996 resultados para Eastern Province [Kenya]
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In the Cape Caribou River allochthon (CCRA), metaigneous and gneissic units occur as a shallowly plunging synform in the hanging wall of the Grand Lake thrust system (GLTS), a Grenvillian structure that forms the boundary between the Mealy Mountains and Groswater Bay terranes. The layered rocks of the CCRA are cut by a stockwork of monzonite dykes related to the Dome Mountain suite and by metadiabase-amphibolite dykes that probably form part of the ca. 1380 Ma Mealy swarm. The mafic dykes appear to postdate much of the development of subhorizontal metamorphic layering within the lower parts of the CCRA. The uppermost (least metamorphosed) units of the CCRA, the North West River anorthosite-metagabbro and the Dome Mountain monzonite suite, have been dated at 1625 +/- 6 and 1626 +/- 2 Ma, respectively. An amphibolite unit that concordantly underlies the anorthosite-metagabbro and is intruded discordantly by monzonite dykes has given metamorphic ages of 1660 +/- 3 and 1631 +/- 2 Ma. Granitoid gneisses that form the lowest level of the CCRA have given a migmatization age of 1622 +/- 6 Ma. The effects of Grenvillian metamorphism become apparent in the lower levels of the allochthon where gneisses, amphibolite, and mafic dykes have given new generation zircon ages of 1008 +/- 2, 1012 +/- 3, and 1011 +/- 3 Ma, respectively. A posttectonic pegmatite has also given zircon and monazite ages of 1016(-3)(+7) and 1013 +/- 3 Ma, respectively. Although these results indicate new growth of Grenvillian zircon, this process was generally not accompanied by penetrative deformation or melting. Thus, the formation of gneissic fabrics and the overall layered nature of the lower CCRA are a result primarily of Labradorian (1660-1620 Ma) tectonism and intrusion, and probably reflect early movement on an ancestral GLTS. Grenvillian heating and metamorphism (up to granulite facies) was strongly concentrated towards the base of the CCRA and probably occurred during northwestward thrusting of the allochthon over the Groswater Bay terrane.
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The Hamersley province of northwest Australia is one of the world's premier iron ore regions with high-grade martite-microplaty hematite iron ore deposits mostly hosted within banded iron formation (BIF) sequences of the Brockman Iron Formations of the Hamersley Group. These high-grade iron ores contain between 60 and 68 wt percent Fe, and formed by the multistage interaction of hydrothermal fluids with the host BIF formation. The oxygen isotope compositions of magnetite and hematite from BIF, hydrothermal alteration assemblages, and high-grade iron Ore were analyzed from the Mount Tom Price, Paraburdoo, and Charmar iron ore deposits. The delta(18)O values of magnetite and hematite from hydrothermal alteration assemblages and high-grade iron ore range from -9.0 to -2.9 per mil, a depletion of 5 to 15 per mil relative to the host BIF. The delta(18)O values are spatially controlled by faults within the deposits, a response to higher fluid flux and larger influence the isotopic compositions by the hydrothermal fluids. The oxygen isotope composition of hydrothermal fluids (delta(18)O(fluid)) indicates that the decrease in the (18)O content of iron oxides was due to the interaction of both basinal brines and meteoric fluids with the original BIF. Late-stage talc-bearing ore at the Mount Tom Price deposit formed in the presence of a pulse of delta(18)O-enriched basinal brine, indicating that hydrothermal fluids may have repeatedly interacted with the BIFs during the Paleoproterozoic.
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Aim The spotted knapweed (Centaurea stoebe), a plant native to south-east and central Europe, is highly invasive in North America. We investigated the spatio-temporal climatic niche dynamics of the spotted knapweed in North America along two putative eastern and western invasion routes. We then considered the patterns observed in the light of historical, ecological and evolutionary factors. Location Europe and North America. Methods The niche characteristics of the east and west invasive populations of spotted knapweed in North America were determined from documented occurrences over 120 consecutive years (1890-2010). The 2.5 and 97.5 percentiles of values along temperature and precipitation gradients, as given by the two first axes of a principal component axis (PCA), were then calculated. We additionally measured the climatic dissimilarity between invaded and native niches using a multivariate environmental similarity surface (MESS) analysis. Results Along both invasion routes, the species established in regions with climatic conditions that were similar to those in the native range in Europe. An initial spread in ruderal habitats always preceded spread in (semi-)natural habitats. In the east, the niche gradually increased over time until it reached limits similar to the native niche. Conversely, in the west the niche abruptly expanded after an extended time lag into climates not occupied in the native range; only the native cold niche limit was conserved. Main conclusions Our study reveals that different niche dynamics have taken place during the eastern and western invasions. This pattern indicates different combinations of historical, ecological and evolutionary factors in the two ranges. We hypothesize that the lack of a well-developed transportation network in the west at the time of the introduction of spotted knapweed confined the species to a geographically and climatically isolated region. The invasion of dry rangelands may have been favoured during the agricultural transition in the 1930s by release from natural enemies, local adaptation and less competitive vegetation, but further experimental and molecular studies are needed to explain these contrasting niche patterns fully. Our study illustrates the need and benefit of applying large-scale, temporally explicit approaches to understanding biological invasions.
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Des del segon quart del s. I aC i, especialment, durant el regnat d’August, es va desenvolupar a l’antiga província Tarraconensis un sistema productiu centrat en l’explotació agrària vitivinícola amb una finalitat clarament comercial. La majoria d’assentament vitivinícoles es troben emplaçats al litoral català, associats de vegades a figlinae que fabricaven les àmfores per al transport i comerç de l’excedent vinícola. No obstant, a l’àrea del Vallès Occidental i del Baix Llobregat es troben una sèrie de vil•les vinculades a la producció de vi i a la fabricació d’àmfores que han proporcionat restes molt significatives sobre la contribució d’aquesta zona a l’expansió econòmica de la província. La caracterització arqueològica i arqueomètrica d’un gran nombre d’àmfores procedents de diversos tallers ceràmics situats al Vallès Occidental i al Baix Llobregat, utilitzant diverses tècniques d’anàlisi química, mineralògica i petrogràfica, ha portat a establir quins tipus d’àmfores es van fabricar a cada taller i de quina manera. S’han identificat alguns dels processos tecnològics de la cadena operativa: la selecció i processat de les matèries primeres per conformar la pasta procedents, generalment, de l’àrea on es troba cada centre de producció, el modelatge, l’assecat i la cocció de les peces. En alguns dels casos analitzats, s’ha identificat quins tipus de contenidors van ser importants a l’establiment i la seva provinença. La integració d’aquests resultats en la base de dades analítica que disposa l’ERAAUB ha permès avaluar el grau d’estandardització dels processos tecnològics en aquesta àrea. La contrastació final amb les dades històriques i arqueològiques contribueix al coneixement arqueològic de les àmfores vinàries de la Tarraconensis i, a través d’elles, al coneixement de les societats que les van fabricar, comercialitzar i utilitzar.
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Collection : Physiologies Laisné-Aubert
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[Traditions. Asie. Inde. Présidence de Madras [i.e. Chennai]. Ceded Districts]
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[Traditions. Asie. Inde. Province de Madras [i.e. Chennai]. État du Kerala. Etat du tamil Nadu. Travancore]
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[Traditions. Asie. Inde. Province de Madras [i.e. Chennai]. État du Kerala. Etat du tamil Nadu. Travancore]
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[Traditions. Asie. Inde. Province de Madras [i.e. Chennai]. Etat du Tamil Nadu. Tinnevelly]
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[Traditions. Asie. Inde. Province de Madras [i.e. Chennai]. Etat du Karnataka. Mysore]
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[Traditions. Asie. Inde. Présidence de Madras [i.e. Chennai]. Ceded Districts]
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[Traditions. Asie. Inde. Province de Madras [i.e. Chennai]]