Unexpected postglacial faulting in passive continental margins: Storfjorden glacial trough, Barents Sea-Reference-Cited by-同舟云学术

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Unexpected postglacial faulting in passive continental margins: Storfjorden glacial trough, Barents Sea

Published:2024-02 Issue: Volume:873 Page:230217
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Pedrosa-González María Teresa,Galindo-Zaldivar Jesús,González-Castillo Lourdes,Ercilla Gemma

Publisher

Elsevier BV

Reference110 articles.

1. Possible role for tectonics in the evolving stability of the Greenland Ice Sheet;Alley;J. Geophys. Res. Earth,2019

2. Sedimentation beneath ice shelves—the view from ice stream B;Alley;Mar. Geol.,1989

3. The Dynamics of Faulting and Dyke Formation with Applications to Britain;Anderson,1951

4. Fennoscandian earthquakes: whole crustal rupturing related to postglacial rebound;Arvidsson;Science,1996

5. Submarine moraines in Southeast Greenland fjords reveal contrasting outlet-glacier behavior since the last Glacial Maximum;Batchelor;Geophys. Res. Lett.,2019

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