Zobrazeno 1 - 10
of 22
pro vyhledávání: '"Gijs A. Henstra"'
Autor:
Gijs A. Henstra, Timothy M. Cullen, Robert L. Gawthorpe, Jhon M. Munoz‐Barrera, Martin Muravchik, Atle Rotevatn
Publikováno v:
Basin Research.
Autor:
Rob L. Gawthorpe, Thomas Berg Kristensen, Atle Rotevatn, Gijs A. Henstra, Rodmar Ravnås, Maria Marvik
Publikováno v:
Geological Society, London, Special Publications. 495:43-71
The growth of faults and folds in basins formed under transtension has been less studied than that in their extensional counterparts. In this study, we capitalize on 3D seismic reflection data to investigate the evolution of faults and folds that evo
Publikováno v:
Journal of Structural Geology
Faults commonly form loci for high fluid flux in sedimentary basins, where fluids, rocks and deformation processes frequently interact. Here, we elucidate the interaction of fluid flow, diagenesis and deformation near basin-bounding faults in sedimen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::768b6a31cbfbb07538d443e1d5b7c43a
https://doi.org/10.31223/x5fp57
https://doi.org/10.31223/x5fp57
Autor:
Emmanuel Skourtsos, Gijs A. Henstra, Martin Muravchik, Haralambos Kranis, Gauti T. Eliassen, Rob L. Gawthorpe, Mike Leeder, Julian E. Andrews
Publikováno v:
Basin Research
[Tectono‐sedimentary models of the evolution of the Rethi‐Dendro Formation depositional environment in the Amphithea fault block. Plio‐Pleistocene syn‐rift of the Corinth Rift, Greece. , Abstract Our current understanding on sedimentary deep
Publikováno v:
Basin Research. 31:1083-1097
Recent studies of natural, multiphase rifts suggest that the presence of pre‐existing faults may strongly influence fault growth during later rift phases. These findings compare well with predictions from recent scaled analogue experiments that sim
Autor:
Atle Rotevatn, Rob L. Gawthorpe, Jhon M. Muñoz-Barrera, Gijs A. Henstra, Thomas Berg Kristensen
Publikováno v:
Journal of Structural Geology
The role of inherited structures during the development of normal faults in continental rifts and proximal domains of passive margins have been extensively studied. Few studies, however, have a focus on deciphering the role of inheritance in the deve
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c17f54a9c8c902464c99e96f8b4c3fc3
https://hdl.handle.net/11250/2739958
https://hdl.handle.net/11250/2739958
Autor:
Eric Salomon, Atle Rotevatn, Thomas Berg Kristensen, Sten-Andreas Grundvåg, Gijs Allard Henstra, Anna Nele Meckler, Axel Gerdes, Richard Albert
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::939f8938a36ff86f754aa45284e74354
https://doi.org/10.5194/se-2020-72-supplement
https://doi.org/10.5194/se-2020-72-supplement
Autor:
Eric Salomon, Atle Rotevatn, Thomas Berg Kristensen, Sten-Andreas Grundvåg, Gijs Allard Henstra, Anna Nele Meckler, Axel Gerdes, Richard Albert
In marine rift basins, rift-climax deep-water clastics in the hanging wall of rift- or basin-bounding fault systems are commonly juxtaposed against crystalline basement rocks in the footwall. Displacing highly permeable, unconsolidated sediments agai
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d5777bf89144b79c819e8056fcb2c942
https://doi.org/10.5194/se-2020-72
https://doi.org/10.5194/se-2020-72
Autor:
Martin Muravchik, Gauti T. Eliassen, Gijs A. Henstra, Rob L. Gawthorpe, Gunn Mangerud, Katerina Kouli, Haralambos Kranis, Emmanuel Skoutsos, Mike Leeder, Julian Andrews, Darren F. Mark
The sedimentary record of deep-water lakes is often used to investigate past climate and environmental change. Correct identification however, of the main controls driving the production and transport of sediment to the deepest parts of tectonically
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a13cf44c33c458d6cb8056bc554c00c8
https://doi.org/10.5194/egusphere-egu2020-17438
https://doi.org/10.5194/egusphere-egu2020-17438
Autor:
Sten-Andreas Grundvåg, Richard Albert Roper, Gijs A. Henstra, Thomas Berg Kristensen, Axel Gerdes, Anna Nele Meckler, Eric Salomon, Atle Rotevatn
In marine rift basins, rift-climax deep-water clastics in the hanging wall of rift- or basin-bounding fault systems are commonly juxtaposed against crystalline basement rocks in the footwall. Displacing highly permeable, unconsolidated sediments agai
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::befd2ed3d05d91c339fe6eec2da06b1b
https://doi.org/10.5194/egusphere-egu2020-14590
https://doi.org/10.5194/egusphere-egu2020-14590