The read-out system of spatial distribution of thermoluminescence in meteorites

The thermoluminescence (TL) technique used for dating the terrestrial age of meteorites is based on the TL fading of interior samples. The depth dependence of the TL for Antarctic meteorites with fusion crust is measured. Usually, meteorites are powdered and their TL measured under a photomultiplier...

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Main Authors: Takaoka, N., Takano, Y., Ninagawa, K., Yamamoto, I., Wada, T., Yamashita, Y.
Format: Other/Unknown Material
Language:unknown
Published: 1985
Subjects:
SPACE RADIATION
Antarctic
Antarc*
Online Access:http://hdl.handle.net/2060/19850026818
id ftnasantrs:oai:casi.ntrs.nasa.gov:19850026818
record_format openpolar
spelling ftnasantrs:oai:casi.ntrs.nasa.gov:19850026818 2023-05-15T13:58:36+02:00 The read-out system of spatial distribution of thermoluminescence in meteorites Takaoka, N. Takano, Y. Ninagawa, K. Yamamoto, I. Wada, T. Yamashita, Y. Unclassified, Unlimited, Publicly available Aug 1, 1985 application/pdf http://hdl.handle.net/2060/19850026818 unknown Document ID: 19850026818 Accession ID: 85N35131 http://hdl.handle.net/2060/19850026818 No Copyright CASI SPACE RADIATION SH-9.1-16 19th Intern. Cosmic Ray Conf - Vol. 5; p 514-517; NASA-CP-2376-VOL-5 1985 ftnasantrs 2019-07-21T09:45:09Z The thermoluminescence (TL) technique used for dating the terrestrial age of meteorites is based on the TL fading of interior samples. The depth dependence of the TL for Antarctic meteorites with fusion crust is measured. Usually, meteorites are powdered and their TL measured under a photomultiplier. In this case, a TL spatial distribution of a cross section of antarctic meteorites is measured using a read out system of spatial distribution of TL, since a meteorite is made up of inhomogeneous material. Antarctic meteorites MET-78028(L6) and ALH-77278(L13) are used. Other/Unknown Material Antarc* Antarctic NASA Technical Reports Server (NTRS) Antarctic
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic SPACE RADIATION
spellingShingle SPACE RADIATION
Takaoka, N.
Takano, Y.
Ninagawa, K.
Yamamoto, I.
Wada, T.
Yamashita, Y.
The read-out system of spatial distribution of thermoluminescence in meteorites
topic_facet SPACE RADIATION
description The thermoluminescence (TL) technique used for dating the terrestrial age of meteorites is based on the TL fading of interior samples. The depth dependence of the TL for Antarctic meteorites with fusion crust is measured. Usually, meteorites are powdered and their TL measured under a photomultiplier. In this case, a TL spatial distribution of a cross section of antarctic meteorites is measured using a read out system of spatial distribution of TL, since a meteorite is made up of inhomogeneous material. Antarctic meteorites MET-78028(L6) and ALH-77278(L13) are used.
format Other/Unknown Material
author Takaoka, N.
Takano, Y.
Ninagawa, K.
Yamamoto, I.
Wada, T.
Yamashita, Y.
author_facet Takaoka, N.
Takano, Y.
Ninagawa, K.
Yamamoto, I.
Wada, T.
Yamashita, Y.
author_sort Takaoka, N.
title The read-out system of spatial distribution of thermoluminescence in meteorites
title_short The read-out system of spatial distribution of thermoluminescence in meteorites
title_full The read-out system of spatial distribution of thermoluminescence in meteorites
title_fullStr The read-out system of spatial distribution of thermoluminescence in meteorites
title_full_unstemmed The read-out system of spatial distribution of thermoluminescence in meteorites
title_sort read-out system of spatial distribution of thermoluminescence in meteorites
publishDate 1985
url http://hdl.handle.net/2060/19850026818
op_coverage Unclassified, Unlimited, Publicly available
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source CASI
op_relation Document ID: 19850026818
Accession ID: 85N35131
http://hdl.handle.net/2060/19850026818
op_rights No Copyright
_version_ 1766266965636153344

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