Influence of 3D Earth Structure on Glacial Isostatic Adjustment in the Russian Arctic-Reference-Cited by-同舟云学术

Influence of 3D Earth Structure on Glacial Isostatic Adjustment in the Russian Arctic

Published:2022-03 Issue:3 Volume:127 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Li Tanghua¹^ORCID,Khan Nicole S.²^ORCID,Baranskaya Alisa V.³,Shaw Timothy A.¹^ORCID,Peltier W. Richard⁴^ORCID,Stuhne Gordan R.⁴^ORCID,Wu Patrick⁵^ORCID,Horton Benjamin P.¹⁶^ORCID

Affiliation:

1. Earth Observatory of Singapore Nanyang Technological University Singapore Singapore

2. Department of Earth Sciences and the Swire Institute of Marine Science University of Hong Kong Hong Kong Hong Kong

3. Lomonosov Moscow State University Laboratory of Geoecology of the North Moscow Russia

4. Department of Physics University of Toronto Toronto Ontario Canada

5. Department of Geoscience University of Calgary Calgary AB Canada

6. Asian School of the Environment Nanyang Technological University Singapore Singapore

Funder

Ministry of Education - Singapore

National Research Foundation Singapore

Natural Sciences and Engineering Research Council of Canada

Russian Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JB023631

Reference55 articles.

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2. Glacial isostatic adjustment associated with the Barents Sea ice sheet: A modelling inter-comparison

3. Baranskaya A.V.(2015). The role of the latest tectonic movements in the formation of the relief of the coasts of the Russian Arctic.Summary of the thesis for a degree of Doctor of Philosophy (geographical science) speciality 25.00.25 ‐ geomorphology and evolutional geography (PhD Thesis). Saint Petersburg State University. Saint‐Petersburg. pp. 26. (In Russian).

4. A postglacial relative sea-level database for the Russian Arctic coast

5. Joint inversion for global isotropic and radially anisotropic mantle structure including crustal thickness perturbations

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