et al.

The southern Koryak Upland located north and northwest of the Olyutor zone composed of Upper Cre-taceous siliceous–volcanogenic sequences (Bogdanov et al., 1987) hosts the Ukelayat trough (Central Koryak structural-facies zone) (Ermakov and Suprunenko, 1975). The trough is filled with highly deforme...

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Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published:
Subjects:
Ukelayat
Koryak
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.616.4720
http://earth.geology.yale.edu/~brandon/Eprints/Shapiro_etal2001_KamchatkaZirconFT.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.616.4720 2023-05-15T17:05:19+02:00 et al. The Pennsylvania State University CiteSeerX Archives 24 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.616.4720 http://earth.geology.yale.edu/~brandon/Eprints/Shapiro_etal2001_KamchatkaZirconFT.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.616.4720 http://earth.geology.yale.edu/~brandon/Eprints/Shapiro_etal2001_KamchatkaZirconFT.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://earth.geology.yale.edu/~brandon/Eprints/Shapiro_etal2001_KamchatkaZirconFT.pdf text ftciteseerx 2016-01-08T14:46:02Z The southern Koryak Upland located north and northwest of the Olyutor zone composed of Upper Cre-taceous siliceous–volcanogenic sequences (Bogdanov et al., 1987) hosts the Ukelayat trough (Central Koryak structural-facies zone) (Ermakov and Suprunenko, 1975). The trough is filled with highly deformed Upper Cretaceous and Lower Paleogene sandy–shaly sequences frequently of the flyschlike appearance (Ermakov Text Koryak Unknown Ukelayat ENVELOPE(173.467,173.467,61.717,61.717)
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description The southern Koryak Upland located north and northwest of the Olyutor zone composed of Upper Cre-taceous siliceous–volcanogenic sequences (Bogdanov et al., 1987) hosts the Ukelayat trough (Central Koryak structural-facies zone) (Ermakov and Suprunenko, 1975). The trough is filled with highly deformed Upper Cretaceous and Lower Paleogene sandy–shaly sequences frequently of the flyschlike appearance (Ermakov
author2 The Pennsylvania State University CiteSeerX Archives
format Text
title et al.
spellingShingle et al.
title_short et al.
title_full et al.
title_fullStr et al.
title_full_unstemmed et al.
title_sort et al.
publishDate
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.616.4720
http://earth.geology.yale.edu/~brandon/Eprints/Shapiro_etal2001_KamchatkaZirconFT.pdf
long_lat ENVELOPE(173.467,173.467,61.717,61.717)
geographic Ukelayat
geographic_facet Ukelayat
genre Koryak
genre_facet Koryak
op_source http://earth.geology.yale.edu/~brandon/Eprints/Shapiro_etal2001_KamchatkaZirconFT.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.616.4720
http://earth.geology.yale.edu/~brandon/Eprints/Shapiro_etal2001_KamchatkaZirconFT.pdf
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