Relative motions between Eurasia and North America in the Bering Sea region
Knowledge of the relative motion of the North American and Eurasian plates during the late Mesozoic and Cenozoic provides insight into the observed timing and style of deformational events in the Bering Sea region. Periods of strong convergence from ≈ 70 to ≈ 50 Ma (Maastrichtian to Paleocene) are c...
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ftunivpittsburgh:oai:d-scholarship.pitt.edu:13589 2023-09-05T13:11:48+02:00 Relative motions between Eurasia and North America in the Bering Sea region Harbert, W Frei, LS Cox, A Engebretson, DC 1987-03-15 text/plain http://d-scholarship.pitt.edu/13589/ http://d-scholarship.pitt.edu/13589/1/licence.txt en eng http://d-scholarship.pitt.edu/13589/1/licence.txt Harbert, W and Frei, LS and Cox, A and Engebretson, DC (1987) Relative motions between Eurasia and North America in the Bering Sea region. Tectonophysics, 134 (4). 239 - 261. ISSN 0040-1951 attached Article PeerReviewed 1987 ftunivpittsburgh 2023-08-14T17:31:08Z Knowledge of the relative motion of the North American and Eurasian plates during the late Mesozoic and Cenozoic provides insight into the observed timing and style of deformational events in the Bering Sea region. Periods of strong convergence from ≈ 70 to ≈ 50 Ma (Maastrichtian to Paleocene) are correlated with compressional deformation between the Chukotsk Peninsula and northern Alaska and movement along the Denali fault. The convergence may also be the cause of a previously proposed counterclockwise rotation of western Alaska. Transform motion between these plates from 50 to 38 Ma (Middle to Late Eocene) correlates with subsidence of the Bering Shelf, creation of a series of pull-apart basins along the Bering margin and cessation of calc-alkaline volcanism in western Alaska. Slight compressive convergence from 37 Ma to the present may be responsible for the anticlinal deformation of basin filling sediments in the Anadyr and Khatyrka basins. © 1987. Article in Journal/Newspaper Anadyr Anadyr' Bering Sea Alaska University of Pittsburgh: D-Scholarship@Pitt Bering Sea Anadyr ENVELOPE(177.510,177.510,64.734,64.734) Anadyr’ ENVELOPE(176.233,176.233,64.882,64.882) Bering Shelf ENVELOPE(-170.783,-170.783,60.128,60.128) Khatyrka ENVELOPE(175.288,175.288,62.062,62.062) |
institution |
Open Polar |
collection |
University of Pittsburgh: D-Scholarship@Pitt |
op_collection_id |
ftunivpittsburgh |
language |
English |
description |
Knowledge of the relative motion of the North American and Eurasian plates during the late Mesozoic and Cenozoic provides insight into the observed timing and style of deformational events in the Bering Sea region. Periods of strong convergence from ≈ 70 to ≈ 50 Ma (Maastrichtian to Paleocene) are correlated with compressional deformation between the Chukotsk Peninsula and northern Alaska and movement along the Denali fault. The convergence may also be the cause of a previously proposed counterclockwise rotation of western Alaska. Transform motion between these plates from 50 to 38 Ma (Middle to Late Eocene) correlates with subsidence of the Bering Shelf, creation of a series of pull-apart basins along the Bering margin and cessation of calc-alkaline volcanism in western Alaska. Slight compressive convergence from 37 Ma to the present may be responsible for the anticlinal deformation of basin filling sediments in the Anadyr and Khatyrka basins. © 1987. |
format |
Article in Journal/Newspaper |
author |
Harbert, W Frei, LS Cox, A Engebretson, DC |
spellingShingle |
Harbert, W Frei, LS Cox, A Engebretson, DC Relative motions between Eurasia and North America in the Bering Sea region |
author_facet |
Harbert, W Frei, LS Cox, A Engebretson, DC |
author_sort |
Harbert, W |
title |
Relative motions between Eurasia and North America in the Bering Sea region |
title_short |
Relative motions between Eurasia and North America in the Bering Sea region |
title_full |
Relative motions between Eurasia and North America in the Bering Sea region |
title_fullStr |
Relative motions between Eurasia and North America in the Bering Sea region |
title_full_unstemmed |
Relative motions between Eurasia and North America in the Bering Sea region |
title_sort |
relative motions between eurasia and north america in the bering sea region |
publishDate |
1987 |
url |
http://d-scholarship.pitt.edu/13589/ http://d-scholarship.pitt.edu/13589/1/licence.txt |
long_lat |
ENVELOPE(177.510,177.510,64.734,64.734) ENVELOPE(176.233,176.233,64.882,64.882) ENVELOPE(-170.783,-170.783,60.128,60.128) ENVELOPE(175.288,175.288,62.062,62.062) |
geographic |
Bering Sea Anadyr Anadyr’ Bering Shelf Khatyrka |
geographic_facet |
Bering Sea Anadyr Anadyr’ Bering Shelf Khatyrka |
genre |
Anadyr Anadyr' Bering Sea Alaska |
genre_facet |
Anadyr Anadyr' Bering Sea Alaska |
op_relation |
http://d-scholarship.pitt.edu/13589/1/licence.txt Harbert, W and Frei, LS and Cox, A and Engebretson, DC (1987) Relative motions between Eurasia and North America in the Bering Sea region. Tectonophysics, 134 (4). 239 - 261. ISSN 0040-1951 |
op_rights |
attached |
_version_ |
1776197095834779648 |