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Thermal Metamorphism of Primitive Meteorites - X. Additional Trace Elements in Allende (C3V) heated to 1400 CShow simple item record

dc.creatorNgo, H. T.
dc.creatorLipschutz, Michael E.
dc.date.accessioned2023-02-14T17:43:56Z
dc.date.available2023-02-14T17:43:56Z
dc.date.issued1980-01-10
dc.identifier.urihttps://repository.tcu.edu/handle/116099117/57140
dc.descriptionArticle focused on comparing elemental retentivity between samples from the Allende and Murchison stones when heated to high temperatures. Concludes that the broad differences demonstrates vastly different compositions.
dc.relationOscar Monnig Papers (MS 124)
dc.rightsPrior written permission from TCU Special Collections required to use any document or photograph.
dc.sourceBox 05, Allende-Parralde Chihuhua-Mexico folder
dc.subjectMeteorite
dc.subjectAllende (Mexico)
dc.subjectAbee stone
dc.subjectKrymka
dc.subjectTieschitz
dc.subjectMurchison (Victoria, Australia)
dc.subjectEnstatite chondrite
dc.subjectAchondrite
dc.subjectCarbonaceous chondrite
dc.subjectArsenic
dc.subjectCopper
dc.subjectRubidium
dc.subjectAntimony
dc.subjectGeochimica et Cosmochimica Acta
dc.titleThermal Metamorphism of Primitive Meteorites - X. Additional Trace Elements in Allende (C3V) heated to 1400 C
dc.typeDocument
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This item appears in the following Collection(s)
  • Records of the Monnig Meteorite Gallery [2825]
    The files are arranged alphabetically, usually according to the location of discovery of the meteorite. The files contain correspondence and research material on the meteorites in the collection.

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