2019
DOI: 10.32014/2019.2518-170x.26
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On the Closing Date of the Jungar-Balkhash Paleobasin

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“…As a result, the capacity of accumulated sedimentary cover in the Dzungarian trough is 16 km [7], while that of Alakol is four times less. The Dzungarian trough area is five times larger than that of Alakol.…”
Section: Issn 2224-5278mentioning
confidence: 97%
“…As a result, the capacity of accumulated sedimentary cover in the Dzungarian trough is 16 km [7], while that of Alakol is four times less. The Dzungarian trough area is five times larger than that of Alakol.…”
Section: Issn 2224-5278mentioning
confidence: 97%