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Mössbauer and thermoluminescence studies of meteorites from Frontier Mountain, Antarctica
Author(s) -
Calogero Sandro,
Stievano Lorenzo,
Benoit Paul H.
Publication year - 1999
Publication title -
journal of geophysical research: planets
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/1999je001074
Subject(s) - chondrite , thermoluminescence , meteorite , geology , mössbauer spectroscopy , feldspar , geochemistry , weathering , mineralogy , astrobiology , olivine , regolith , materials science , chemistry , paleontology , physics , quartz , optoelectronics , luminescence , crystallography
Mössbauer and thermoluminescence (TL) data have elucidated the terrestrial histories of five equilibrated chondrites, of petrologic types 5 and 6, collected on blue ice fields near Frontier Mountain in Antarctica. Mössbauer spectroscopy substantially reflects the destruction of iron‐bearing species with formation of finely divided aggregates of iron oxides or oxyhydroxides. TL sensitivity reflects the possible coating of the feldspar grains due to the iron oxide mobility during progressive weathering.

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