Trace element distribution in mineral separates of the Allende inclusions and their genetic implications |
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| Authors: | Hiroshi Nagasawa Douglas P Blanchard Jeffrey W Jacobs Joyce C Brannon John A Philpotts Naoki Onuma |
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| Institution: | Lunar Science Institute, Houston, TX 77058, U.S.A.;National Aeronautics and Space Administration, Johnson Space Center, Houston, TX 77058, U.S.A.;Lockheed Electronics Company Incorporated, Houston, TX 77058, U.S.A.;National Aeronautics and Space Administration, Goddard Space Flight Center, Greenbelt, MD 20771, U.S.A.;Tsukuba University, Ibaraki 300-31, Japan |
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| Abstract: | Concentrations of the REE, Sc, Co, Fe, Zn, Ir, Na and Cr were determined by instrumental neutron activation and mass spectrometric isotope dilution analysis for mineral separates of the coarseand fine-grained types (group I and II of Martin and Mason's classification) of the Allende inclusions.These data, combined with data on mineral/liquid partition coefficients, oxygen isotope distributions and diffusion calculations, suggest the following: (1) Minerals in the coarse-grained inclusions (group I) crystallized in a closed system with respect to refractory elements. On the other hand, differences in oxygen isotope distributions among minerals preclude a totally molten stage in the history of the inclusion. Group I inclusions were formed by rapid condensation (either to liquid or solid) in a supercooled solar nebula; extrasolar pyroxene and spinel dust were included but not melted in the condensing inclusions, thus preserving their extrasolar oxygen isotope composition. REE were distributed by diffusion during the subsequent heating at subsolidus temperatures; because oxygen diffuses much more slowly at these temperatures, the oxygen isotope anomalies were preserved. (2) The fine-grained (group II) inclusions were also formed by condensation from a super-cooled nebular gas; however, REE-rich clinopyroxene and spinel were formed early and REE-poor sodalite and nepheline were formed later and mechanically mixed with clinopyroxene and spinel to form the inclusions. The REE patterns of the bulk inclusions and the mineral separates are fractionated, indicating that REE abundances in the gaseous phase were already fractionated at the time of condensation of the minerals. (3) Pre-existing Mg isotope anomalies in the coarse-grained inclusions must have been erased during the heating stage thus resetting the 26Al-26Mg chronometer. |
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