A5010066846- Paleontology and Stratigraphy of Fossils
- Geological and Geochemical Analysis
- Geological Studies and Exploration
- Geological and Geophysical Studies
- Paleontology and Evolutionary Biology
- Geochemistry and Elemental Analysis
- Geochemistry and Geologic Mapping
- China's Ethnic Minorities and Relations
- Hydrocarbon exploration and reservoir analysis
- Marine and environmental studies
Senckenberg Research Institute and Natural History Museum Frankfurt/M
2021-2024
Mongolian University of Science and Technology
2020-2022
Mahasarakham University
2022
Appalachian State University
2022
Unité Évolution, Écologie et Paléontologie
2022
Université de Lille
2022
Centre National de la Recherche Scientifique
2022
Abstract A Late Devonian to (?)Early Mississippian section at Hushoot Shiveetiin gol in the Baruunhuurai Terrane of Central Asian Orogenic Belt (CAOB) exposes large parts cyclic Famennian shallow-water siliciclastic shelf deposits composed siltstones, sandstones, shales, volcaniclastics, and intercalated autochthonous carbonates. The youngest part section, possibly Early Mississippian, is represented by arkosic sandstones with plant remains. facies reflects a range from shallow-intertidal...
Abstract This report provides new stratigraphical and facies data from Devonian Carboniferous rocks in the Shine Jinst region (Trans Altai Zone, southern Mongolia) with a special focus on Lower Chuluun Formation, Middle Tsagaankhalga Upper to Mississippian Heermorit Member of Indert Formation. Facies development exhibits fundamental break carbonate platform evolution as reef building organisms were affected by major regression deposition several metres-thick conglomerates at base Tsakhir...
Abstract Upper Devonian carbonates deposited through the Frasnian/Famennian (F/F) stage boundary in Xom Nha Formation, Central Vietnam, were studied. The section is mainly composed of fossiliferous, brecciated, and laminated limestone beds, while shale beds occur a subordinate number. Microfacies generally suggests hemipelagic setting on an outer shelf environment with low sedimentation rates. A sediment accumulation rate 0.217 cm/kyrs for this calculated. does not exhibit characteristic...
Abstract The Bayankhoshuu Ruins section in southern Mongolia is characterized by strongly thrusted and folded sequences. Overall, three sections ranging from Ordovician to Carboniferous rocks were studied. Facies analysis combined with stratigraphic data provide improved lithostratigraphic descriptions of Palaeozoic successions the Mushgai region. overall marine sedimentary sequence punctuated volcanic – basaltic lava Silurian Middle Devonian age volcaniclastic bentonite tuff Late...