А. Hassan1,2,3, S.V. Rasskazov1,3, I.S. Chuvashova1,3, A. Al-hamud1,4
1Irkutsk State University, Irkutsk, Russia
2Al-Bass University, Homs, Syria
3Institute of Earth's Crust SB RAS, Irkutsk, Russia
4Al-Furat University, Deir ez-Zor, Syria
Hassan Abdulmonem,
664003 Irkutsk, Lenina str., 3,
Irkutsk State University, Geological Faculty,
master's student,
Homs, Syria,
Al-Bass University,
lecturer,
email: abdulmonemhassan86@gmail.com.
Rasskazov Sergei Vasilevich,
Doctor of Geology and Mineralogy, Professor,
664003 Irkutsk, Lenina str., 3,
Irkutsk State University, Geological Faculty,
Head of the Dynamic Geology Chair,
664033 Irkutsk, Lermontov, 128,
Institute of Earth’s crust of SB RAS,
Head of the Laboratory for isotopic and geochronological studies,
tel.: (3952) 51–16–59,
email: rassk@crust.irk.ru.
Chuvashova Irina Sergeevna,
Candidate of Geology and Mineralogy,
664003 Irkutsk, Lenina str., 3
Irkutsk State University, Geological Faculty,
assistant professor,
664003 Irkutsk, Lermontov str., 128,
Institute of Earth’s crust of SB RAS,
Senior Researcher,
tel.: (3952) 51–16–59,
email: chuvashova@crust.irk.ru.
Al Hamoud Adnan,
664003 Irkutsk, Lenina str., 3,
Irkutsk State University, Geological Faculty,
master's student,
Deir-Ez-Zor, Syria,
Al-Furat University lecturer,
email: hamoudadnan04@gmail.com.
Abstract. The central part of the Baikal Rift System is exhibited by the lacustrine South Baikal basin and land Barguzin and Tunka valleys. In the Late Cenozoic, the former valley developed consistently with the South Baikal basin as its distal extensional pattern, the latter underwent both extension and compression as an individual structure of the Hangay-Belaya orogenic zone.
Keywords: сenozoic, sediments, Lake Baikal, Tunka Valley, Barguzin Valley.
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Access Mode: http://geoenvir.ru/archive/g&e21-1-1/hassan17-1.htm (08.12.2021).