SOME DATA ON THE PALEOMAGNETISM OF THE LOWER CARBONIFEROUS ROCKS IN THE MINUSINSK BASIN
Paleomagnetism, a new and rapidly developing branch of geophysics, is the study of the history of the geomagnetic field on the basis of natural remanent rock magnetism. The present paper describes the results of a paleomagnetic research on Lower Carboniferous sedimentary rocks, the purpose of which...
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ftdtic:AD0654480 2023-05-15T17:05:29+02:00 SOME DATA ON THE PALEOMAGNETISM OF THE LOWER CARBONIFEROUS ROCKS IN THE MINUSINSK BASIN Vlasov,A. Ya. Kovalenko,G. V. Popova,A. V. DIRECTORATE OF SCIENTIFIC INFORMATION SERVICES OTTAWA (ONTARIO) 1967-05 text/html http://www.dtic.mil/docs/citations/AD0654480 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0654480 en eng http://www.dtic.mil/docs/citations/AD0654480 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Geomagnetism Geology Geochemistry and Mineralogy (*SEDIMENTARY ROCK *GEOMAGNETISM) (*PALEONTOLOGY *MAGNETIC PROPERTIES) DEPOSITS SAMPLING MAGNETIC FIELDS STRATIGRAPHY THICKNESS STABILITY ROCK MATHEMATICAL ANALYSIS SEDIMENTATION TABLES(DATA) RIVERS MEASUREMENT SANDSTONE MAGNETOMETERS USSR Text 1967 ftdtic 2016-02-18T20:13:52Z Paleomagnetism, a new and rapidly developing branch of geophysics, is the study of the history of the geomagnetic field on the basis of natural remanent rock magnetism. The present paper describes the results of a paleomagnetic research on Lower Carboniferous sedimentary rocks, the purpose of which was to establish the positions of the geomagnetic poles during the said geological period. The selection of orientated samples was made in the Minusinsk Basin region (southern part of the Krasnoyarsk Krai). The Lower Carboniferous is here represented by a complex of variegated rocks, known as the Minusinsk Suite. The thickness of the suite has been set at 1200-1500 m. The rock samples were selected according to established procedure (1, 2) from natural outcrops. The Lower Carboniferous sedimentary rocks were represented, in these outcrops, by red and grey sandstones and aleurolites. The remanent magnetization and the magnetic susceptibility of the samples were measured by means of an astatic magnetometer. (Author) Trans. of Geologiya i Geofizika (USSR), n9 p112-4 1961. Text Krasnoyarsk Krai Defense Technical Information Center: DTIC Technical Reports database |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
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ftdtic |
language |
English |
topic |
Geomagnetism Geology Geochemistry and Mineralogy (*SEDIMENTARY ROCK *GEOMAGNETISM) (*PALEONTOLOGY *MAGNETIC PROPERTIES) DEPOSITS SAMPLING MAGNETIC FIELDS STRATIGRAPHY THICKNESS STABILITY ROCK MATHEMATICAL ANALYSIS SEDIMENTATION TABLES(DATA) RIVERS MEASUREMENT SANDSTONE MAGNETOMETERS USSR |
spellingShingle |
Geomagnetism Geology Geochemistry and Mineralogy (*SEDIMENTARY ROCK *GEOMAGNETISM) (*PALEONTOLOGY *MAGNETIC PROPERTIES) DEPOSITS SAMPLING MAGNETIC FIELDS STRATIGRAPHY THICKNESS STABILITY ROCK MATHEMATICAL ANALYSIS SEDIMENTATION TABLES(DATA) RIVERS MEASUREMENT SANDSTONE MAGNETOMETERS USSR Vlasov,A. Ya. Kovalenko,G. V. Popova,A. V. SOME DATA ON THE PALEOMAGNETISM OF THE LOWER CARBONIFEROUS ROCKS IN THE MINUSINSK BASIN |
topic_facet |
Geomagnetism Geology Geochemistry and Mineralogy (*SEDIMENTARY ROCK *GEOMAGNETISM) (*PALEONTOLOGY *MAGNETIC PROPERTIES) DEPOSITS SAMPLING MAGNETIC FIELDS STRATIGRAPHY THICKNESS STABILITY ROCK MATHEMATICAL ANALYSIS SEDIMENTATION TABLES(DATA) RIVERS MEASUREMENT SANDSTONE MAGNETOMETERS USSR |
description |
Paleomagnetism, a new and rapidly developing branch of geophysics, is the study of the history of the geomagnetic field on the basis of natural remanent rock magnetism. The present paper describes the results of a paleomagnetic research on Lower Carboniferous sedimentary rocks, the purpose of which was to establish the positions of the geomagnetic poles during the said geological period. The selection of orientated samples was made in the Minusinsk Basin region (southern part of the Krasnoyarsk Krai). The Lower Carboniferous is here represented by a complex of variegated rocks, known as the Minusinsk Suite. The thickness of the suite has been set at 1200-1500 m. The rock samples were selected according to established procedure (1, 2) from natural outcrops. The Lower Carboniferous sedimentary rocks were represented, in these outcrops, by red and grey sandstones and aleurolites. The remanent magnetization and the magnetic susceptibility of the samples were measured by means of an astatic magnetometer. (Author) Trans. of Geologiya i Geofizika (USSR), n9 p112-4 1961. |
author2 |
DIRECTORATE OF SCIENTIFIC INFORMATION SERVICES OTTAWA (ONTARIO) |
format |
Text |
author |
Vlasov,A. Ya. Kovalenko,G. V. Popova,A. V. |
author_facet |
Vlasov,A. Ya. Kovalenko,G. V. Popova,A. V. |
author_sort |
Vlasov,A. Ya. |
title |
SOME DATA ON THE PALEOMAGNETISM OF THE LOWER CARBONIFEROUS ROCKS IN THE MINUSINSK BASIN |
title_short |
SOME DATA ON THE PALEOMAGNETISM OF THE LOWER CARBONIFEROUS ROCKS IN THE MINUSINSK BASIN |
title_full |
SOME DATA ON THE PALEOMAGNETISM OF THE LOWER CARBONIFEROUS ROCKS IN THE MINUSINSK BASIN |
title_fullStr |
SOME DATA ON THE PALEOMAGNETISM OF THE LOWER CARBONIFEROUS ROCKS IN THE MINUSINSK BASIN |
title_full_unstemmed |
SOME DATA ON THE PALEOMAGNETISM OF THE LOWER CARBONIFEROUS ROCKS IN THE MINUSINSK BASIN |
title_sort |
some data on the paleomagnetism of the lower carboniferous rocks in the minusinsk basin |
publishDate |
1967 |
url |
http://www.dtic.mil/docs/citations/AD0654480 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0654480 |
genre |
Krasnoyarsk Krai |
genre_facet |
Krasnoyarsk Krai |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0654480 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766060012644335616 |