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Loess-like siltstones from the urzhumian (middle permian) red beds of Kazan Volga Region, Russia

Mouraviev F.A., Kropotova T.V., Gareev B.I., Batalin G.A., Gordeev A.S.

focused on the massive, non-pedogenic, loess-like siltstones, which are common within the fluvio

КЕРОГЕННЫЕ ОТЛОЖЕНИЯ В КОТ-д’ИВУАРЕ

Матюрен Й.К.

siltstone

Lithological and petrophysical characteristics oil-saturated deposits of Bobrikovsky horizon on the southern slope of the South-Tatarian arc

Korolev E., Nurgalieva N., Smelkov V., Eskin A., Kalcheva A.

, siltstones and sandstones. Sections are marked by regularity rise of sand layers thickness with increasing

Paleosols and host rocks from the Middle–Upper Permian reference section of the Kazan Volga region, Russia: A case study

Mouraviev F., Arefiev M., Silantiev V., Eskin A., Kropotova T.

Ravine (Kazan Volga region, Russia), contains two siltstone lithofacies: (a) laminated and (b) massive

The late miocene pelitic siltstone of the ishim formation (Southwestern Siberia): Mineralogical and geochemical characterization and prospects for further use

The late miocene pelitic siltstone of the ishim formation (Southwestern Siberia): Mineralogical

Middle Cambrian to Lower Ordovician faunas from the Chingiz Mountain Range, central Kazakhstan

Tolmacheva T.Ju.

of siltstones, sandstones and volcaniclastic rocks with rare beds of micritic carbonates, black shales

Lithological and petrophysical characteristics oil-saturated deposits of Bobrikovsky horizon on the southern slope of the South-Tatarian arc

Korolev E., Nurgalieva N., Smelkov V., Eskin A., Kalcheva A.

, siltstones and sandstones. Sections are marked by regularity rise of sand layers thickness with increasing

Microbial involvement in carbon transformation via ch4 and co2 in saline sedimentary pool

Goraj W., Szafranek-Nakonieczna A., Grzadziel J., Polakowski C., Słowakiewicz M., Zheng Y., Gałazka A., Stępniewska Z., Pytlak A.

(clayey salt with veins of fibrous salt and lenses of gypsum and anhydrite; siltstone and sandstone

Geoheritage Resource of a Small Town: Evidence from Southwestern Russia

Ruban D.A., Mikhailenko A.V., Zorina S.O., Yashalova N.N.

red (iron rich) siltstones, dolomitic siltstones and dolomitic marlstones. They accumulated in sabkha

Euxinia as a dominant process during OAE1a (Early Aptian) on the Eastern Russian Platform and during OAE1b (Early Albian) in the Middle Caspian

Zorina S., Pavlova O., Galiullin B., Morozov V., Eskin A.

in the bituminous siltstones and in the host siltstones of OAE1a on the Eastern Russian Platform, as well as a high

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