Geochemistry and petrogenesis of basalts from DSDP Leg 92 holes

Basalts recovered on DSDP Leg 92 include all the major basalt types so far recovered from the ocean crust of the eastern Pacific. Basalts from Holes 597, 597A, 597B, 597C, and 599B are tholeiites exhibiting all the mineralogical and geochemical characteristics of N-type mid-ocean ridge basalts (MORB). Fragments of ferrobasalts and alkali basalts were also obtained, however, from Holes 60IB and 602B, respectively. Hole 597C, which penetrated 91 m into basement and is the deepest hole so far drilled in fast-spreading crust, yielded basalts that can be divided into three major lithologic units. The lowest unit, Unit III, contains modal olivine and comprises basalts which, at about 8 to 10% MgO, are as basic as any sampled from fast-spreading crust. The middle unit, Unit II, is the most evolved; its basalts are olivine free and contain between 6 and 7.5% MgO. The upper unit, Unit I, is intermediate in composition between Units II and III; it is characterized by both modal olivine and glomerocrysts made up of plagioclase and rare olivine. Unit I is probably a massive flow, whereas Units II and III may be massive flows or sills. The basalts appear to have undergone three stages of alteration ("deuteric," "relatively reducing," and "oxidizing"), the intensity of alteration decreasing markedly downcore. Hole 597B, at 26.4 m of basement penetration the only other "deep" hole, contains just one lithologic unit, which closely resembles Unit I of Hole 597C. Petrogenetic modeling reveals that the three lithologic units in Hole 597C are cogenetic and that they were derived from a depleted mantle source similar to the source of the tholeiites and ferrobasalts sampled in other holes; the alkali basalts are the only rocks derived from enriched mantle. Lavas of Unit III probably lay on the olivine-plagioclase cotectic, whereas the other lavas lay on an olivine-plagioclase-clinopyroxene peritectic. Some 60% of closed-system crystallization is needed to generate the most-evolved from the last-fractionated tholeiite, and a further 50% crystallization (80% overall) is needed to generate the ferrobasalts. Xenocrysts of calcic plagioclase and pseudomorphosed olivine in tholeiites from Hole 597B and Unit I of Hole 597C, and in the ferrobasalts from Hole 601B, provide evidence, however, that some magma mixing may have taken place.

Effect of Size Reduction on Magnetic Ordering in Sm1-x Ca (x) MnO3 (x=0.35, 0.65 and 0.92) Manganites: Magnetic and EMR Studies

We have employed the highly sensitive electron magnetic resonance technique complimented by magnetization measurements to study the impact of size reduction on the magnetic ordering in nanosized Sm1-x Ca (x) MnO3 (x = 0.35, 0.65 and 0.92). In the bulk form, x = 0.35 sample shows a charge ordering transition at 235 K followed by a mixed magnetic phase, the sample with x = 0.65 exhibits charge order below 275 K and shows an antiferromagnetic insulator phase below 135 K while that with x = 0.92 has a ferromagnetic-cluster glass ground state. Thus, a comparative study of magnetic ground states of bulk and nanoparticles (diameter similar to 25 nm) enables us to investigate size-induced effects on different types of magnetic ordering. It is seen that in the bulk samples the temperature dependences of the EPR parameters are quite different from each other. This difference diminishes for the nanosamples where all the three samples show qualitatively similar behavior. The magnetization measurements corroborate this conclusion.

Estudio de observación de ciento doce líneas de arroz (Oryza sativa L.) VIOAL-92, bajo ecosistema de riego en la localidad de Malacatoya

Con el objetivo de evaluar 112 líneas de Arroz de porte semienano, procedentes en su mayoría de Colombia, Vivero IRRI (IIRON), Argentina, Cuba y Perú, y utilizando como testigos internacionales las variedades CICA-8 y ORYZICA-1 y como testigos locales las variedades ALTAM1RA-9, ALTAM1RA-10 y CICA-8 también considerada como testigo local, se llevó a cabo un estudio en la "Finca Venllano", ubicada en Malacatoya, municipio del departamento de Granada, bajo el agroecosistema de riego. A cada línea se le evalúo las características agronómicas (floración, altura, desgrane, senescencia, exerción, acame y aceptabilidad fenotípica) y los componentes del rendimiento ( long de panícula, número de granos por panícula, porcentaje de fertilidad, peso de 1000 granos, rendimiento y rendimiento industrial ( % de arroz integral, % de arroz pulido y % de arroz oro). Se seleccionaron 15 líneas por sus características agronómicas y su potencial de rendimiento, lo que da un 13% de selección del material evaluado. La línea de mejor rendimiento fue la 113 (ECIA 561 con 5980 Kg/ha y la de menor rendimiento fue la línea 30 (CT9508-48-1-1P-2PT) con 3195 Kg/ha. El material de mejor calidad industrial fue la línea 10 (CT8837-1-17-1P-4) con 58.5 % de Arroz Oro y la línea más baja fue la 41 (CT7B05-17-4A-M-4P) con 48.0 % de Arroz Oro.