Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Sheona Masterton"'
The Fram Strait (North-eastern Atlantic Ocean) developed along a narrow transform margin that separates the Arctic Basin in the north from the Atlantic Basins in the south. The transform margin developed from the Miocene to Present Day and provided t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bb3842fc3ef8078781e25206147c79fc
https://doi.org/10.5194/egusphere-egu23-15682
https://doi.org/10.5194/egusphere-egu23-15682
Temperature and heat flow are key parameters for understanding the potential for source rock maturation in sedimentary basins. Knowledge of the thermal structure of the lithosphere in both a regional and local context can provide important constraint
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::be592223aecef853f979e2ce1665daa6
https://doi.org/10.5194/egusphere-egu2020-19005
https://doi.org/10.5194/egusphere-egu2020-19005
Autor:
Sheona Masterton, Simon Williams, Joanne M. Whittaker, Paul Wessel, Maria Seton, Ralph Müller, Juan Carlos Afonso
Publikováno v:
Nature Geoscience. 8:479-483
Tectonic plate and lower-mantle motions are often considered independent. Plate tectonic reconstructions reveal long-lived interactions between mantle plumes and mid-ocean ridges that imply feedback between plate boundaries and the deep mantle.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9cc9c96f58f9ba94646c7c0db03d5925
https://doi.org/10.1038/ngeo2437
https://doi.org/10.1038/ngeo2437
Autor:
Jade L. Dickinson, Ahmed Salem, J. Derek Fairhead, Simon Campbell, Colm A. Murphy, Sheona Masterton
Publikováno v:
Geophysical Prospecting. 61:1065-1076
Full Tensor Gravity Gradiometry (FTG) data are routinely used in exploration programmes to evaluate and explore geological complexities hosting hydrocarbon and mineral resources. FTG data are typically used to map a host structure and locate target r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::95ec311795962718ac506b37a869eb71
https://doi.org/10.1111/1365-2478.12039
https://doi.org/10.1111/1365-2478.12039
Publikováno v:
Geophysical Prospecting. 59:1072-1086
This paper interprets aeromagnetic data for a deep basin section of the Karroo rift in south-east Tanzania.We use a novel integrated approach involving the application of advanced derivatives to define structure and the tilt-depth method to determine
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c9f60bf2db0dbc783cde74c6d3f784ff
https://doi.org/10.1111/j.1365-2478.2011.01001.x
https://doi.org/10.1111/j.1365-2478.2011.01001.x
Publikováno v:
Geophysical Journal International. 187:99-117
SUMMARY The lithospheric contribution to the geomagnetic field arises from magnetized rocks in a thin shell at the Earth’s surface. The lithospheric field can be calculated as an integral of the distribution of magnetization using standard results
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8f6b8d25575ce94becd0193c85dcd546
https://doi.org/10.1111/j.1365-246x.2011.05153.x
https://doi.org/10.1111/j.1365-246x.2011.05153.x
Publikováno v:
Proceedings.
Gravity data are an important tool for plate tectonic modelling as they image oceanic fracture zones which delineate the movement of plates as well as plate boundaries and geological structures on conjugate plate margins. Reconstructing gravity image
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::84c46ff80bccd5337f94dbbae7ea013e
https://doi.org/10.3997/2214-4609.20141068
https://doi.org/10.3997/2214-4609.20141068
Publikováno v:
IndraStra Global.
We construct a model of remanence for the oceans, combine it with a model of induced magnetization for the whole Earth from a previous study, compute the predicted lithospheric geomagnetic field and compare the result with a model, MF7, that is based
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::42b9b7771a10e9c92c252c074ce4c56a
https://igi.indrastra.com/items/show/58439
https://igi.indrastra.com/items/show/58439
Publikováno v:
Scopus-Elsevier
This contribution has three primary objectives: 1) We demonstrate that there are notable regions in both the Central and South Atlantic that are devoid of secondary fracture zones, following structural interpretation of high quality aeromagnetic and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2ff37a52b6a1c117573b1a5b879db347
https://doi.org/10.3997/2214-4609.20148658
https://doi.org/10.3997/2214-4609.20148658