Titlebook: Hypersaline Ecosystems; The Gavish Sabkha Gerald M. Friedman,Wolfgang E. Krumbein Book 1985 Springer-Verlag Berlin Heidelberg 1985 Sediment

hermitage

玷污

杠桿支點

licence

Coastal Evaporite Systemse coastal sabkhas of the Arabo-Persian Gulf, demonstrating that evaporite formation was not limited to subaquatic environments. These initial studies of Wells (1962) and colleagues of Shell Research (The Netherlands) and of Shearman (1963) and other researchers of Imperial College (London) have been

受辱

Hypersaline Sea-marginal Flats of the Gulfs of Elat and Suezforming ocean. The climatic conditions that prevail enable considerable quantities of carbonates and evaporites to form and the active tectonism results in the unusual juxtaposition of abundant terrigenous elastics. We studied the characteristics and distribution of the various sea-marginal environm

猛擊

Infusion

Geomorphology, Mineralogy and Groundwater Geochemistry as Factors of the Hydrodynamic System of the s in mineralogy and brine geochemistry in the uniquely restricted marine system of the sabkha south of Nabq, called the Gavish Sabkha. Also, we give a more specific geological and geochemical description of this particular sabkha than has been described previously (Gavish 1980, Gavish et al. 1978, K

Diverticulitis

Melatonin

Salinity and Water Activity Related Zonation of Microbial Communities and Potential Stromatolites ofanently ice-covered lakes in the Antarctic (Bauld 1981 a, b, Borowitzka 1981, Brock 1978, Castenholz 1973, Y. Cohen et al. 1977 b, c, Horodyski 1977 a, Javor 1979, Krumbein et al. 1977, Krumbein and Lange-Giele 1979, Parker et al. 1981, Wright and Burton 1981).