A NEW TECTONIC CHART OF THE ARCTIC
On the tectonic chart, that great part of the Arctic and sub-Arctic territory where the crust is of continental type is subdivided into fold systems, recent geosynclines and parageosynclines. The fold systems in their turn are subdivided into two groups, basically as follows: PreCambrian systems, wh...
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ftdtic:AD0610386 2023-05-15T14:46:38+02:00 A NEW TECTONIC CHART OF THE ARCTIC ATLASOV,I. P. Vakar,V. A. Dibner,V. D. Egyazarov,B. Kh. zimkin,A. B. DIRECTORATE OF SCIENTIFIC INFORMATION SERVICES OTTAWA (ONTARIO) 1964-08 text/html http://www.dtic.mil/docs/citations/AD0610386 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0610386 en eng http://www.dtic.mil/docs/citations/AD0610386 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS STRUCTURAL GEOLOGY ARCTIC OCEAN USSR FAULTS(GEOLOGY) FOLDS(GEOLOGY) OCEAN BOTTOM TOPOGRAPHY Text 1964 ftdtic 2016-02-21T19:04:26Z On the tectonic chart, that great part of the Arctic and sub-Arctic territory where the crust is of continental type is subdivided into fold systems, recent geosynclines and parageosynclines. The fold systems in their turn are subdivided into two groups, basically as follows: PreCambrian systems, which have passed through the stage of postgeosynclinal development have been converted into platforms; Paleozoic and Mesozoic systems, still in the stage of post-geosynclinal development. The recent geosynclines are subdivided into two groups: mature geosynclines --- Cenozoic fold systems that have entered (or are entering) into the stage of post-geosynclinal development; young geosynclines, still in the initial stages of geosynclinal development, and related to geostructures of oceanic type. The parageosynclines are subdivided on the chart into three groups: peripheral parageosynclines --- zones of geosynclines formed in marginal downwarps, in foredeeps, and in part in submontane downwarps; internal parageosynclines, associated with the central massifs found in the interior of folded regions; finally, certain oceanic depressions with protracted and intense subsidence. Trans. of Akademiya Nauk SSSR. Doklady, 1964, v. 156, no. 6, p. 1341-1342. Also available from the National Research Council of Canada, Ottawa (Ontario) as C-5040. Text Arctic Arctic Ocean Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean Canada |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
STRUCTURAL GEOLOGY ARCTIC OCEAN USSR FAULTS(GEOLOGY) FOLDS(GEOLOGY) OCEAN BOTTOM TOPOGRAPHY |
spellingShingle |
STRUCTURAL GEOLOGY ARCTIC OCEAN USSR FAULTS(GEOLOGY) FOLDS(GEOLOGY) OCEAN BOTTOM TOPOGRAPHY ATLASOV,I. P. Vakar,V. A. Dibner,V. D. Egyazarov,B. Kh. zimkin,A. B. A NEW TECTONIC CHART OF THE ARCTIC |
topic_facet |
STRUCTURAL GEOLOGY ARCTIC OCEAN USSR FAULTS(GEOLOGY) FOLDS(GEOLOGY) OCEAN BOTTOM TOPOGRAPHY |
description |
On the tectonic chart, that great part of the Arctic and sub-Arctic territory where the crust is of continental type is subdivided into fold systems, recent geosynclines and parageosynclines. The fold systems in their turn are subdivided into two groups, basically as follows: PreCambrian systems, which have passed through the stage of postgeosynclinal development have been converted into platforms; Paleozoic and Mesozoic systems, still in the stage of post-geosynclinal development. The recent geosynclines are subdivided into two groups: mature geosynclines --- Cenozoic fold systems that have entered (or are entering) into the stage of post-geosynclinal development; young geosynclines, still in the initial stages of geosynclinal development, and related to geostructures of oceanic type. The parageosynclines are subdivided on the chart into three groups: peripheral parageosynclines --- zones of geosynclines formed in marginal downwarps, in foredeeps, and in part in submontane downwarps; internal parageosynclines, associated with the central massifs found in the interior of folded regions; finally, certain oceanic depressions with protracted and intense subsidence. Trans. of Akademiya Nauk SSSR. Doklady, 1964, v. 156, no. 6, p. 1341-1342. Also available from the National Research Council of Canada, Ottawa (Ontario) as C-5040. |
author2 |
DIRECTORATE OF SCIENTIFIC INFORMATION SERVICES OTTAWA (ONTARIO) |
format |
Text |
author |
ATLASOV,I. P. Vakar,V. A. Dibner,V. D. Egyazarov,B. Kh. zimkin,A. B. |
author_facet |
ATLASOV,I. P. Vakar,V. A. Dibner,V. D. Egyazarov,B. Kh. zimkin,A. B. |
author_sort |
ATLASOV,I. P. |
title |
A NEW TECTONIC CHART OF THE ARCTIC |
title_short |
A NEW TECTONIC CHART OF THE ARCTIC |
title_full |
A NEW TECTONIC CHART OF THE ARCTIC |
title_fullStr |
A NEW TECTONIC CHART OF THE ARCTIC |
title_full_unstemmed |
A NEW TECTONIC CHART OF THE ARCTIC |
title_sort |
new tectonic chart of the arctic |
publishDate |
1964 |
url |
http://www.dtic.mil/docs/citations/AD0610386 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0610386 |
geographic |
Arctic Arctic Ocean Canada |
geographic_facet |
Arctic Arctic Ocean Canada |
genre |
Arctic Arctic Ocean |
genre_facet |
Arctic Arctic Ocean |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0610386 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766317840266166272 |