Big Chemical Encyclopedia

Chemical substances, components, reactions, process design ...

Articles Figures Tables About

Bituminous rock

Asphalt (Natural) A natural mineral pitch, tar or bitumen composed principally of hydrocarbons a natural bituminous rock that is dark colored, comparatively hard and nonvolatile. Does not include asphalt, bitumen, tar or other substances, derived from petroleum processing. [Pg.12]

Dead Sea area (Jordan Valley Rift)—kerogens, bitumens, immature asphalts and bituminous rocks (Senonian Formation, Israel)... [Pg.27]

Pyrite in the bituminous rocks appears as both framboids and single crystals (<50 /rm) that are undetected by X-ray diffraction analysis because they are coated with OM (Spiro, 1980 Spiro et al, 1983a,b). Very small amounts of humic matter occur in these samples, but more than 95% of the OM in the bimminous rocks is high sulfur kerogen (8-10% w/w). The richest samples in both TOC and organically bonded sulfur occur in the Nabi Musa (Israel) area (S/C atomic ratio 0.05-0.065). Various maturity parameters indicate that all of the kerogens are immature with an H/C ratio of 1.3-1.6. [Pg.27]

Spiro B. (1980) Geochemistry and mineralogy of bituminous rocks in Israel. Ph.D. Thesis, The Hebrew University of Jerusalem (in Hebrew abstract in English). [Pg.32]

Spiro B., Welte D. H., Rullkoeter J. and Schaefer R. G. (1983b) Asphalts, oils and bituminous rocks from the Dead Sea area—a geochemical correlation study. Am. Assoc. Petrol. Geol. Bull. 67, 1163-1175. [Pg.33]

Senonian age Ghareb Formation, bituminous rocks, asphalts and oil shows Dead Sea Area Israel... [Pg.44]

Studies of organic matter in both bituminous rocks of the Ghareb Formation as well as asphalts and petroleum shows of the Northern Negev and the Dead Sea area in Israel have been previously published (Spiro et al, 1983a,b Tannenbaum, 1983 Tannenbaum et al, 1987 Almogy-Labin et al, 1993). The diagenesis of these sulfur-rich deposits is discussed in... [Pg.44]

Fig. 6. Kerogens, asphalts, biodegraded asphalts (oil) and oil shows of the Dead Sea area, Israel are plotted on versus maturation. See also Fig. 4 in Part I. We assume that the kerogens that are isolated from the Ghareb-Senonian age bituminous rocks (type II-S), represent the deeper, more mature members, which generated the asphalts and the oils. Scale of maturation is arbitrary. See also Table 1 in Part I. Fig. 6. Kerogens, asphalts, biodegraded asphalts (oil) and oil shows of the Dead Sea area, Israel are plotted on versus maturation. See also Fig. 4 in Part I. We assume that the kerogens that are isolated from the Ghareb-Senonian age bituminous rocks (type II-S), represent the deeper, more mature members, which generated the asphalts and the oils. Scale of maturation is arbitrary. See also Table 1 in Part I.
Bitumen (native asphalt) Bituminous rock Bituminous sand ... [Pg.42]

Petroleum Heavy oil Mineral wax Bitumen Asphaltite Asphaltoid Migrabitumen Bituminous rock Bituminous sand Kerogen Natural gas Coal... [Pg.538]

See other pages where Bituminous rock is mentioned: [Pg.359]    [Pg.324]    [Pg.420]    [Pg.66]    [Pg.368]    [Pg.359]    [Pg.35]    [Pg.15]    [Pg.27]    [Pg.36]    [Pg.39]    [Pg.44]    [Pg.50]   
See also in sourсe #XX -- [ Pg.368 ]



SEARCH



Bitumin

Bituminous

© 2024 chempedia.info