Element concentrations and isotopic composition of tholeiite and whole rocks samples from the east Mariana Basin

Studies of seafloor magnetic anomaly patterns suggest the presence of Jurassic oceanic crust in a large area in the western Pacific that includes the East Mariana, Nauru and Pigafetta Basins. Sampling of the igneous crust in this area by the Deep Sea Drilling Program (DSDP) and the Ocean Drilling Program (ODP) allows direct evaluation of the age and petrogenesis of this crust. ODP Leg 129 drilled a 51 m sequence of basalt pillows and massive flows in the central East Mariana Basin. 40Ar/39Ar ages determined in this study for two Leg 129 basalts average 114.6 +/- 3.2 Ma. This age is in agreement with the Albian-late Aptian paleontologic age of the overlying sediments, but is distinctively younger than the Jurassic age predicted by magnetic anomaly patterns in the basin. Compositionally, the East Mariana Basin basalts are uniformly low-K tholeiites that are depleted in highly incompatible elements compared to moderately incompatible ones, which is typical of mid-ocean ridge basalts (MORB) erupted near hotspots. The Sr, Nd and Pb isotopic compositions of the tholeiites (87Sr/86Sr init = 0.70360-0.70374; 143Nd/144Nd init = 0.512769-0.512790; 206Pb/204Pb meas = 18.355-18.386) also overlap with some Indian Ocean Ridge MORB, although they are distinct from the isotopic compositions of Jurassic basalts drilled in the Pigafetta Basin, the oldest Pacific MORB. The isotopic compositions of the East Mariana Basin tholeiites are also similar to those of intraplate basalts, and in particular, to the isotopic signature of basalts from the nearby Ontong Java and Manihiki Plateaus. The East Mariana Basin tholeiites also share many petrologic and isotopic characteristics with the oceanic basement drilled in the Nauru Basin at DSDP Site 462. In addition, the new 110.8 +/- 1.0 Ma 40Ar/39Ar age for two flows from the bottom of Site 462 in the Nauru Basin is indistinguishable from the age of the East Mariana Basin flows. Thus, while magnetic anomaly patterns predict that the igneous basement in the Nauru and East Mariana Basins is Jurassic in age, the geochemical and chronological results discussed here suggest that the basement formed during a Cretaceous rifting event within the Jurassic crust. This magmatic and tectonic event was created by the widespread volcanism responsible for the genesis of the large oceanic plateaus of the western Pacific.

La piedad divina. Desde el paganismo hasta el Cristianismo

El concepto de misericordia divina ha pasado por diversos estadios en su evolución, pero las concepciones de la religión cristiana y de la religión pagana no siempre se oponen. En este artículo se examinan las fuentes filosóficas (Aristóteles, filosofía helenística), literarias (Sófocles, Homero) y epigráficas, hallándose significados variados, a veces superpuestos temporalmente, y también el uso del concepto en las plegarias paganas y en las peticiones oficiales. Si bien el racionalismo estoico considera a la misericordia como incompatible con la sabiduría y la justicia, el cristiano Lactancio recupera el valor de las pasiones utilizadas apropiadamente, marcando un hito en la conversión de una emoción pagana en una virtud y un deber cristianos

Mineralogy and geochemistry of ODP Hole 176-735B minerals

We present a synthesis of some 20,504 mineral analyses of ~500 Hole 735B gabbros, including 10,236 new analyses conducted for this paper. These are used to construct a mineral stratigraphy for 1.5-km-deep Hole 735B, the only long section of the lower crust drilled in situ in the oceans. At long wavelengths, generally >200 m, there is a good chemical correlation among the principal silicate phases, consistent with the in situ crystallization of three or four distinct olivine gabbro bodies, representing at least two major cycles of intrusion. Initial cooling and crystallization of these bodies must have been fairly rapid to form a crystal mush, followed by subsequent compaction and migration of late iron-titanium-rich liquids into shear zones and fractures through which they were emplaced to higher levels in the lower crust where they crystallized and reacted with the olivine gabbro host rock to form a wide variety of ferrogabbros. At the wave lengths of the individual intrusions, as represented by the several olivine gabbro sequences, there is a general upward trend of iron and sodium enrichment but a poor correlation between the compositions of the major silicate phases. This, together with a wide range in minor incompatible and compatible element concentrations in olivine and pyroxene at a given Mg#, is consistent with widespread permeable flow of late melt through these intrusions, in contrast to what has been documented for a 600-m section of reputedly fast-spreading ocean crust in the Oman Ophiolite. This unexpected finding could be related to enhanced compaction and deformation-controlled late-stage melt migration at the scale of intrusion at a slow-spreading ocean ridge, compared to the relatively static environment in the lower crust at fast-spreading ridges.

Petrology and geochemistry of basalts from the Vavilov Basin

During ODP Leg 107, two holes were drilled in the basement of Vavilov Basin, a central oceanic area of the Tyrrhenian sea. Hole 655B is located near the Gortani ridge in off-axis position at the western rim of the basin; Hole 651A is located on a basement swell at the axis of the basin. This paper deals with mineral chemistry, major and trace element geochemistry, and petrogenesis of the basalts recovered in the two holes. The mineralogy of the basalts is broadly homogeneous, but all of them have suffered important seawater alteration. Their major-element compositions are similar to both normal-mid-ocean-ridge-basalts (N-MORB) and back-arc-basalts (BAB) except for Na2O contents (BAB-like), and K2O which is somewhat enriched in upper unit of Hole 651 A. Their affinity with N-MORB and BAB is confirmed by using immobile trace elements such as Zr, Y, and Nb. However, basalts from the two sites present contrasting geochemical characteristics on spidergrams using incompatible elements. Hole 655B basalts are homogeneous enriched tholeiites, similar to those from DSDP Hole 373 (located on the opposite side of the basin near the eastern rim), and show affinities with enriched MORB (E-MORB). At Hole 651 A, the two basalt units are chemically distinct. One sample recovered in lower unit is rather similar to those from Hole 655B, but basalts from upper unit display calc-alkaline characteristic evidenced by the increase of light-ion-lithophile-element (LILE)/high-field-strength-element (HFSE) ratio, and appearance of a negative Nb-anomaly, making them comparable with orogenic lavas from the adjacent Eolian arc. The observed chemical compositions of the basalts are consistent with a derivation of the magmas from a N-MORB type source progressively contaminated by LILE-enriched fluids released from dehydration of the bordering subducted plate. Implications for evolution of the Tyrrhenian basin are tentatively proposed taking into consideration geochemical and chronological relationships between basalts from Leg 107 Holes 655B and 651 A, together with data from Leg 42 Site 373 and Vavilov Seamount. These data illustrate back-arc spreading in ensialic basin closely associated with the maturation of the adjacent subduction, followed by the growth of late off-axis central volcano, whereas the active subduction retreats southeastward.

Memorias en conflicto : Dialécticas de la violencia política en la novela vasca actual

Este trabajo pretende abordar algunas de las particularidades de las representaciones de la violencia política en la novela actual en lengua vasca. A partir de la constatación de que en la sociedad vasca, como en toda sociedad, existe un conflicto entre memorias de violencias de distinto signo, el artículo pretende ilustrar cómo se han articulado cuestionestales como las categorías de víctima y victimario, cuya distinción no es siempre nítida, o los orígenes de la violencia política en dos novelas vascas actuales: Soinujolearen semea (El hijo del acordeonista) de Bernardo Atxaga y Antzararen bidea (El camino de la oca) de Jokin Muñoz. El autor sostiene que estas novelas plantean dos modos distintos, aunque no incompatibles, de ficcionalización de la violencia y el deber de memoria

Chemical and isotopic compositions of rocks and minerals from the Franz Josef Land Archipelago

Rb, Sr, Sm, Nd, U, and Pb contents and Sr, Nd, and Pb isotopic composition were determined in tholeiite and subalkaline basalts (in both whole-rock samples and individual minerals) from the Franz Josef Land Archipelago. Isotopic data obtained for the Arctic basin are similar to those for islands from the Pacific, Atlantic, and Indian oceans. The assimilation of crustal (sedimentary) rocks by primary depleted material makes isochron determination of basalt age difficult or impossible. The subalkaline basalts (basaltic andesites) were presumably formed by the metasomatic introduction of incompatible elements in tholeiitie basalts and, only partially, through crustal contamination and fractional crystallization.

La planificación estática-la planificación dinámica : Ausencia de planes de ordenamiento territorial municipal

Mucho ofthe towns of Mendoza have been working for years with a methodology built with traditional zoningand code of permitted uses,not permitted or conditional. With these instrument sexpectthe presentation of private enter prisesto assess whether it complies with these regulationsto authorize the works.These agencies have a plan with zoning and code application shave already considered planning. This form of work, shows clearly the lack of actions to drive urban developmentsin the department, initiatives on the issue only limited to astatic situation, waiting for proposal sand external actions,not being able to see the advantagesand /or contribution saccom panying the Land Use Plan. Une of the important elements to considerin the Plan process, is the incorporation of participatory stage allows, consensus and guidanceto policy makers, community in territorial actions. For this way are designed and constructed public works, to address concerns of the population and in some cases,works that will produce community supportat election time. A look at the performance of Cities hall suchas Granada City Council, Churriana de la Vega and Jun, you can observe that the planning can be done other wise, as articulated action from the same organism. In principle determining zoning and uses of spaceis integral to the Land Use Planand that it further comprises the development proposals,the lines of action and prioritization of programs and projects. These local governants, which manage a municipality, working withdy namic planning councilasit implements the proposed urban development, agricultural, commercial and industrialin its territory and build public work saccording to plan. Since 2009,the province has a Law of Zoningand Land Use demanded Municipal Land Management Plans, but three years after the enactmentof the 18 only has aplan.Thisis due to two reasons:the policy makersdo not understand the multiplicity of elements and facets of a plan covering the other,the plans are perceived as a limitation on their actions , a fact not willing to accept. The dissemination of know ledge and the, new ways toaddress the Land Use Planning and management of conflicts generated by the unprecedented growthwith incompatible usesin these cities that the component swhich will requirel and manager stoimplement aplanning Plans. Tusa dinámica risión Fromm te municipalitos in thais contexto de can tal abur innovación and a newway of governing

Chemical composition of Ninetyeast Ridge basalts

On Leg 121 of the Ocean Drilling Program, we recovered basaltic rocks from a total of three basement sites in the southern, central, and northern regions of Ninetyeast Ridge. These new sites complement the previous four basement holes drilled during Legs 22 and 26 of the Deep Sea Drilling Project, and confirm the predominantly tholeiitic, light rare earth element-enriched character of the basalts that cap the ridge. The basalts show marked iron enrichment; ferrobasalts occur at Sites 214 and 216 and oceanic andesites at Site 253. All of the basalts recovered during Leg 121 are altered, and range from aphyric olivine tholeiites (Site 756), to strongly plagioclase-phyric basalts (Site 757). Basalts from Site 758, which were clearly erupted in a submarine environment (pillow basalts are present in the section), are sparsely to strongly plagioclase-phyric. The basalts recovered at any one hole are isotopically homogeneous (except for the basalts from Site 758, which show a range of Pb isotopes), and it is possible to relate the magmas at any one site by high-level fractionation processes. However, there are significant variations in isotope ratios and highly incompatible element ratios between sites, which suggest that the mantle source for the ridge basalts was compositionally variable. Such variation, in view of the large volume of magmatic products that form the ridge system, is not surprising. There is not, however, a systematic variation in basalt composition along the ridge. We agree with previous models that relate Ninetyeast Ridge to a mantle plume in the southern Indian Ocean. The tholeiitic, iron-enriched, and voluminous character of the ridge basalts is typical of oceanic islands associated with plumes on or near a mid-ocean ridge (e.g., Iceland, Galapagos Islands, and St. Paul/Amsterdam islands). The absence of recovered alkalic suites is inconsistent with an intraplate setting, such as the Hawaiian Islands or Kerguelen Island. Thus, the major element data, like the gravity data, strongly suggest that the ridge was erupted on or very close to an active spreading center. Isotopically, the most likely plume that created the excess magmatism on the Ridge is the Kerguelen-Heard plume system, but the Ninetyeast Ridge basalts do not represent a simple mixing of the Kerguelen plume and mid-ocean Ninetyeast Ridge basalt mantle.

Chemical and isotopic composition of rocks and minerals at ODP Site 209-1275

This paper reports results of an investigation of a representative collection of samples recovered by deep-sea drilling from the oceanic basement 10 miles west of the rift valley axis in the crest zone of the Mid- Atlantic Ridge at 15°44'N (Sites 1275B and 1275D). Drilling operations were carried out during Leg 209 of the Drilling Vessel JOIDES Resolution within the framework of the Ocean Drilling Program (ODP). The oceanic crust was penetrated to depth of 108.7 m at Site 1275B and 209 m at Site 1275D. We reconstructed the following sequence of magmatic and metamorphic events resulting in the formation of a typical oceanic core complex of slow-spreading ridges: (1) formation of strongly fractionated (enriched in iron and titanium) tholeiitic magmatic melt parental to gabbroids under investigation in a large magma chamber located in a shallow mantle and operating for a long time under steady-state conditions; (2) transfer of the parental magmatic melt of the gabbroids to the base of the oceanic crust, its interaction with host mantle peridotites, and formation of troctolites and plagioclase peridotites; (3) intrusion of enriched trondhjemite melts as veins and dikes in the early formed plutonic complex, contact recrystallization of the gabbro, and development in the peridotite-gabbro complex of enriched geochemical signatures owing to influence of trondhjemite injections; (4) emplacement of dolerite dikes (transformed to diabases); (5) metamorphism of upper epidoteamphibolite facies with participation of marine fluids; and (6) rapid exhumation of the plutonic complex to the seafloor accompanied by greenschist-facies metamorphism. Distribution patterns of Sr and Nd isotopes and strongly incompatible elements in the rocks suggest contributions from two melt sources to the magmatic evolution of the MAR crest at 15°44'N: a depleted reservoir responsible for formation of the gabbros and diabases and an enriched reservoir, from which trondhjemites (granophyres) were derived.

Hacia un principio de complementariedad en lingüística : Análisis del status epistemológico de la teoría generativa y de la teoría sistémico-funcional a partir de la dualidad 'facultad de la mente'-'producto de la cultura'

La teoría generativa y la teoría sistémico-funcional pueden concebirse como teorías científicas: Han confirmado hipótesis, proveen explicaciones y, a partir de estas últimas, efectúan predicciones. Sin embargo, ambas teorías manejan supuestos incompatibles sobre el mismo objeto: el lenguaje. Después de analizar el problema de las confirmaciones y las explicaciones en lingüística, se intentará demostrar que esa incompatibilidad puede resolverse mediante un "principio de complementariedad": El lenguaje es, al mismo tiempo, una "facultad de la mente" y un "producto de la cultura", aunque los dos aspectos (el "mental" y el "cultural") no puedan captarse en el ámbito de una sola teoría.

La piedad divina. Desde el paganismo hasta el Cristianismo

El concepto de misericordia divina ha pasado por diversos estadios en su evolución, pero las concepciones de la religión cristiana y de la religión pagana no siempre se oponen. En este artículo se examinan las fuentes filosóficas (Aristóteles, filosofía helenística), literarias (Sófocles, Homero) y epigráficas, hallándose significados variados, a veces superpuestos temporalmente, y también el uso del concepto en las plegarias paganas y en las peticiones oficiales. Si bien el racionalismo estoico considera a la misericordia como incompatible con la sabiduría y la justicia, el cristiano Lactancio recupera el valor de las pasiones utilizadas apropiadamente, marcando un hito en la conversión de una emoción pagana en una virtud y un deber cristianos

La planificación estática-la planificación dinámica : Ausencia de planes de ordenamiento territorial municipal

Mucho ofthe towns of Mendoza have been working for years with a methodology built with traditional zoningand code of permitted uses,not permitted or conditional. With these instrument sexpectthe presentation of private enter prisesto assess whether it complies with these regulationsto authorize the works.These agencies have a plan with zoning and code application shave already considered planning. This form of work, shows clearly the lack of actions to drive urban developmentsin the department, initiatives on the issue only limited to astatic situation, waiting for proposal sand external actions,not being able to see the advantagesand /or contribution saccom panying the Land Use Plan. Une of the important elements to considerin the Plan process, is the incorporation of participatory stage allows, consensus and guidanceto policy makers, community in territorial actions. For this way are designed and constructed public works, to address concerns of the population and in some cases,works that will produce community supportat election time. A look at the performance of Cities hall suchas Granada City Council, Churriana de la Vega and Jun, you can observe that the planning can be done other wise, as articulated action from the same organism. In principle determining zoning and uses of spaceis integral to the Land Use Planand that it further comprises the development proposals,the lines of action and prioritization of programs and projects. These local governants, which manage a municipality, working withdy namic planning councilasit implements the proposed urban development, agricultural, commercial and industrialin its territory and build public work saccording to plan. Since 2009,the province has a Law of Zoningand Land Use demanded Municipal Land Management Plans, but three years after the enactmentof the 18 only has aplan.Thisis due to two reasons:the policy makersdo not understand the multiplicity of elements and facets of a plan covering the other,the plans are perceived as a limitation on their actions , a fact not willing to accept. The dissemination of know ledge and the, new ways toaddress the Land Use Planning and management of conflicts generated by the unprecedented growthwith incompatible usesin these cities that the component swhich will requirel and manager stoimplement aplanning Plans. Tusa dinámica risión Fromm te municipalitos in thais contexto de can tal abur innovación and a newway of governing

Memorias en conflicto : Dialécticas de la violencia política en la novela vasca actual

Este trabajo pretende abordar algunas de las particularidades de las representaciones de la violencia política en la novela actual en lengua vasca. A partir de la constatación de que en la sociedad vasca, como en toda sociedad, existe un conflicto entre memorias de violencias de distinto signo, el artículo pretende ilustrar cómo se han articulado cuestionestales como las categorías de víctima y victimario, cuya distinción no es siempre nítida, o los orígenes de la violencia política en dos novelas vascas actuales: Soinujolearen semea (El hijo del acordeonista) de Bernardo Atxaga y Antzararen bidea (El camino de la oca) de Jokin Muñoz. El autor sostiene que estas novelas plantean dos modos distintos, aunque no incompatibles, de ficcionalización de la violencia y el deber de memoria

Platinum group elements and geochemistry of altered oceanic crust of ODP Hole 140-504B

Primary chemical heterogeneity in the sheeted dike complex in Deep Sea Drilling Project Hole 504B makes these rocks unsuitable for conventional mass balance calculations in determining element mobility associated with hydrothermal alteration. Due to the original heterogeneity and variable degrees of fractionation in the dikes, an appropriate reference sample on which calculations can be based is difficult to find. Therefore, the use of incompatible element ratios is developed to evaluate geochemical changes during alteration(s). For example, on a Zr/Yb-La/Yb plot, scatter along a straight line suggests tapping of a variably depleted mantle source and deviation from the line suggests element mobility (gain or loss). Using this method, our data indicates that the hydrothermal evolution of the sheeted dike complex was accompanied by significant loss of Cu, Zn, and Ti and some loss of La. The sheeted dike complex has low platinum group element (PGE) concentrations and steep PGE patterns, typical of mid-ocean ridge basalts (MORBs) on the global scale. We propose that the unusual PGE patterns of MORBs cannot be entirely generated by a partial melting and sulfide segregation model; instead, these patterns in part must have been inherited from their mantle source. The Au data show no evidence for mobilization during hydrothermal alteration of the dikes.

Composition of minerals from peridotides at the Mid-Atlantic Ridge, 13°N

Peridotites (diopside-bearing harzburgites) found at 13°N of the Mid-Atlantic Ridge fall into two compositional groups. Peridotites P1 are plagioclase-free rocks with minerals of uniform composition and Ca-pyroxene strongly depleted in highly incompatible elements. Peridotites P2 bear evidence of interaction with basic melt: mafic veinlets; wide variations in mineral composition; enrichment of minerals in highly incompatible elements (Na, Zr, and LREE); enrichment of minerals in moderately incompatible elements (Ti, Y, and HREE) from P1 level to abundances 4-10 times higher toward the contacts with mafic aggregates; and exotic mineral assemblages Cr-spinel + rutile and Cr-spinel + ilmenite in peridotite and pentlandite + rutile in mafic veinlets. Anomalous incompatible-element enrichment of minerals from peridotites P2 occurred at the spinel-plagioclase facies boundary, which corresponds to pressure of about 0.8-0.9 GPa. Temperature and oxygen fugacity were estimated from spinel-orthopyroxene-olivine equilibria. Peridotites P1 with uniform mineral composition record temperature of the last complete recrystallization at 940-1050°C and FMQ buffer oxygen fugacity within the calculation error. In peridotites P2, local assemblages have different compositions of coexisting minerals, which reflects repeated partial recrystallization during heating to magmatic temperatures (above 1200°C) and subsequent reequilibration at temperatures decreasing to 910°C and oxygen fugacity significantly higher than FMQ buffer (delta log fO2 = 1.3-1.9). Mafic veins are considered to be a crystallization product from basic melt enriched in Mg and Ni via interaction with peridotite. The geochemical type of melt reconstructed by the equilibrium with Ca-pyroxene is defined as T-MORB: (La/Sm)_N~1.6 and (Ce/Yb) )_N~2.3 that is well consistent with compositional variations of modern basaltic lavas in this segment of the Mid-Atlantic Ridge, including new data on quenched basaltic glasses.