Seismic Volcanostratigraphy: The Key to Resolving the Jan Mayen Microcontinent and Iceland Plateau Rift Evolution-Reference-Cited by-同舟云学术

Seismic Volcanostratigraphy: The Key to Resolving the Jan Mayen Microcontinent and Iceland Plateau Rift Evolution

Published:2022-04 Issue:4 Volume:23 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

Blischke Anett¹²^ORCID,Brandsdóttir Bryndís¹^ORCID,Stoker Martyn S.³^ORCID,Gaina Carmen⁴⁵^ORCID,Erlendsson Ögmundur⁶^ORCID,Tegner Christian⁷^ORCID,Halldórsson Sæmundur A.¹^ORCID,Helgadóttir Helga M.⁶^ORCID,Gautason Bjarni²^ORCID,Planke Sverre⁴⁸^ORCID,Koppers Anthony A. P.⁹^ORCID,Hopper John R.¹⁰^ORCID

Affiliation:

1. Institute of Earth Sciences Science Institute University of Iceland – Askja Reykjavík Iceland

2. Iceland GeoSurvey Akureyri Iceland

3. Australian School of Petroleum and Energy Resources University of Adelaide Adelaide SA Australia

4. Centre for Earth Evolution and Dynamics (CEED) University of Oslo Oslo Norway

5. School of Earth and Atmospheric Sciences Queensland University of Technology Brisbane QLD Australia

6. Iceland GeoSurvey Reykjavík Iceland

7. Department of Geoscience—Earth System Petrology Aarhus University Aarhus C Denmark

8. Volcanic Basin Petroleum Research AS Oslo Norway

9. College of Earth, Ocean and Atmospheric Sciences Oregon State University Corvallis OR USA

10. Geological Survey of Denmark and Greenland (GEUS) Copenhagen Denmark

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GC009948

Reference255 articles.

1. Pre-breakup magmatism on the Vøring Margin: Insight from new sub-basalt imaging and results from Ocean Drilling Program Hole 642E

2. The development of volcanic sequences at rifted margins: New insights from the structure and morphology of the Vøring Escarpment, mid-Norwegian Margin

3. Seismic volcanostratigraphy of the Norwegian Margin: constraints on tectonomagmatic break-up processes

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