Zobrazeno 1 - 10
of 122
pro vyhledávání: '"Rolf Mjelde"'
Publikováno v:
Geosciences, Vol 9, Iss 4, p 160 (2019)
Magmatic intrusions affect the basin temperature in their vicinity. Faulting and physical properties of the basin may influence the magnitudes of their thermal effects and the potential source rock maturation. We present results from a sensitivity st
Externí odkaz:
https://doaj.org/article/1f80a86e8904409ab92b75e6c406cb1a
Publikováno v:
Polar Research, Vol 31, Iss 0, Pp 1-13 (2012)
A detailed map of the structure of the west Spitsbergen fold-and-thrust belt in the Isfjorden area, Spitsbergen, is presented. The map was constructed from a dense grid of two-dimensional multichannel reflection seismic and bathymetric data. Joint in
Externí odkaz:
https://doaj.org/article/011c12a128de4db8b3c0045ab2e44e7b
The structure of the oceanic crust generated by the ultraslow-spreading mid-ocean Knipovich Ridge still remains relatively uninvestigated compared to the other North Atlantic spreading ridges further south. The complexity of the Knipovich Ridge, with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::519184460c0cf8a5c91b34d16590de68
https://doi.org/10.5194/egusphere-egu23-1879
https://doi.org/10.5194/egusphere-egu23-1879
Autor:
Rafet Ender Alemdar, Metin Kahraman, Alexey Shulgin, Rolf Mjelde, Irina Artemieva, Hans Thybo
The Senja onshore-offshore seismic profile is located in the north-western part of Europe across the Norwegian coast into the North Atlantic ocean. A number of terranes and microcontinents collided to form this region from the Archean to the Paleopro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::029042711ef09fe190ef5e254ed6ac31
https://doi.org/10.5194/egusphere-egu23-15662
https://doi.org/10.5194/egusphere-egu23-15662
The Baltic Shield is located in the northern part of Europe. It formed by amalgamation of a series of terranes and microcontinents during the Archean to the Paleoproterozoic, followed by significant modification in Neoproterozoic to Paleozoic time by
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::612c0a031627f9edaec1f8d7bdae726e
https://doi.org/10.5194/egusphere-egu22-3139
https://doi.org/10.5194/egusphere-egu22-3139
The Baltic Shield is located in the northern part of Europe, which formed by amalgamation of a series of terranes and microcontinents during the Archean to the Paleoproterozoic, followed by significant modification in Neoproterozoic to Paleozoic time
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b82157bd1e9129043e51ac0937548b63
https://doi.org/10.5194/egusphere-egu21-15666
https://doi.org/10.5194/egusphere-egu21-15666
Publikováno v:
Geophysical Journal International
SUMMARY The crustal architecture of the Barents Sea is still enigmatic due to complex evolution during the Timanian and Caledonian orogeny events, further complicated by several rifting episodes. In this study we present the new results on the crusta
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cc329401428952eaf1f3b817bded4a2a
https://hdl.handle.net/11250/2982690
https://hdl.handle.net/11250/2982690
Publikováno v:
Tectonophysics
Highlights • Crustal thickness of the Lofoten/Vesterålen shelf is greater than old study suggested. • Mafic lower crust of the shelf area explains observed resistance to deformation. • Four Mesozoic-Cenozoic erosion episodes are indicated by s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::592aaadbddf4019066ec447b900b7792
https://hdl.handle.net/11250/2755876
https://hdl.handle.net/11250/2755876
Publikováno v:
Geosciences
Volume 9
Issue 11
Volume 9
Issue 11
Diagenetic changes in sedimentary basins may alter hydrocarbon reservoir quality with respect to porosity and permeability. Basins with magmatic intrusions have specific thermal histories that at time of emplacement and in the aftermath have the abil
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::589e52b88b640b67a6fa494734c5e968
Publikováno v:
Geosciences, Vol 9, Iss 4, p 160 (2019)
Geosciences
Volume 9
Issue 4
Geosciences
Volume 9
Issue 4
Magmatic intrusions affect the basin temperature in their vicinity. Faulting and physical properties of the basin may influence the magnitudes of their thermal effects and the potential source rock maturation. We present results from a sensitivity st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0a3e55042fc03d1ec7b778ee083bcc70
https://www.mdpi.com/2076-3263/9/4/160
https://www.mdpi.com/2076-3263/9/4/160