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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Bibliographic Details
Main Author: Ry S
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
12
4C
2
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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Summary: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