors. The size of the Ni-BPDC-MOF nanostructure is tuned through different synthesization temperatures. Among them, sample...

10.3390/nano12122062 article EN cc-by Nanomaterials 2022-06-15

Abstract The Lower Yangtze foreland basin is situated to the northwest of early Palaeozoic Wuyi–Yunkai orogen in South China. To demonstrate its provenance history and denudation orogen, seven sandstone samples were collected from upper Ordovician Silurian strata for U–Pb dating. zircons show a broad range ages that can be linked with specific units orogen. zircon spectra late are similar those pre-orogenic strata, suggesting recycled source. dominant age population 880–740 Ma Llandovery...

10.1017/s0016756812000969 article EN Geological Magazine 2013-03-21

This article presents the results of a finite-thickness, three-dimensional (3-D) kinematic model for fault-related deformation above an active diapir. Based on field examples, models are (1) circular in map view; (2) offset by radially distributed normal faults; (3) faulted or smooth at top salt; (4) relatively unstrained flanks; and (5) highly deformed central graben, if present. Field examples suggest that diapirs may initiate with either two three master faults crossing near dome crest....

10.1306/10240606034 article EN AAPG Bulletin 2007-02-14
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