Výsledky vyhledávání - "Julie Linnéa Sehested Gresseth"

Footwall geomorphology during necking domain evolution: A new model for the Frøya High, mid‐ N orwegian rifted margin

Autor: Julie Linnéa Sehested Gresseth, Per Terje Osmundsen, Gwenn Péron‐Pinvidic

Publikováno v: Basin Research.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::14ff4740a02b57ff42653d4c8069f05f
https://doi.org/10.1111/bre.12775

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Late Paleozoic supradetachment basin configuration in the southwestern Barents Sea—Intrabasement seismic facies of the Fingerdjupet Subbasin

Autor: Jan Inge Faleide, Christopher Sæbø Serck, Per Terje Osmundsen, Julie Linnéa Sehested Gresseth, Alvar Braathen

Publikováno v: Basin Research

Late to post-Caledonian, Devonian extension remains unresolved in the SW Barents Sea, despite considerable knowledge from onshore Norway, East Greenland and Svalbard. We analyse intrabasement seismic facies in high-resolution 3D and reprocessed 2D da

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::06ffe7c052041338e91401ff9ef773b0
https://doi.org/10.1111/bre.12631

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Evolution of detachment fault systems within necking domains: insights from the Frøya and Gossa Highs, mid-Norwegian margin

Autor: Julie Linnéa Sehested Gresseth, Per Terje Osmundsen, Gwenn Péron-Pinvidic

Within rifted margins, the necking domain corresponds to the area where drastic reduction in basement thickness leads the crust to attain a wedge-shape. The crustal thinning occurs along detachment fault systems typically recording displacements in t

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::ea65970aa8982c63c26fd7adb96053b9
https://doi.org/10.5194/egusphere-egu22-8003

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Detachment Faulting, Successive Incision and Controls on Supradetachment Basin Formation at the Mid-Norwegian Rifted Margin

Autor: Julie Linnéa Sehested Gresseth, Gwenn Péron-Pinvidic, Per Terje Osmundsen

Detachment fault systems recording displacements in the order of 10s to 100s of km remain poorly understood compared to smaller scale normal faults. The evolutionary models developed for the growth and interaction of Andersonian-type faults are not f

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::795565ec7f6a990d4e7fc4bef162bc21
https://doi.org/10.5194/egusphere-egu21-9481

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