Zihao Zhao

ORCID: 0009-0001-5310-3498
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About
Contact & Profiles
Research Areas
  • Hydrocarbon exploration and reservoir analysis
  • Geological and Geochemical Analysis
  • Geology and Paleoclimatology Research
  • earthquake and tectonic studies
  • Geological Studies and Exploration
  • High-pressure geophysics and materials
  • Geological formations and processes
  • Geochemistry and Geochronology of Asian Mineral Deposits
  • Landslides and related hazards
  • Geological and Geophysical Studies
  • Paleontology and Stratigraphy of Fossils
  • Geochemistry and Geologic Mapping

China University of Geosciences
2024

Southwest Petroleum University
2015-2018

This study explores the formation, preservation, and uplift of relict low-relief surfaces in Barkol Mountains, coupled with sedimentological geochemical insights from Hami Basin. By integrating digital geomorphic analysis, structural mapping, thermochronology, sedimentary data, research reconstructs tectonic evolution this region.Using Shuttle Radar Topography Mission (SRTM) data (3-arc-second resolution), Mountains were identified based on slope thresholds (

10.5194/egusphere-egu25-2555 preprint EN 2025-03-14

The Tian Shan is a typical active intracontinental orogenic belt that driven by the ongoing indentation of India into Eurasia. However, geological features Quaternary deformation, especially in easternmost sector near Harlik Mountain, remain elusive. Field observations, topographic analysis, and Electron Spin Resonance (ESR) dating were employed to comprehensively assess deformation evaluate pattern for this region during period. results disclose evidence northern southern foreland basins...

10.3390/rs16173343 article EN cc-by Remote Sensing 2024-09-09

Abstract. Relict low-relief surfaces, formed during tectonically quiescent periods, are prevalent within the active mountain ranges of Central Asia, but timing and processes their formation Mesozoic-Cenozoic tectonic context remain poorly understood. In Harlik Mountains easternmost Tianshan, extensive surfaces preserved. Terrain analysis structural interpretations based on DEM data reveal that these segmented by WNW-ESE striking faults, which experienced an initial phase right-lateral...

10.5194/egusphere-2024-3668 preprint EN cc-by 2024-12-17
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