Aguilar, C. , Štípská, P. , Schulmann, K. , Kylander-Clark, A. , Lexa, O. , Sukhbaatar, T. , Peřestý, V. , Jiang, Y. and Hanžl, P. 2024. Carboniferous Barrovian to Permian Buchan-type metamorphic cycles in the Mongolian Altai Zone: Implication for pressure cycles in accretionary orogens. Journal of Metamorphic Geology. 42, 979–1033.
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Researcher
Turbold Sukhbaatar
Alumni
Petrology, geochemistry and geochronology
+420221951471
turboldtmn@gmail.com
About me
I am doing my Ph.D. under the supervision of Dr. Ondrej Lexa at Charles University in Prague. My Ph.D. project is involving an interest in the internal architecture of the accretionary wedge and the collisional orogenic system in Mongolia in the Central Asian Orogenic Belt (CAOB). Before I start my Ph.D. project at Charles University in Czech Republic, I had worked at the Institute of Geology Mongolian Academy of Sciences for nearly four years.
Research interests
- Structural and metamorphic characterization of the rocks in accretionary wedges and understanding their dynamics in CAOB
- Petrology, geochemistry and geochronology (U-Pb and Lu-Hf in mineral accessories such as zircons and monazites) of the Altai orogenic system in CAOB
Research projects
Principal mechanisms of peripheral continental growth during supercontinent cycle
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The growth of eastern Pangea involves three contrasting orogenic cycles: 1) Baikalian cycle (570-540 Ma) consists of accretion of peri-Rodinian continental, Mirovoi and Panthalassan oceanic fragments to the Siberian margin followed by extensional HT reworking, the growth of magmatic arc, giant accretionary wedge and intraoceanic basin. 2) Altai cycle is typified by crustal thickening followed by syn-extensional melting of the accretionary wedge (420-380 Ma) and the opening of Mongol-Okhotsk ocean.
Publications
Sukhbaatar, T. , Schulmann, K. , Janoušek, V. , Soejono, I. , Lexa, O. , Míková, J. , Hora, J. , Song, D. , Xiao, W. , Poujol, M. and 2024. Magmatic and sedimentological arguments for an Ediacaran active margin in the Bayankhongor Zone in western Mongolia, Central Asian Orogenic Belt. Gondwana Research. 134, 385–409.
DOI Google ScholarSukhbaatar, T. , Lexa, O. , Schulmann, K. , Aguilar, C. , Štípská, P. , Wong, J. , Jiang, Y. , Míková, J. and Zhao, D. 2022. Paleozoic geodynamics and architecture of the southern part of the Mongolian Altai Zone. Tectonics. 41, e2022TC007498.
DOI Google ScholarRen, Q. , Zhang, S. , Sukhbaatar, T. , Zhao, H. , Wu, H. , Yang, T. , Li, H. , Gao, Y. and Jin, X. 2021. Did the Boreal Realm extend into the equatorial region? New paleomagnetic evidence from the Tuva–Mongol and Amuria blocks. Earth and Planetary Science Letters. 576.
DOI Google ScholarRen, Q. , Zhang, S. , Sukhbaatar, T. , Zhao, H. , Wu, H. , Yang, T. , Li, H. , Gao, Y. and Jin, X. 2021. Did the Boreal Realm extend into the equatorial region? New paleomagnetic evidence from the Tuva–Mongol and Amuria blocks. Earth and Planetary Science Letters. 576, 117246.
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