Geochemistry at DSDP Leg 82 Holes

DSDP Leg 82 drilled nine sites to the southwest of the Azores Islands on the west flank of the Mid-Atlantic Ridge (MAR) in an attempt to determine the temporal and spatial evolution of the Azores "hot-spot" activity. The chemistry of the basalts recovered during Leg 82 is extremely varied: in Holes 558 and 561, both enriched (E-type: CeN/YbN = 1.5 to 2.7; Zr/Nb = 4.5 to 9.6) and depleted (or normal-N-type: CeN/YbN = 0.6 to 0.8; Zr/Nb > 20) mid-ocean ridge basalts (MORB) occur as intercalated lava flows. To the north of the Hayes Fracture Zone, there is little apparent systematic relationship between basalt chemistry and geographic position. However, to the south of the Hayes Fracture Zone, the chemical character of the basalts (N-type MORB) is more uniform. The coexistence of both E-type and N-type MORB in one hole may be explicable in terms of either complex melting/ fractionation processes during basalt genesis or chemically heterogeneous mantle sources. Significant variation in the ratios of strongly incompatible trace elements (e.g., La/Ta; Th/Ta) in the basalts of Holes 558 and 561 are not easily explicable by processes such as dynamic partial melting or open system crystal fractionation. Rather, the trace element data require that the basalts are ultimately derived from at least two chemically distinct mantle sources. The results from Leg 82 are equivocal in terms of the evolution of the Azores "hot spot," but would appear not to be compatible with a simple model of E-type MORB magmatism associated with upwelling mantle "blobs." Models that invoke a locally chemically heterogeneous mantle are best able to account for the small-scale variation in basalt chemistry.

Geochemistry of oceanic crust of the Cocos Plate

New geochemical data from the Cocos Plate constrain the composition of the input into the Central American subduction zone and demonstrate the extent of influence of the Galápagos Hotspot on the Cocos Plate. Samples include sediments and basalts from Ocean Drilling Program (ODP) Site 1256 outboard of Nicaragua, gabbroic sills from ODP Sites 1039 and 1040, tholeiitic glasses from the Fisher Ridge off northwest Costa Rica, and basalts from the Galápagos Hotspot Track outboard of Central Costa Rica. Site 1256 basalts range from normal to enriched MORB in incompatible elements and have Pb and Nd isotopic compositions within the East Pacific Rise MORB field. The sediments have similar 206Pb/204Pb and only slightly more radiogenic 207Pb/204Pb and 208Pb/204Pb isotope ratios than the basalts. Altered samples from the subducting Galápagos Hotspot Track have similar Nd and Pb isotopic compositions to fresh Galápagos samples but have significantly higher Sr isotopic composition, indicating that the subduction input will have a distinct geochemical signature from Galápagos-type mantle material that may be present in the wedge beneath Costa Rica. Gabbroic sills from Sites 1039 and 1040 in East Pacific Rise (EPR) crust show evidence for influence of the Galápagos Hotspot ?100 km beyond the morphological hotspot track.

Geochemistry of dikes and lavas from the north wall of the Hess Deep Rift

An investigation of ~1-m.y.-old dikes and lavas from the north wall of the Hess Deep Rift (2°15'N, 101°30'W) collected during Alvin expeditions provides a detailed view of the evolution of fast spreading oceanic crust. The study area encompasses 25 km of an east-west flow line, representing ~370,000 years of crustal accretion at the East Pacific Rise. Samples analyzed exhibit depleted incompatible trace element abundances and ratios [(La/Sm)N < 1]. Indices of fractionation (MgO), and incompatible element ratios (La/Sm, Nb/Ti) show no systematic trends along flow line. Rather, over short (<4 m) and long (~25 km) distances, significant variations are observed in major and trace element concentrations and ratios. Modeling of these variations attests to the juxtaposition of dikes of distinct parental magma compositions. These findings, combined with studies of segmentation of the subaxial magma chamber and lateral magma transport in dikes along rift-dominated systems, suggest a more realistic model of the magmatic system underlying the East Pacific Rise relative to the commonly assumed twodimensional model. In this model, melts from a heterogeneous mantle feed distinct portions of a segmented axial magma reservoir. Dikes emanating from these distinct reservoirs transport magma along axis, resulting in interleaved dikes and host lavas with different evolutionary histories. This model suggests the use of axial or flow line lava compositions to infer the evolution of axial magma chambers should be approached with caution because dikes may never erupt lava or may transport magma significant distances along axis and erupt lavas far from their axial magma chamber of origin.

Geochemistry of ODP Leg 125 peridotites

Trace element analyses (first-series transition elements, Ti, Rb, Sr, Zr, Y, Nb, and REE) were carried out on whole rocks and minerals from 10 peridotite samples from both Conical Seamount in the Mariana forearc and Torishima Forearc Seamount in the Izu-Bonin forearc using a combination of XRF, ID-MS, ICP-MS, and ion microprobe. The concentrations of incompatible trace elements are generally low, reflecting the highly residual nature of the peridotites and their low clinopyroxene content (<2%). Chondrite-normalized REE patterns show extreme U shapes with (La/Sm)n ratios in the range of 5.03-250.0 and (Sm/Yb)n ratios in the range of 0.05-0.25; several samples show possible small positive Eu anomalies. LREE enrichment is common to both seamounts, although the peridotites from Conical Seamount have higher (La/Ce)n ratios on extended chondrite-normalized plots, in which both REEs and other trace elements are organized according to their incompatibility with respect to a harzburgitic mantle. Comparison with abyssal peridotite patterns suggests that the LREEs, Rb, Nb, Sr, Sm, and Eu are all enriched in the Leg 125 peridotites, but Ti and the HREEs exhibit no obvious enrichment. The peridotites also give positive anomalies for Zr and Sr relative to their neighboring REEs. Covariation diagrams based on clinopyroxene data show that Ti and the HREEs plot on an extension of an abyssal peridotite trend to more residual compositions. However, the LREEs, Rb, Sr, Sm, and Eu are displaced off this trend toward higher values, suggesting that these elements were introduced during an enrichment event. The axis of dispersion on these plots further suggests that enrichment took place during or after melting and thus was not a characteristic of the lithosphere before subduction. Compared with boninites sampled from the Izu-Bonin-Mariana forearc, the peridotites are significantly more enriched in LREEs. Modeling of the melting process indicates that if they represent the most depleted residues of the melting events that generated forearc boninites they must have experienced subsolidus enrichment in these elements, as well as in Rb, Sr, Zr, Nb, Sm, and Eu. The lack of any correlation with the degree of serpentinization suggests that low-temperature fluids were not the prime cause of enrichment. The enrichment in the high-field-strength elements also suggests that at least some of this enrichment may have involved melts rather than aqueous fluids. Moreover, the presence of the hydrous minerals magnesio-hornblende and tremolite and the common resorption of orthopyroxene indicate that this high-temperature peridotite-fluid interaction may have taken place in a water-rich environment in the forearc following the melting event that produced the boninites. The peridotites from Leg 125 may therefore contain a record of an important flux of elements into the mantle wedge during the initial formation of forearc lithosphere. Ophiolitic peridotites with these characteristics have not yet been reported, perhaps because the precise equivalents to the serpentinite seamounts have not been analyzed.

Geochemistry of the lower sheeted dike complex of ODP Holes 137-504B and 140-504B

Sixty-three samples representing 379 m of sheeted dikes from Deep Sea Drilling Project/Ocean Drilling Program Site 504B have been analyzed for major and selected trace elements by X-ray fluorescence. The samples range from microcrystalline aphyric basalts to moderately phyric (2%-10% phenocrysts) diabase that are typically multiply saturated with plagioclase, olivine, and clinopyroxene, in order of relative abundance. All analyzed samples are classified as Group D compositions with moderate to slightly elevated compatible elements (MgÆ-value = 0.65% ± 0.03%; Al2O3 = 15.5% ± 0.8%; CaO = 13.0% ± 0.3%; Ni = 114 ± 29 ppm), and unusually depleted levels of moderate to highly incompatible elements (Nb < 1 ppm; Zr = 44 ± 7 ppm; Rb < 0.5 ppm; Ba ~ 1 ppm; P2O5 = 0.07% ± 0.02%). These compositions are consistent with a multistage melting of a normal ocean ridge basaltic mantle source followed by extensive fractionation of olivine, plagioclase, and clinopyroxene. Leg 140 aphyric to sparsely phyric (0%-2% phenocrysts) basalts and diabases are compositionally indistinguishable from similarly phyric samples at higher levels in the hole. An examination of the entire crustal section, from the overlying volcanics through the sheeted dikes observed in Leg 140, reveals no significant trends indicating the enrichment or depletion of Costa Rica Rift Zone source magmas over time. Similarly, significant trends toward increased or decreased differentiation cannot be identified, although compositional patterns reflecting variable amounts of phenocryst addition are apparent at various depths. Below ? 1700 mbsf to the bottom of the Leg 140 section, there is a broadly systematic pattern of Zn depletion with depth, the result of high-temperature hydrothermal leaching. This zone of depletion is thought to be a significant source of Zn for the hydrothermal fluids depositing metal sulfides at ridge-crest hydrothermal vents and the sulfide-mineralization zone, located in the transition between pillow lavas and sheeted dikes. Localized zones of intense alteration (60%-95% recrystallization) are present on a centimeter to meter scale in many lithologic units. Within these zones, normally immobile elements Ti, Zr, Y, and rare-earth elements are strongly depleted compared with "fresher" samples centimeters away. The extent of compositional variability of these elements tends to obscure primary igneous trends if the highly altered samples are not identified or removed. At levels up to 40% (or possibly 60%) recrystallization, Ti, Zr, and Y retain their primary signatures. Although the mechanisms are unclear, it is possible that these intense alteration zones are a source of Y and rare-earth elements for the typically rare-earth-element-enriched hydrothermal vent fluids of mid-ocean ridges.

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

Major oxides, trace elements and rare earth elements of selected basalt samples at DSDP Hole 83-504B

DSDP Hole 504B is the deepest section drilled into oceanic basement, penetrating through a 571.5-m lava pile and a 209-m transition zone of lavas and dikes into 295 m of a sheeted dike complex. To define the basement composition 194 samples of least altered basalts, representing all lithologic units, were analyzed for their major and 26 trace elements. As is evident from the alteration-sensitive indicators H2O+, CO2, S, K, Mn, Zn, Cu, and the iron oxidation ratio, all rocks recovered are chemically altered to some extent. Downhole variation in these parameters enables us to distinguish five depth-related alteration zones that closely correlate with changes in alteration mineralogy. Alteration in the uppermost basement portion is characterized by pronounced K-uptake, sulfur loss, and iron oxidation and clearly demonstrates low-temperature seawater interaction. A very spectacular type of alteration is confined to the depth range from 910 to 1059 m below seafloor (BSF). Rocks from this basement portion exhibit the lowest iron oxidation, the highest H2O+ contents, and a considerable enrichment in Mn, S, Zn, and Cu. At the top of this zone a stockwork-like sulfide mineralization occurs. The chemical data suggest that this basement portion was at one time within a hydrothermal upflow zone. The steep gradient in alteration chemistry above this zone and the ore precipitation are interpreted as the result of mixing of the upflowing hydrothermal fluids with lower-temperature solutions circulating in the lava pile. Despite the chemical alteration the primary composition and variation of the rocks can be reliably established. All data demonstrate that the pillow lavas and the dikes are remarkably uniform and display almost the same range of variation. A general characteristic of the rocks that classify as olivine tholeiites is their high MgO contents (up to 10.5 wt.%) and their low K abundances (-200 ppm). According to their mg-values, which range from 0.60 to 0.74, most basalts appear to have undergone some high-level crystal fractionation. Despite the overall similarity in composition, there are two major basalt groups that have significantly different abundances and ratios of incompatible elements at similar mg-values. The majority of the basalts from the pillow lava and dike sections are chemically closely related, and most probably represent differentiation products of a common parental magma. They are low in Na2O, TiO2, and P2O5, and very low in the more hygromagmaphile elements. Interdigitated with this basalt group is a very rarely occurring basalt that is higher in Na2O, TiO2, P2O5, much less depleted in hygromagmaphile elements, and similar to normal mid-ocean ridge basalt (MORB). The latter is restricted to Lithologic Units 5 and 36 of the pillow lava section and Lithologic Unit 83 of the dike section. The two basalt groups cannot be related by differentiation processes but have to be regarded as products of two different parental magmas. The compositional uniformity of the majority of the basalts suggests that the magma chamber beneath the Costa Rica Rift reached nearly steady-state conditions. However, the presence of lavas and dikes that crystallized from a different parental magma requires the existence of a separate conduit-magma chamber system for these melts. Occasionally mixing between the two magma types appears to have occurred. The chemical characteristics of the two magma types imply some heterogeneity in the mantle source underlying the Costa Rica Rift. The predominant magma type represents an extremely depleted source, whereas the rare magma type presumably originated from regions of less depleted mantle material (relict or affected by metasomatism).

Major and trace element abundances of igneous rocks from DSDP Site 37-334

REE abundances in gabbros and peridotites from Site 334 of DSDP Leg 37 show that these rocks are cumulates produced by fractional crystallization of a primitive oceanic tholeiite magma. They may be part of a layered oceanic complex. The REE distributions in the residual liquids left after such a fractionation are similar to those of incompatible element-depleted oceanic tholeiites. The REE data indicate that the basalts which overlie the gabbro-peridotite complex, are not genetically related to plutonic rocks.

Diversificación y persistencia de pequeños productores apícolas. El caso del Partido de Magdalena. Periodo 1990-2013

Los cambios en el uso del suelo agrario en la Provincia de Buenos Aires y su repercusión en un grupo de pequeños productores apícolas que residen en el Partido de Magdalena ha evidenciado en los últimos años un cambio consecuencia de la aplicación del nuevo modelo agroindustrial en la región pampeana. Este nuevo modelo aplicado en el agro, que tiene como cultivo por excelencia las oleaginosas, genera una flora incompatible para que polinicen las abejas, no pudiendo producir derivados apícolas como en este caso la miel. Esta situación generó que los pequeños productores apícolas del Partido tuvieran que diversificarse para persistir en sus actividades. En este contexto, a partir de la búsqueda de información bibliográfica y de la realización de entrevistas a actores claves se tratara de analizar las estrategias que implementaron los pequeños productores apícolas para poder subsistir en la actividad y diversificarse, a partir de la pluriactividad, en otras labores tanto prediales como extraprediales para la reproducción social de la unidad familiar en el periodo de 1990-2013

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

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

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

Diversificación y persistencia de pequeños productores apícolas. El caso del Partido de Magdalena. Periodo 1990-2013

Los cambios en el uso del suelo agrario en la Provincia de Buenos Aires y su repercusión en un grupo de pequeños productores apícolas que residen en el Partido de Magdalena ha evidenciado en los últimos años un cambio consecuencia de la aplicación del nuevo modelo agroindustrial en la región pampeana. Este nuevo modelo aplicado en el agro, que tiene como cultivo por excelencia las oleaginosas, genera una flora incompatible para que polinicen las abejas, no pudiendo producir derivados apícolas como en este caso la miel. Esta situación generó que los pequeños productores apícolas del Partido tuvieran que diversificarse para persistir en sus actividades. En este contexto, a partir de la búsqueda de información bibliográfica y de la realización de entrevistas a actores claves se tratara de analizar las estrategias que implementaron los pequeños productores apícolas para poder subsistir en la actividad y diversificarse, a partir de la pluriactividad, en otras labores tanto prediales como extraprediales para la reproducción social de la unidad familiar en el periodo de 1990-2013

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.