(Table 1) Isotopic and trace-element composition of ODP Leg 127/128 basalts

The western Pacific includes many volcanic island arc and backarc complexes, yet multi-isotopic studies of them are rare. Basement rocks of the Sea of Japan backarc basin were encountered at Sites 794,795, and 797, and consisted of basaltic sills and lava flows. These rocks exhibit a broad range in isotopic composition, broader than that seen in any other western Pacific arc or backarc system: 87Sr/86Sr = 0.70369 to 0.70499, 143Nd/144Nd = 0.51267 to 0.51317, 206Pb/204Pb = 17.64 to 18.36. The samples form highly correlated arrays between very depleted mid-ocean ridge basalt (MORB) and the Pacific pelagic sediment fields on Pb-Pb plots. Similarly, on plots of Sr-Pb and Nd-Pb, the Sea of Japan samples lie on mixing curves between depleted mantle and enriched mantle ("EM II"), which is interpreted to be of average crustal or pelagic sediment composition. The source of these backarc rocks appears to be a MORB-like mantle source, contaminated by pelagic sediments. Unlike the Mariana and Izu arc/backarc systems, Japanese arc and backarc rocks are indistinguishable from each other in a Sr-Nd isotope plot, and have similar trends in Pb-Pb plots. Thus, sediment contamination of the mantle wedge appears to control the isotopic compositions of both the arc and backarc magmas. Two-component mixing calculations suggest that the percentage of sediments in the magma source varies from 0.5% to 2.5%.

Chemistry of minerals from ODP Leg 127/128 basalts

Suites of basalts drilled during Legs 127 and 128 can be distinguished by their mineral assemblages and compositions of phenocrysts and groundmass phases. An upper suite of plagioclase phyric basaltic sills with a groundmass composed of plagioclase, augite, and magnetite was recovered from Site 794. The upper, evolved part of this suite is highly plagioclase phyric, including calcic plagioclases (~An90). The most primitive, lower part of this upper suite, in addition, contains olivine, but lacks calcic plagioclase. A lower suite at Site 794 is plagioclase and olivine phyric to aphyric basaltic sills and flows with a groundmass of plagioclase, augite, olivine (~Fo75-83), and magnetite. At Site 795, plagioclase and augite phyric basalts and andesites were recovered. The relatively low Ti and Cr contents of augite of these basalts suggest typical arc tholeiitic parental magmas. Two suites of basalt were recovered from Site 797, an upper suite of plagioclase and olivine phyric to aphyric olivine basalts, and a lower suite of evolved plagioclase phyric basaltic sills. The most evolved sills at both sites lack olivine as phenocryst and groundmass phases, while this phase is present in the relatively primitive sills. The olivine-bearing suites contain plagioclase with relatively low potassium content and augite with relatively high sodium content. An exception is the olivine-bearing sills of the upper suite at Site 794 that contains plagioclase with relatively high potassium content similar to the associated olivine-free sills. The olivine-free suites contain plagioclase with high potassium content and augite with low sodium content and have the most evolved compositions of any of the Japan Sea rocks.

Manuel Claro: Para un análisis ideológico del periodismo. 127 p. Editorial Precursora, Buenos Aires, 1983.

Fil: Pró, Diego F..

Incidencia del agua consumida en la zona de influencia del centro de salud nº 127 El Cortaderal, como determinante de prevalencia de hipertensión arterial en sus habitantes, Malargüe, 2011

La EPA (Environmental Protection Agency) ha establecido estándares de seguridad para más de 80 contaminantes que pueden encontrarse en el agua potable y presentan un riesgo a la salud humana. Los efectos agudos ocurren dentro de unas horas o días posteriores al momento en que la persona consume un contaminante. Casi todos los contaminantes pueden tener un efecto agudo si se consume en niveles extraordinariamente altos en el agua potable, en esos casos los contaminantes más probables que causen efectos agudos son las bacterias y virus. Los contaminantes en el agua potable que pueden causar efectos crónicos son los químicos (tales como solventes y plaguicidas), radionucléidos (tal como el radio) y minerales (tal como el arsénico y algunas sales). Entre los ejemplos de efectos crónicos de los contaminantes del agua potable, están el cáncer, problemas del hígado o riñones o dificultades en la reproducción. Este estudio persigue los siguientes objetivos: -Determinar si las características del agua de consumo de El Manzano son determinante de la alta prevalencia de HTA entre sus habitantes -Conocer las características físicas de la composición del agua de consumo del Paraje El Cortaderal. -Comparar la calidad del agua de consumo de las localidades de El Cortaderal y El Manzano. -Comparar si los hábitos alimenticios de los parajes estudiados presentan diferencias significativas que pudieran incidir en la aparición de las Patologías como la HTA y la Fluorosis