Palaeogeography, Palaeoclimatology, Palaeoecology
Coal and oil shale of Early Carboniferous age in northern Canada: significance for paleoenvironmental and paleoclimatic interpretations
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Relative combustion efficiency of composite fuels based on of wood processing and oil production wastes
2019, EnergyCitation Excerpt :There is virtually no coal mining in this region, but oil production and forestry are well developed. It should be noted that such distribution is typical of other countries as well (for example, some regions of Norway, China, Canada, and the USA) [40–45]. Coal and combustible coal processing waste can only be imported from neighboring regions.
Maastrichtian oil shale deposition on the southern Tethys margin, Egypt: Insights into greenhouse climate and paleoceanography
2018, Palaeogeography, Palaeoclimatology, PalaeoecologyCitation Excerpt :Therefore, the source of high nutrient influxes was not external and other factors must have governed the surface productivity variation via nutrients concentration. Another possible explanation for nutrient-enriched water within the photic zone and high organic productivity is upwelling due to ocean circulation (Cameron et al., 1994; Perkins et al., 2008). During Late Cretaceous times, an intensive coastal upwelling system occurred, essentially controlled by the wind regime, along the continental shelf of Egypt, in the south-east Tethyan Ocean (Eladawy et al., 2017).
Depositional environment, sequence stratigraphy and sedimentary mineralization mechanism in the coal bed- and oil shale-bearing succession: A case from the Paleogene Huangxian Basin of China
2017, Journal of Petroleum Science and EngineeringCitation Excerpt :Coal beds and oil shale are two types of sedimentary rocks formed in different depositional environments. Peat swamps (coal bed) were present between water and dry land (Diessel, 1992), while oil shale was formed by the preservation and aggregation of algae in deep-water environments (Cameron et al., 1994). Coal–forming environments are various including fan, braided channels, meandering river, barrier-lagoon, tidal flat and delta plain and so on (Cadle et al., 1993; Caldera and Gibling, 1994; Banerjee et al., 1996; Greb and Weisenfluh, 1996; Holz, 1998; Valero et al., 1997; Diessel et al., 2000;Caldera and Gibling, 1994; Li et al., 2014).
The stratigraphic distribution of inertinite
2010, International Journal of Coal GeologyMongolian coal-bearing basins: Geological settings, coal characteristics, distribution, and resources
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