Davlatkhudzha Murodov

ORCID: 0000-0002-2970-0583
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About
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Research Areas
  • earthquake and tectonic studies
  • High-pressure geophysics and materials
  • Geological and Geochemical Analysis
  • Hydrology and Watershed Management Studies
  • Water Resources and Management
  • Groundwater and Watershed Analysis
  • Geology and Paleoclimatology Research
  • Tree-ring climate responses
  • Groundwater and Isotope Geochemistry
  • Geophysical and Geoelectrical Methods
  • Transboundary Water Resource Management
  • Archaeology and ancient environmental studies

Academy of Sciences of the Republic of Tajikistan
2022-2024

Lanzhou University
2022-2023

Institute of Tibetan Plateau Research
2013-2023

Chinese Academy of Sciences
2013-2023

University of Chinese Academy of Sciences
2018

Center for Excellence in Tibetan Plateau Earth Sciences
2013-2018

We present herein detailed images of the Moho depth and Vp/Vs ratio along ANTILOPE-1 profile beneath western Tibetan Plateau derived from receiver function analysis. Along profile, a rapidly northward-dipping extends ∼50 km below Himalaya to ∼80 across Indus–Yarlung suture, shallowing ∼66 under central Lhasa terrane. The shows dramatic increase north Bangong–Nujiang suture ∼93 Qiangtang terrane where it reaches maximum observed this before steeply rising ∼73 km. interpret both 15 20 offsets...

10.1093/gji/ggy170 article EN Geophysical Journal International 2018-04-26

The Cenozoic convergence between India and Asia has created Earth’s thickest crust in the Pamir–Tibetan plateau, leading to broadly distributed deformation extensive crustal shortening; however, of high plateau is still poorly constrained. variation Moho topography composition beneath an important correlation with major tectonic units. In this study, results receiver functions have been reviewed analyzed observe variations depth Vp/Vs ratio plateau. We found a notable SE–NW-oriented deep...

10.3389/feart.2022.821497 article EN cc-by Frontiers in Earth Science 2022-03-15

Abstract The Amu Darya contributed 70% of the flow to Aral Sea in central Asia before 1960s, when streamflow started dwindle. severe environmental and socioeconomic disaster happened mainly due intensified water abstraction with backdrop climate change. However, knowledge up most recent extreme conditions their changes, as well relations basin, is still lacking. This study aims understand hydrometeorological past several decades, especially upper basin. spatial patterns means all temperature...

10.1175/jhm-d-22-0025.1 article EN Journal of Hydrometeorology 2022-12-12
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