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[en] Investment opportunities with Yacimientos Petroliferos Fiscales Bolivianos (LPFB) in La Paz, Bolivia, were discussed, especially as they may be affected by the new Hydrocarbon Law No. 1689, whose main objective is to encourage investments in Bolivia and to increase production capacity through investors' incorporation. Some of the areas of potential importance examined included reserve development, transportation, upstream consulting, and hydrocarbon development
[en] With a strong global demand for some 30 years, natural gas is a particular challenge for countries of South and Central America since each cubic meter of natural gas that is consumed is produced in this continent. It therefore seems appropriate to consider the risk of a collision gas and its effects on the countries most dependent on gas (either as producers or as consumers). Thus, in this paper, we study the vulnerability of gas in several countries on four ratios developed by Cabalu (2010). Once calculated from empirical data, these ratios helped to determine indicators and to classify countries according to their vulnerability in the event of a gas shock (sudden rise in prices). A picture emerges which represents an indicative classification of the countries. - Highlights: ► In this paper, we study the vulnerability of gas with four indicators. ► We focus on eight countries in South America and Central. ► These indicators helped to classify countries according to their vulnerability. ► The least vulnerable country is Bolivia. ► The most vulnerable countries are Chile and Venezuela.
[en] Tertiary felsic volcanics of the Sierra Pena Blanca in Mexico host potentially economic uranium deposits, and of Meseta Los Frailes in Bolivia contain interesting U anomalies but no significant deposits. A comparative study of the two uranium districts reveals differences that may explain the different degrees of U concentration. The host ignimbrite in Mexico, namely the Nopal Formation dated at 44 Myr. ago, is potassic alkaline rhyolite which is poorly compacted and contains phenocrysts of quartz, orthoclase, ilmenite and magnetite, totalling < 15% of the rock. The 16-Myr. old host tuffs in Bolivia on the other hand, are rhyodacites of calc-alkaline character, and contain phenocrysts of plagioclase, biotite and accessory minerals, amounting to > 30% of the rock. Vapour phase crystallization is well developed in the Mexican tuff, and has led to a primary concentration of labile U not tied up in refractory accessory minerals, as shown by fission-track studies. The Bolivian tuffs lack such vapour phase primary concentration of U. Subsequent hydrothermal alteration, in particular kaolinization is intense in the Mexican district, but is relatively less intense in the Bolivian one. It is postulated that an intense hydrothermal activity, probably of prolonged duration, in rocks displaying primary enrichment of labile U, is essential to form volcanogenic U deposits of the type found in Mexico. 26 refs.; 13 figs.; 3 plates; 3 tabs