Varying rock responses as an indicator of changes in CO2-H2O fluid composition

The formation of the late Archean charnockite zone of southern India was ascribed to dehydration recrystallization due to an influx of CO2. Pressure temperature conditions for the metamorphism were calculated at about 750 C and 7.5 Kbar. The composition of the volatile species presently contained in fluid inclusions in the rocks changes across the transition zone. The transition zone was studied at Kabbaldurga and the paths taken by the fluids were identified

Communications planning: a review of policy and communications

This report presents a discussion of communications strategies to influence policy outcomes. It is based on a series of interviews with projects, NGOs and regional organisations to review current activities and assess the implications for STREAM of developing a communications strategy within a livelihoods framework. The main message of the report is that in order to fulfil its guiding principles. STREAM must acknowledge that policy change is related to governance and civil society, and requires a broad range of partnerships and a broad range of voices in the policy-making arena. (Pdf contains 49 pages)

Significance of the late Archaean granulite facies terrain boundaries, Southern West Greenland

Three distinct episodes and occurrences of granulite metamorphism in West Greenland are described: (1) the oldest fragmentary granulites occur within the 3.6-Ga Amitsoq gneisses and appear to have formed 200 Ma after the continental crust in which they lie (Spatially associated rapakivi granites have zircon cores as old as 3.8 Ga, but Rb-Sr, whole-rock Pb-Pb, and all other systems give 3.6 Ga, so these granulites apparently represent a later metamorphic event); (2) 3.0-Ga granulites of the Nordlandet Peninsula NW of Godthaab, developed immediately after crustal formation in hot, dry conditions, are carbonate-free, associated with voluminous tonalite, and formed at peak metamorphic conditions of 800 C and 7 to 8 kbar (Synmetamorphic trondhjemite abounds and the activity of H2O has been indicated by Pilar to have varied greatly); and (3) 2.8-Ga granulites south of Godthaab, lie to the south of retrogressed amphibolite terranes. Prograde amphibolite-granulite transitions are clearly preserved only locally at the southern end of this block, near Bjornesund, south of Fiskenaesset. Progressively deeper parts of the crust are exposed from south to north as a major thrust fault is approached. Characteristic big hornblende pegmatites, which outcrop close to the thrust in the east, have been formed by replacement of orthopyroxene. Comparable features were not seen in South Indian granulites. It was concluded that no one mechanism accounts for the origin of all granulites in West Greenland. Various processes have interacted in different ways, and what happened in individual areas must be worked out by considering all possible processes

Assessing and Preserving Intellectual Property in Online Collaborative Composition

See presentation description

Five patients with oedema: written for the Wightman Prize in Clinical Medicine, 1962

This is an account of five patients seen in :. iards 21, 23 and 24 of the Royal Infirmary, Edinburgh; all the patients suffered from some form of oedema. The severity of the oedema varied greatly in the different patients, as did the factors responsible for its appearance. This account aims merely to recount the clinical histories, with special emphasis on the oedema, and to discuss the causes as revealed in each patient.In the interests of brevity and clarity, it has been necessary to omit some of the details of the history and clinical findings in each patient where they were not strictly relevant to the problem of oedema, but any details of special interest have also been included. Although this is intended primarily as a clinical account, the discussion of the pathogenesis of oedema in each patient must, as so often in medicine today, delve into mechanisms at a microscopic and even at a molecular level. At this level, the discussion runs the risk of either being too brief and dogmatic, or else too detailed and inconclusive; and at any level the discussion must inevitably be incomplete. Many of the theories of the pathogenesis of oedema are speculative and controversial, and the more complete the reading of the literature, the more confusing the picture becomes. The author has attempted, in this account, to discuss some of the more important factors in the production of oedema, but has tried to avoid confusing himself and the reader with too much detail.Oedema, which may be defined as a localised or generalised increase in the volume of the interstitial fluid, can arise in many diseases, and be the result of the interplay of a number of factors. These factors are not well understood - but the first patient suffered from oedema of a type where the simpler explanations would seem to suffice

Attitudes and knowledge of forestry by high school agricultural education teachers in West Virginia

The purpose of this study was to determine the attitudes and knowledge of high school agricultural education teachers in West Virginia towards forestry. A descriptive research design was used for this study. Of the 86 West Virginia high school agricultural teachers selected for this study 40 teachers responded for a response rate of 47%. Of the responding teachers 85% wanted or needed more information on forestry. Also 57% of the responding teachers had not taken any other formal forestry training besides their college course work. When respondents were asked to react to the following statement: agricultural education teachers need more training in forestry , they agreed

The geology and petrogenesis of the southern closepet granite

The Archaean Closepet Granite is a polyphase body intruding the Peninsular Gneiss Complex and the associated supracrustal rocks. The granite out-crop runs for nearly 500 km with an approximate width of 20 to 25 km and cut across the regional metamorphic structure passing from granulite facies in the South and green schist facies in the north. In the amphibolite-granulite facies transition zone the granite is intimately mixed with migmatites and charnockite. Field observations suggests that anatexis of Peninsular gneisses led to the formation of granite melt, and there is a space relationship between migmatite formation, charnockite development and production and emplacement of granite magma. Based on texture and cross cutting relationships four major granite phases are recognized: (1) Pyroxene bearing dark grey granite; (2) Porphyritec granite; (3) Equigranular grey granite; and (4) Equigranular pink granite. The granite is medium to coarse grained and exhibit hypidiomorphic granular to porphyritic texture. The modal composition varies from granite granodiorite to quartz monzonite. Geochemical variation of the granite suite is consistent with either fractional crystallization or partial melting, but in both the cases biotite plus feldspar must be involved as fractionating or residual phases during melting to account trace element chemistry. The trace element data has been plotted on discriminant diagrams, where majority of samples plot in volcanic arc and within plate, tectonic environments. The granite show distinct REE patterns with variable total REE content. The REE patterns and overall abundances suggests that the granite suite represents a product of partial melting of crustal source in which fractional crystallization operated in a limited number of cases

The 'Lindholme Advance' and the extent of the Last Glacial Maximum in the Vale of York

The limits of the glacier that occupied the southwest part of the southern Vale of York at the Last Glacial Maximum are defined in relation to recent temporary exposures at Lindholme and previous regional mapping by Geoff Gaunt. Erratic content of associated diamicts indicates sources in the Yorkshire Dales, over Stainmore and along the Permo-Triassic outcrops on the west side of the Vale of York. The advance is dated to an episode associated with a high level of pro-glacial Lake Humber within the Last Glacial Maximum. Lidar imagery suggests that the northeastern ice limit is concealed beneath later alluvium of the rivers Ouse and Trent