Chevkinite-Group Minerals from Granulite-Facies Metamorphic Rocks and Associated Pegmatites of East Antarctica and South India

Electron microprobe data are presented for chevkinite-group minerals from granulite-facies rocks and associated pegmatities of the Napier Complex and Mawson Station charnockite in East Antarctica and from the Eastern Ghats, South India. Their compositions conform to the general formula for this group, viz. A(4)BC(2)D(2)Si(4)O(22) where, in the analysed specimens A = (rare-earth elements (REE), Ca, Y, Th), B = Fe(2+) Mg, C = (Al, Mg, Ti, Fe(2+), Fe(3+), Zr) and D = Ti and plot within the perrierite field oftlic total Fe (as FeO) (wt.%) vs. CaO (wt.%) discriminator diagram of Macdonald and Belkin (2002). In contrast to most chevkinite-group minerals, the A site shows unusual enrichment in the MREE and HREE relative to the LREE and Ca. In one sample from the Napier Complex, Y is the dominant cation among the total REE + Y in the A site, the first reported case of Y-dominance in the chevkinite group. The minerals include the most Al-rich yet reported in the chevkinite group (<= 9.15 wt.% Al(2)O(3)), sufficient to fill the C site in two samples. Conversely, the amount of Ti in these samples does not fill the D site. and, thus, some of the Al could be making up the deficiency at D, a situation not previously reported in the chevkinite group. Fe abudances are low, requiring Mg to occupy up to 45% of the B site. The chevkinite-group minerals analysed originated from three distinct parageneses: (1) pegmatites containing hornblende and orthopyroxene or garnet; (2) orthopyroxene-bearing gneiss and granulite; (3) highly aluminous paragneisses in which the associated minerals are relatively magnesian or aluminous. Chevkinite-group minerals from the first two parageneses have relatively high FeO content and low MgO and Al(2)O(3) contents; their compositions plot in the field for mafic and intermediate igneous rocks. In contrast, chevkinite-group minerals from the third paragenesis are notably more aluminous and have greater Mg/Fe ratios.

Measurement of the differential cross-section of B⁺ meson production in pp collisions at sqrts = 7 TeV at ATLAS

The production cross-section of B+ mesons is measured as a function of transverse momentum p T and rapidity y in proton-proton collisions at centre-of-mass energy root s = 7 TeV, using 2.4 fb(-1) of data recorded with the ATLAS detector at the Large Hadron Collider. The differential production cross-sections, determined in the range 9 GeV < p(T) < 120 GeV and vertical bar y vertical bar < 2.25, are compared to next-to-leading-order theoretical predictions.

Sensory innervation of the dorsal longitudinal ligament and the meninges in the lumbar spine of the dog

Although intervertebral disc herniation is a well-known disease in dogs, pain management for this condition has remained a challenge. The goal of the present study is to address the lack of information regarding the innervation of anatomical structures within the canine vertebral canal. Immunolabeling was performed with antibodies against protein gene product 9.5, Tuj-1 (neuron-specific class III β-tubulin), calcitonin gene-related peptide, and neuropeptide Y in combination with the lectin from Lycopersicon esculentum as a marker for blood vessels. Staining was indicative of both sensory and sympathetic fibers. Innervation density was the highest in lateral areas, intermediate in dorsal areas, and the lowest in ventral areas. In the dorsal longitudinal ligament (DLL), the highest innervation density was observed in the lateral regions. Innervation was lower at mid-vertebral levels than at intervertebral levels. The presence of sensory and sympathetic fibers in the canine dura and DLL suggests that pain may originate from both these structures. Due to these regional differences in sensory innervation patterns, trauma to intervertebral DLL and lateral dura is expected to be particularly painful. The results ought to provide a better basis for the assessment of medicinal and surgical procedures.

The New Cockney: New Ethnicities and Adolescent Speech in the Traditional East End of London

The New Cockney provides a sociolinguistic account of speech variation among adolescents in the 'traditional' East End of London. The study takes account of the social and economic upheaval in the area since the 1950s, primarily concentrating on factors such as the immigration of the Bangladeshi community and its effect on the Cockney dialect. By paying attention to the particular, this book contributes to a better understanding of the more general concerns of linguistic variation. With a focus on the interaction and social practices of a group of adolescents attending a youth centre, the study highlights some of the possible mechanisms for language change.

Investigación en el campo del arte : Presentación de un caso y niveles de anclaje

Muchas veces en la investigación en el campo del arte los términos son ambiguos si no se los precisa. Retomamos la distinción entre cuestiones ontológicas (tipos de objetos de investigación), epistemológicas (conocimientos producidos) y metodológicas propiamente dichas (discusiones en torno de los vínculos con las Ciencias Sociales). A su vez distinguimos la investigación en el campo del arte de la investigación artística (IENA) propiamente dicha, reservando para esta última los sentidos de un tipo de indagación estética creativa en la incorporación de nuevos lenguajes y modalidades de obras. El trabajo busca ser una excusa para que, presentando una exploración en curso dentro de la casa/museo El fogón de los arrieros, podamos actualizar brevemente un debate sobre dos concepciones vinculadas: la IENA y la investigación sobre objetos artísticos. Además de arriesgar una propuesta de abordaje con matriz de datos para estratificar los niveles de análisis, dejando interrogantes para sucesivos planteos que contengan los rasgos propios de la pesquisa teórica y práctica sobre artes.

Belleza y Felicidad en la vorágine del 2001 : Algunas percepciones contemporáneas sobre las condiciones de un arte político

Muy discutida en su momento, la producción de Belleza y Felicidad, y especialmente los debates que generó en torno suyo, permite iluminar retrospectivamente los conceptos y valoraciones subyacentes en las discusiones sobre arte y poesía de fines de los noventa y principios de la década del dos mil. Este artículo recorre, desde esta premisa, tres textos críticos publicados en el período por Martín Prieto y Daniel García Helder, César Aira y Mario Ortiz, en los que a propósito de la lectura crítica de Belleza y Felicidad, se ordenan ciertos modos posibles de la vinculación entre poesía y política.

Investigación en el campo del arte : Presentación de un caso y niveles de anclaje

Muchas veces en la investigación en el campo del arte los términos son ambiguos si no se los precisa. Retomamos la distinción entre cuestiones ontológicas (tipos de objetos de investigación), epistemológicas (conocimientos producidos) y metodológicas propiamente dichas (discusiones en torno de los vínculos con las Ciencias Sociales). A su vez distinguimos la investigación en el campo del arte de la investigación artística (IENA) propiamente dicha, reservando para esta última los sentidos de un tipo de indagación estética creativa en la incorporación de nuevos lenguajes y modalidades de obras. El trabajo busca ser una excusa para que, presentando una exploración en curso dentro de la casa/museo El fogón de los arrieros, podamos actualizar brevemente un debate sobre dos concepciones vinculadas: la IENA y la investigación sobre objetos artísticos. Además de arriesgar una propuesta de abordaje con matriz de datos para estratificar los niveles de análisis, dejando interrogantes para sucesivos planteos que contengan los rasgos propios de la pesquisa teórica y práctica sobre artes.

Investigación en el campo del arte : Presentación de un caso y niveles de anclaje

Muchas veces en la investigación en el campo del arte los términos son ambiguos si no se los precisa. Retomamos la distinción entre cuestiones ontológicas (tipos de objetos de investigación), epistemológicas (conocimientos producidos) y metodológicas propiamente dichas (discusiones en torno de los vínculos con las Ciencias Sociales). A su vez distinguimos la investigación en el campo del arte de la investigación artística (IENA) propiamente dicha, reservando para esta última los sentidos de un tipo de indagación estética creativa en la incorporación de nuevos lenguajes y modalidades de obras. El trabajo busca ser una excusa para que, presentando una exploración en curso dentro de la casa/museo El fogón de los arrieros, podamos actualizar brevemente un debate sobre dos concepciones vinculadas: la IENA y la investigación sobre objetos artísticos. Además de arriesgar una propuesta de abordaje con matriz de datos para estratificar los niveles de análisis, dejando interrogantes para sucesivos planteos que contengan los rasgos propios de la pesquisa teórica y práctica sobre artes.

Belleza y Felicidad en la vorágine del 2001 : Algunas percepciones contemporáneas sobre las condiciones de un arte político

Muy discutida en su momento, la producción de Belleza y Felicidad, y especialmente los debates que generó en torno suyo, permite iluminar retrospectivamente los conceptos y valoraciones subyacentes en las discusiones sobre arte y poesía de fines de los noventa y principios de la década del dos mil. Este artículo recorre, desde esta premisa, tres textos críticos publicados en el período por Martín Prieto y Daniel García Helder, César Aira y Mario Ortiz, en los que a propósito de la lectura crítica de Belleza y Felicidad, se ordenan ciertos modos posibles de la vinculación entre poesía y política.

Investigación en el campo del arte : Presentación de un caso y niveles de anclaje

Muchas veces en la investigación en el campo del arte los términos son ambiguos si no se los precisa. Retomamos la distinción entre cuestiones ontológicas (tipos de objetos de investigación), epistemológicas (conocimientos producidos) y metodológicas propiamente dichas (discusiones en torno de los vínculos con las Ciencias Sociales). A su vez distinguimos la investigación en el campo del arte de la investigación artística (IENA) propiamente dicha, reservando para esta última los sentidos de un tipo de indagación estética creativa en la incorporación de nuevos lenguajes y modalidades de obras. El trabajo busca ser una excusa para que, presentando una exploración en curso dentro de la casa/museo El fogón de los arrieros, podamos actualizar brevemente un debate sobre dos concepciones vinculadas: la IENA y la investigación sobre objetos artísticos. Además de arriesgar una propuesta de abordaje con matriz de datos para estratificar los niveles de análisis, dejando interrogantes para sucesivos planteos que contengan los rasgos propios de la pesquisa teórica y práctica sobre artes.

Belleza y Felicidad en la vorágine del 2001 : Algunas percepciones contemporáneas sobre las condiciones de un arte político

Muy discutida en su momento, la producción de Belleza y Felicidad, y especialmente los debates que generó en torno suyo, permite iluminar retrospectivamente los conceptos y valoraciones subyacentes en las discusiones sobre arte y poesía de fines de los noventa y principios de la década del dos mil. Este artículo recorre, desde esta premisa, tres textos críticos publicados en el período por Martín Prieto y Daniel García Helder, César Aira y Mario Ortiz, en los que a propósito de la lectura crítica de Belleza y Felicidad, se ordenan ciertos modos posibles de la vinculación entre poesía y política.

Neogene and Paleocene-Maestrichtian calcareous nannofossils in sediments of the upper continental rise off New Jersey

Maestrichtian to Holocene calcareous nannofossils from two closely spaced sites on the upper continental rise some 100 miles (161 km) southeast of Atlantic City, New Jersey, were zoned in order to help date a major canyon-cutting event in the late Miocene and to delineate and correlate other hiatuses with seismic stratigraphy. Mid-middle Eocene through middle Miocene sediments (Zones CP14 to CN6) were not recovered in these holes, but nearly all other zones are accounted for. The Eocene section is described in a companion chapter (Applegate and Wise, 1987, doi:10.2973/dsdp.proc.93.118.1987). Nannofossils are generally sparse and moderately preserved in the clastic sediments of Site 604. Sedimentation rates are extremely high for the upper Pleistocene (201 m/m.y. minimum) above a hiatus calculated to span 0.44 to 1.1 Ma. The associated disconformity is correlated with local seismic reflection Horizon Pr . Sedimentation rates continue to be high (93 m/m.y.) down to a second hiatus in the upper Pliocene dated from about 2.4 to 2.9 (or possibly 3.3) Ma. The disconformity associated with this hiatus is correlated with local seismic reflection Horizon P2 and regional Reflector Blue, which can be interpreted to mark either the onset of Northern Hemisphere continental glaciation or circulation changes associated with the closure of the Central American Seaway. Sedimentation rates in the pre-glacial lower Pliocene are only about a third those in the glacial upper Pliocene. A prominent disconformity in the upper Miocene marks a major lithologic boundary that separates Messinian(?) glauconitic claystones above from lower Tortonian conglomeratic debris flows and turbidites below. The debris flows recovered are assigned to nannofossil Zones CN8a and CN7, but drilling difficulties prevented penetration of the bottom of this sequence some 100 m below the terminal depth of the hole. Correlation of the lower bounding seismic reflector (M2/Merlin?) to a drift sequence drilled on the lower rise at DSDP Site 603, however, predicts that the debris flows began close to the beginning of the late Miocene (upper Zone CN6 time) at about 10.5 Ma. The debris flows represent a major canyon-cutting event that we correlate with the beginning of the particularly severe late Miocene glaciations believed to be associated with the formation of the West Antarctic Ice Sheet. The existence of these spectacular debris flows strongly suggest that the late Miocene glacio-eustatic low stand occurred during Vail Cycle TM3.1 (lower Tortonian) rather than during Vail Cycle TM3.2 (Messinian) as originally published. Beneath a set of coalesced regional disconformities centered upon seismic reflection Horizon Au, coccoliths are abundant and in general are moderately preserved at Site 605 in a 619-m carbonate section extending from the middle Eocene Zone CP13b to the upper Maestrichtian Lithraphidites quadratus Zone. Sedimentation rates are 37 m/m.y. in the Eocene down to a condensed interval near the base (Zone CP9). A disconformity is suspected near the Eocene/Paleocene boundary. Sedimentation rates for the upper Paleocene Zone CP8 are similar to those of the Eocene, but Zones CP7 and CP6 lie within another condensed interval. The highest Paleocene rates are 67 m/m.y. down through Zones CP5 and CP4 to a major disconformity that separates the upper Paleocene from the Danian. This hiatus spans about 2.6 m.y. (upper Zone CP3 to lower Zone CP2) and corresponds to the major sea-level drop at the base of Vail Cycle TE2.1. As the most prominent break in this Paleogene section, it may correspond to seismic reflection Horizon A* of the North American Basin. Sedimentation rates from this point to the Cretaceous/Tertiary boundary drop to 11 m/m.y., still high for a Paleocene DSDP section. No major break in deposition could be detected at the Cretaceous/Tertiary boundary.

Concentration of the rare-earth elements in metalliferous sediments from DSDP Leg 92 holes

DSDP Leg 92 drilled at four sites along an east-west transect at 19°S on the western flank of the East Pacific Rise (EPR), in an area where sediments are essentially a mixture of hydrothermal and biogenic components, with only a minimal contribution of clastic material. Rare-earth element (REE) data on the metalliferous (non-carbonate) fraction of samples ranging in age from ~2 to ~27 Ma indicate the existence of two distinct groups of patterns corresponding to two broad age groups, one <=8 Ma, the other >=10 Ma. Within each group, REE patterns have characteristics which are near-uniform, despite large variations in total REE abundances. Sediments of the younger group are enriched in light REE (LREE) relative to deep bottom waters influenced by the hydrothermal plume extending west from the EPR at 19°S. Sediments of the older groups show further relative LREE enrichment and/or heavy REE (HREE) depletion. Surficial sediments deposited beneath the lysocline have high Sum REE concentrations resulting from slow accumulation rates, and patterns resembling older sediments due to early diagenetic effects. A correlation between the mass accumulation rates (MAR) of Sum REE and Fe + Mn suggests that ferromanganese particulate matter supplied by the hydrothermal plume scavenges REE; during this process the LREE are preferentially removed from plume seawater. The MAR of Fe + Mn shows a general decrease with age above basement, whereas Sum REE concentrations in the metalliferous component increase with age above basement. This supports the Ruhlin and Owen model wherein limited scavenging of REE, due to rapid burial of sediment near the palaeo-axis, leads to low concentrations (but high MAR-values) for the REE. Following deposition and burial of the hydrothermal component, further relative flattening of the REE pattern takes place, probably the result of diagenetic reactions over several million years. Phase partitioning data indicate that the proportion of REE residing in more poorly crystalline phases tends to increase with age (from ~45% to 90% of Sum REE). This suggests that as initial ferromanganese precipitates undergo diagenetic recrystallization, REE are transferred to the poorly crystalline phases, and/or are scavenged from pore waters by these phases. Because of the various modifications to REE patterns apparently produced both in the water column and post-depositional settings, the REE patterns of metalliferous sediments will not reflect fine-scale REE variations in associated oceanic water masses.