2nd International Conference on Quaternary, مهر ماه ۱۴۰۰

Accepted papers in 2nd International Conference on Quaternary

• Early Pleistocene climate in north Iran and its correlation with EasternAsia

• Current status of Epipalaeolithic studies in South-Easter Caspian Sea

• Toward the understanding of (post)pedogenic processes behind the peaks and lows of commonly used climate proxies

• Active faulting, earthquakes, and geomorphology of the Main Kopeh Dagh fault, Turkmenistan

• Active tectonics along the Khazar fault (Alborz, Iran)

• Active tectonics of the Kalabagh Fault in Pakistan: implications from morphotectonics and luminescence dating

• Age of the Khvalynian Strait in the Late Pleistocene History of the Manych Depression

• Application of landform planation index (LPI) in identifying planation surfaces and paleotopography of Gorgan loess plateau (northeast of Iran)

• Arctic Oscillation Modulates climate over Northeast Iran

• Can Past Holocene climates and environments be used as analogs for predicting future environmental responses to global warming?

• Changing the motion of Ladar fault during Quaternary, Khur area, Central Iran

• Clay mineralogy of the sediments in Sabzevar playa, NE Iran; implication for the late quaternary climate changes

• Climate change and its footprint on the geohazard amplification in Iran

• New evidence of Late Pleistocene hominin occupations in the Southern Caspian Sea Corridor

• high-resolution paleoclimate record from SE Iran reveals extreme sensitivity of West Asia to temperature changes since the Little Ice Age

• Development of cryogenic processes as a factor in the loess formation in the Lower Volga valley

• Environmental Changes in Lakes of Iran in Anthropocene epoch (Case study: Gavkhuni Swamp)

• Evaluation of the applicability of four global grid precipitation datasets in Iran and analysis of Iran’s modern precipitation features

• Forcing and feedback mechanisms of rainfall on centennial to millennial timescales

• Geochemical indicators of source area and weathering intensity for the loess-paleosol sequence of Neka-Abelou, Northern Iran

• Geohazard aspects of Quaternary faulting within Tehran Region, NNW of Iran

• Holocene moisture variations in western arid central Asia inferred from loess records from NE Iran

• How did Humans Adapt in the Eastern Farming-pastoral zone during the Medieval Warm Period?

• Impact of Climate change and Caspian Sea level fall on decline of Gorgan Bay

• Influence of the composition and properties of Khvalynsk deposits on the evolution of soils and soil cover in the north-western part of the Caspian Lowland (based on the results of mineralogical and micromorphological studies)

• Landscape evolution in the northeastern Iranian Plateau reconstructed from Late Pleistocene to Holocene sediment archives – a project outline

• Living on Quaternary Faults in Iran; High exposure problem in Earthquake Risk

• Loess-paleosol sequence over ۲۳,۰۰۰ years ago in Gorgan

• Lower Volga loess-paleosol sequences

• Luminescence chronology of the great Khvalynian transgression from the Kosika section (Lower Volga)

• Massive dust plumes over West Asia during North Atlantic cold events revealed by a dust record from southeastern Iran

• Middle Pleistocene Cave of Qaleh Kurd: the oldest human occupation in IRAN

• Mineralogical and geochemical characteristics of vesicular horizons of desert soils in the Rayen region-Kerman

• Modern pedogenesis on loess along a climate gradient in Northern Iran

• New data on the structure of the loess-soil series of Tajikistan

• Palaeoenvironmental reconstructions in drylands – an example from the Binaloud Mountains in northeastern Iran

• Paleoclimate and Palaeoenvironment of the Central Zagros

• Paleoclimate implications from grain-size analysis of loess-paleosol sequences from the Carpathian Basin

• Pedogenesis- a likely process to explain the magnetic properties of the Late Pleistocene loess-paleosol sequence at Chenarli, northeastern Iran

• Pedogenetic response to climatic fluctuations within the last glacialinterglacial cycle in the Lower Volga basin

• Pedostratigraphy of the Kuban loess-paleosol sequences

• Persian Gulf Holocene sedimentary environment based on two cores in shallow part of Bandar Abbas and Bushehr

• Quantitative estimates of Holocene glacier meltwater variations on the Western Tibetan Plateau

• Quaternary geology, active tectonics and urban development of the Tehran city

• The dating evidence for the earliest domesticated cattle and sheep/goats and pastoralism history in Gansu-Qinghai regions, NW China

• Rock Magnetic Records of Baluchabad Loess-Paleosol Sequences, Northern Iran

• Soil erosion and its trend in Iran by comparing several case studies

• Soil Erosion Susceptibility Mapping Using GIS and AHP Case Study Kalat-e-Naderi, Northeast Iran

• Southeast Caspian coast evolution during Holocene

• Speleothems: a Quaternary archive of hydroclimate change in Iran

• Stages of loess accumulation of the multilayer Kulbulak Palaeolithic site (Uzbekistan)

• Stratigraphy and Moisture Changes revealed from Iranian Loess- Paleosol in the Western Arid Central Asia since the Last Interglacial

• Structure and chronology of the Chocolate clays facies of the Lower Volga

• Subsurface erosion by soil piping – significance and consequences

• Taman loess-paleosol sequence: structure, age, genesis

• The analysis of Meteorological Parameters Influencing dust Genesis over the Middle East

• The diffusion of animal husbandry in Eurasia and its influence on Hexi Corridor, NW China

• The effect of flood on soil degradation in Gorganrud River Basin

• The Effects of the Southern Zagros Folded Zone on the Adaptive Strategies of the Late Pleistocene Human Occupations in Fars Province

• The Holocene events in the Caspian Sea

• Climate variability analysis for evolution effect over the Garmsar Alluvial fan, Based on field measurements

• The Late Quaternary Environmental changes in Iran

• The Paleolithic cave of Qaleh Kord (Qazvin, IRAN): geoarchaeological study by using micromorphology and physical-chemical analysis

• The role of the aeolian factor in the formation of the landforms of the Lower Volga region

• The spatial and possess analyses of piping and gully head erosions using unmanned aerial vehicles (UAV) images