P ch, J te U
Au water depths to ∼450 m and 750 m have been indicated by geophysical Ridge that is truncated to water depths of almost 1000 m along a stretch of ∼60 km at the very center of the Arctic origin. Similar erosional features are found over a much larger area on the Chukchi Borderland, which extends int...
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.538.1725 http://sci.odu.edu/oceanography/directory/faculty/darby/publications/Polyak_eta_QR_2007.pdf |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.538.1725 2023-05-15T14:57:32+02:00 P ch, J te U Ry S The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.538.1725 http://sci.odu.edu/oceanography/directory/faculty/darby/publications/Polyak_eta_QR_2007.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.538.1725 http://sci.odu.edu/oceanography/directory/faculty/darby/publications/Polyak_eta_QR_2007.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://sci.odu.edu/oceanography/directory/faculty/darby/publications/Polyak_eta_QR_2007.pdf YQRES-02755 No. of pages 12 4C 2 text ftciteseerx 2016-01-08T10:54:37Z Au water depths to ∼450 m and 750 m have been indicated by geophysical Ridge that is truncated to water depths of almost 1000 m along a stretch of ∼60 km at the very center of the Arctic origin. Similar erosional features are found over a much larger area on the Chukchi Borderland, which extends into the interior of the Amerasia Basin (Fig. 1A) (Polyak et al., 2001; Jakobsson et al., 2005). These features include sets of (20 + model Text Arctic Chukchi Unknown Arctic Amerasia Basin ENVELOPE(-170.000,-170.000,80.000,80.000) Chukchi Borderland ENVELOPE(-165.000,-165.000,77.000,77.000) |
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YQRES-02755 No. of pages 12 4C 2 |
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YQRES-02755 No. of pages 12 4C 2 Ry S P ch, J te U |
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YQRES-02755 No. of pages 12 4C 2 |
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Au water depths to ∼450 m and 750 m have been indicated by geophysical Ridge that is truncated to water depths of almost 1000 m along a stretch of ∼60 km at the very center of the Arctic origin. Similar erosional features are found over a much larger area on the Chukchi Borderland, which extends into the interior of the Amerasia Basin (Fig. 1A) (Polyak et al., 2001; Jakobsson et al., 2005). These features include sets of (20 + model |
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The Pennsylvania State University CiteSeerX Archives |
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Ry S |
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P ch, J te U |
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P ch, J te U |
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P ch, J te U |
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P ch, J te U |
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P ch, J te U |
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p ch, j te u |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.538.1725 http://sci.odu.edu/oceanography/directory/faculty/darby/publications/Polyak_eta_QR_2007.pdf |
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ENVELOPE(-170.000,-170.000,80.000,80.000) ENVELOPE(-165.000,-165.000,77.000,77.000) |
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Arctic Amerasia Basin Chukchi Borderland |
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Arctic Amerasia Basin Chukchi Borderland |
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Arctic Chukchi |
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Arctic Chukchi |
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