111,927 research outputs found

    The Role of Culture in Social Development Over the Lifespan: An Interpersonal Relations Approach

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    This article aims to illustrate the role of culture for individual development throughout the life span. First, theoretical approaches how culture affects the ontogenesis is presented, starting from early anthropological to recent eco-cultural and culture-informed approaches. Then, culture-specific conceptualizations of development over the life span are discussed, focusing on development in childhood, adolescence, adulthood, and old age. Finally, we concentrate on selected areas of social development and report on recent studies on subjective theories, transmissions of values, and intergenerational relations. These studies are discussed as aspects of a more extended interpersonal relations approach to development within culture

    author-bios-SRD-19-0063.R1 – Supplemental material for The Network Structure of Police Misconduct

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    Supplemental material, author-bios-SRD-19-0063.R1 for The Network Structure of Police Misconduct by George Wood, Daria Roithmayr and Andrew V. Papachristos in Socius</p

    Incompatible element-rich fluids released by antigorite breakdown in deeply subducted mantle

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    We present first trace element analyses of the fluid produced during breakdown of antigorite serpentine, a major dehydration reaction occurring at depth within subducting oceanic plates. Microinclusions filled with crystals+aqueous liquid are disseminated within olivine and orthopyroxene grown at pressures and temperatures beyond the stability field of antigorite. Despite hydrogen loss and significant major element changes that have affected the analyzed inclusions, their trace element composition still reflects characteristics of the subduction fluid released during serpentinite dehydration. The fluid is enriched in incompatible elements indicating either (1) interaction with fluids derived from crustal slab components, or (2) dehydration of altered (serpentinized) oceanic mantle previously enriched in incompatible elements. Several features of the analyzed fluid+mineral inclusions (high Pb/Th, Pb/U and Pb/Ce) are in agreement with available experimental work, as well as with the geochemical signatures of most arc lavas and of several ocean island basalt mantle sources. The trace element patterns of the fluid+mineral inclusions do not display relative enrichment in large ion lithophile elements compared to high field strength elements, thus suggesting that the latter elements may become soluble in natural subduction fluids
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