Some Features of the Yamato-74013 Diogenite: The Opaque Minerals and the Abundances of Some Trace Elements

In a standard mineralogical-petrological microscopic examination of the Yamato-74013 diogenite attention was given to the opaque minerals, chromite and troilite. Iron-deficient sulphides are supposed to be responsible for some features observed on the thermomagnetic curves. Abundances of Sc, Co, Hg...

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Bibliographic Details
Main Authors: Bruno Lang, Jadwiga Synowiec, Andrzej Pietruszewski, Malgorzata Suplinska, Elzbieta Krol
Format: Report
Language:English
Published: Department of Chemistry, Warsaw University/Department of Chemistry, Warsaw University/Central Laboratory for Radiological Protection/Central Laboratory for Radiological Protection/Institute of Geophysics of the Polish Academy of Sciences 1980
Subjects:
Yamato
Memoirs of National Institute of Polar Research
Polar Research
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=1094
http://id.nii.ac.jp/1291/00001094/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=1094&item_no=1&attribute_id=18&file_no=1
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Summary:In a standard mineralogical-petrological microscopic examination of the Yamato-74013 diogenite attention was given to the opaque minerals, chromite and troilite. Iron-deficient sulphides are supposed to be responsible for some features observed on the thermomagnetic curves. Abundances of Sc, Co, Hg and Zn were determined with INAA and AA.

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