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Maracaibo

This method of analysis has again betin i,f much service, and in the expeiiencc nf this laboratory, has been snfhciently reliable for deciding coniiDercially the purityofall balsams except that from Central America (Maracaibo), which variety, as pointed out a year ago, is at times subject... [Pg.478]

Lake Maracaibo, Venezuela, Offshore Platform, UVCE/Fire... [Pg.80]

El Tablazo, Lake Maracaibo, Venezuela, Chemical Plant Explosion/Fire Fuel leak during truck transfer operations caused storage vessels to BLEVE... [Pg.81]

Of the North American total, about 1,100,000 barrels per day came from Texas, 420,000 from California, 170,000 from Mexico, and the remainder largely from Arkansas, Mississippi, and New Mexico. The sulfurous Venezuelan crudes come from the Lake Maracaibo area and these, like the Mexican crudes, give relatively low yields of naphtha and middle distillates, thus differing from the Middle East crudes. Only small amounts of crude oil with sulfur contents greater than 1% by weight exist in U.S.S.R., Europe, and the Far East. [Pg.153]

Departamento de Quimica Facultad de Ciencias La Universidad del Zulia Maracaibo, Venezuela... [Pg.181]

Carlos De La Cruz, Departamento de Quimica, Facultad de Ciencias, La Universidad del Zulia, Maracaibo, Venezuela (181)... [Pg.530]

Gardner, W. S., J. F. Cavaletto, H. A. Bootsma, P. J. Lavrentyev, and F. Troncone. 1998. Nitrogen cycling rates and light effects in tropical Lake Maracaibo, Venezuela. Limnology and Oceanography 43 1814-1825. [Pg.260]

The Bolivar Coastal Fields (BCF) of eastern Lake Maracaibo, Venezuela, contain five classes of oil as reflected by their API gravities, C15+ saturates-and-aromatics contents as well as their total nitrogen, sulfur, and oxygen (NSO) compositions. Biodegradation appears to have had a major role in controlling the... [Pg.592]

More recent evidence suggests a role in intracellular vesicular trafficking (Caviston and Holzbaur, 2009). HD is the most common of the (CAG)n/Qn-expansion diseases, despite the fact that new expansion mutational expansions in the Htt gene are believed to be exceedingly rare. The incidence of HD worldwide is about 5-10 per 100,000 individuals. Japan has a very low rate (0.1-0.5 per 100,000), whereas in the Lake Maracaibo region of Venezuela the incidence exceeds 100 per... [Pg.331]

Maracaibo Lake water, pH = 7.72 Concentrate of Satiha River fulvic acids... [Pg.515]

Davis C., Pratt L. M., Sliter W. V., Mompart L., and Murat B. (1999) Eactors influencing organic carbon and trace metal accumulation in the Upper Cretaceous La Luna Eormation of the western Maracaibo Basin, Venezuela. In Evolution of the Cretaceous Ocean-Climate System. Geological Society of America Special Paper 332 (eds. E. Barrera and C. Johnson). Geological Society of America, Boulder, pp. 203 -230. [Pg.3614]

Talukdar S., Gallango O., Vallejos C., and Ruggiero A. (1987) Observations on the primary migration of oil in the La Luna source rocks of the Maracaibo Basin, Venezuela. In Migration of Hydrocarbons in Sedimentary Basins (ed. B. Doligez). Editions Technip, Paris, France, pp. 59-78. [Pg.3653]

Alvarado, D. A. Marsden, S. S. In Proceedings of the 2nd International Symposium on Heavy Crude Oils and Tar Sands Maracaibo, Venezuela, 1987, paper no. 275. [Pg.261]

Figure 1. Vertical distribution of principal vegetation belts in the cordillera de Merida, a tropical high range in the northern Andes of Venezuela. The selected transect extends 120 km in the northerly direction across two parallel ranges of different elevation. Vegetation bands appear slanted towards the outer flanks because of greater moisture levels carried by easterly trade winds from the Orinoco basin and northeasterly winds from the Caribbean Sea and the Maracaibo lake basin to the north. Figure 1. Vertical distribution of principal vegetation belts in the cordillera de Merida, a tropical high range in the northern Andes of Venezuela. The selected transect extends 120 km in the northerly direction across two parallel ranges of different elevation. Vegetation bands appear slanted towards the outer flanks because of greater moisture levels carried by easterly trade winds from the Orinoco basin and northeasterly winds from the Caribbean Sea and the Maracaibo lake basin to the north.
Centro de Superficies y Catalisis, Facultad de Ingenieria, Universidad del Zulia, Apartado 15251, Maracaibo 4003A, Venezuela... [Pg.737]

Copaiba. Belsam copaiba balsam capivi Jesuit s balsam. Oleoresin from South American species of Copai-jm (Copaiba). Leguminosac. Habit. Brazil] Venezuela, Colombia, especially the Amazon valley and banks of Orinoco. Constit. Volatile oil. resin illuric and metacopaivic Kid (in Maracaibo balsam) copai vie and oxycopaivic acids (in Para balsam). Brief description of balsam copaiba and its constituents J. A. Wenninger et at-, J- Assoc. Offic. Anal. Ch m. 50, 1304 (1967) D. L, J. Opdyke Food Cosmer. Taxied, 4, 687 (1976) of copaiba oil idem, ibid, 11 1075... [Pg.393]

Oil nf Cepaiba. Volatile oil from copaiba balsam, usually Maracaibo. Constit. Chiefly caryophyllene and cedinene. [Pg.1074]

Sweeney, J. J., Braun, R. L., Burnham, A. K., Taluk-dar, S. Vallejos, C. 1995. Chemical kinetic model of hydrocarbon generation, expulsion and destruction applied to the Maracaibo Basin, Venezuela. American Association of Petroleum Geologists Bulletin, 79(10), 1515-1532. [Pg.173]

O. de Rincon, Statistical analysis of the diffusion coefficients measured in the piles of Maracaibo s bridge ,... [Pg.107]

During the period after World War 11 to the late 1960s, the field of marine geotechnology rapidly developed. These developments involved the following areas (1) shear strength measurements, (2) submarine slope stability, (3) Lake Maracaibo, (4) the Mississippi Delta,... [Pg.6]


See other pages where Maracaibo is mentioned: [Pg.179]    [Pg.82]    [Pg.335]    [Pg.195]    [Pg.131]    [Pg.390]    [Pg.390]    [Pg.265]    [Pg.2949]    [Pg.116]    [Pg.240]    [Pg.506]    [Pg.693]    [Pg.628]    [Pg.168]    [Pg.7]    [Pg.7]    [Pg.11]    [Pg.25]   


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