Recognition of the geologic framework of porphyry deposits on ERTS-1 imagery

The author has identified the following significant results. Photointerpretation methods have been most successfully applied in the less vegetated test sites where several previously unknown geologic features have been recognized and known ones extended. Northwest mid-Tertiary faults in the ELY, Nev...

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Main Author: Wilson, J. C.
Format: Other/Unknown Material
Language:unknown
Published: 1973
Subjects:
Online Access:http://hdl.handle.net/2060/19730017635
id ftnasantrs:oai:casi.ntrs.nasa.gov:19730017635
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spelling ftnasantrs:oai:casi.ntrs.nasa.gov:19730017635 2023-05-15T18:31:19+02:00 Recognition of the geologic framework of porphyry deposits on ERTS-1 imagery Wilson, J. C. Unclassified, Unlimited, Publicly available Jul 12, 1973 application/pdf http://hdl.handle.net/2060/19730017635 unknown Document ID: 19730017635 Accession ID: 73N26362 http://hdl.handle.net/2060/19730017635 No Copyright CASI GEOPHYSICS E73-10762 NASA-CR-132204 1973 ftnasantrs 2019-07-21T05:37:07Z The author has identified the following significant results. Photointerpretation methods have been most successfully applied in the less vegetated test sites where several previously unknown geologic features have been recognized and known ones extended. Northwest mid-Tertiary faults in the ELY, Nevada area are observed to offset north-trending ranges and abruptly terminate older Mesozoic structures. In the Ray, Arizona area the observed patterns of fault and fracture systems appear to be related to the locations of known porphyry copper deposits. In the Tanacross, Alaska area a number of regional circular features observed may represent near surface intrusions and, therefore, permissive environments for copper porphyries. Other/Unknown Material Tanacross Alaska NASA Technical Reports Server (NTRS)
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic GEOPHYSICS
spellingShingle GEOPHYSICS
Wilson, J. C.
Recognition of the geologic framework of porphyry deposits on ERTS-1 imagery
topic_facet GEOPHYSICS
description The author has identified the following significant results. Photointerpretation methods have been most successfully applied in the less vegetated test sites where several previously unknown geologic features have been recognized and known ones extended. Northwest mid-Tertiary faults in the ELY, Nevada area are observed to offset north-trending ranges and abruptly terminate older Mesozoic structures. In the Ray, Arizona area the observed patterns of fault and fracture systems appear to be related to the locations of known porphyry copper deposits. In the Tanacross, Alaska area a number of regional circular features observed may represent near surface intrusions and, therefore, permissive environments for copper porphyries.
format Other/Unknown Material
author Wilson, J. C.
author_facet Wilson, J. C.
author_sort Wilson, J. C.
title Recognition of the geologic framework of porphyry deposits on ERTS-1 imagery
title_short Recognition of the geologic framework of porphyry deposits on ERTS-1 imagery
title_full Recognition of the geologic framework of porphyry deposits on ERTS-1 imagery
title_fullStr Recognition of the geologic framework of porphyry deposits on ERTS-1 imagery
title_full_unstemmed Recognition of the geologic framework of porphyry deposits on ERTS-1 imagery
title_sort recognition of the geologic framework of porphyry deposits on erts-1 imagery
publishDate 1973
url http://hdl.handle.net/2060/19730017635
op_coverage Unclassified, Unlimited, Publicly available
genre Tanacross
Alaska
genre_facet Tanacross
Alaska
op_source CASI
op_relation Document ID: 19730017635
Accession ID: 73N26362
http://hdl.handle.net/2060/19730017635
op_rights No Copyright
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