2010
DOI: 10.3103/s0145875210050054
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A lithofacies model of upper jurassic productive deposits in the eastern part of the Shirotnoye Priobie region (Western Siberia)

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“…The Vakh basin lies some 300 km south of the boundary of continuous permafrost (Vasil'chuk and Vasil'chuk, 2014). Only island permafrost is found in this area, mostly associated with the peat soils (Histosols) of the peatlands, whereas forest Podzols and Stagnosols have no permafrost horizon in the profile (Vasilevskaya et al, 1986).…”
Section: Methodsmentioning
confidence: 81%
“…The Vakh basin lies some 300 km south of the boundary of continuous permafrost (Vasil'chuk and Vasil'chuk, 2014). Only island permafrost is found in this area, mostly associated with the peat soils (Histosols) of the peatlands, whereas forest Podzols and Stagnosols have no permafrost horizon in the profile (Vasilevskaya et al, 1986).…”
Section: Methodsmentioning
confidence: 81%