Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Daniele Thallner"'
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Palaeointensity information enables us to define the strength of Earth’s magnetic field over geological time, providing a window into Earth’s deep interior. The difficulties in acquiring reliable measurements are substantial, particularly from ol
Externí odkaz:
https://doaj.org/article/8e2a55aecd2d4cea9531234642bd4f83
Autor:
Juliane Dannberg, Daniele Thallner, Rene Gassmoeller, Courtney Sprain, Frederick LaCombe, Chloe Ritchie
Mantle convection and plate tectonics are crucial mechanisms for keeping conditions at the Earth’s surface in a suitable range for life. One important mantle process is the transport of heat out of the Earth’s outer core, which impacts the geodyn
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6a354a16781fa9658b598054106f2650
https://doi.org/10.5194/egusphere-egu23-9490
https://doi.org/10.5194/egusphere-egu23-9490
Autor:
Richard K Bono, Greig A Paterson, Annique van der Boon, Yael A Engbers, J Michael Grappone, Benjamin Handford, Louise M A Hawkins, Simon J Lloyd, Courtney J Sprain, Daniele Thallner, Andrew J Biggin
Publikováno v:
Geophysical Journal International. 229:522-545
SUMMARY Palaeomagnetic field intensity measurements, derived from rocks with ages that span geological time, provide a crucial constraint on the evolution of Earth’s deep interior and its magnetic environment. The palaeointensity database PINT has
Autor:
Annique van der Boon, Andrew J. Biggin, Daniele Thallner, Mark W. Hounslow, Richard Bono, Jerzy Nawrocki, Krystian Wójcik, Mariusz Paszkowski, Peter Königshof, Tim de Backer, Pavel Kabanov, Sofie Gouwy, Richard VandenBerg, Anne-Christine Da Silva
The Devonian has long been a problematic period for paleomagnetism. Devonian paleomagnetic data are generally difficult to interpret and have complex partial or full overprints– problems that arise in data obtained from both sedimentary and igneous
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5847703c7cfbf2612f9e3b5f40b1ca19
http://hdl.handle.net/10852/94386
http://hdl.handle.net/10852/94386
Autor:
Andrew J. Biggin, Valera P. Shcherbakov, V. V. Shcherbakova, Daniele Thallner, Vladimir Bakhmutov, G. V. Zhidkov
Publikováno v:
GEOPHYSICAL JOURNAL INTERNATIONAL
SUMMARY The time-averaged geomagnetic field is generally purported to be uniformitarian across Earth history—close to a geocentric axial dipole, with average strength within one order of magnitude of that at present. Nevertheless, recent studies ha
Publikováno v:
Journal of Geophysical Research: Solid Earth. 126
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Palaeointensity information enables us to define the strength of Earth’s magnetic field over geological time, providing a window into Earth’s deep interior. The difficulties in acquiring reliable measurements are substantial, particularly from ol
Autor:
Sofie Gouwy, Mark W. Hounslow, Annique van der Boon, Daniele Thallner, Peter Königshof, Tim de Backer, Kristyan Wójcik, Pavel Kabanov, Andrew J. Biggin, Mariusz Paszkowski, Jerzy Nawrocki, Richard K. Bono, Richard Vandenberg
The Devonian has long been a problematic era for paleomagnetism. Devonian data are generally difficult to interpret and have complex partial or full overprints. These problems arise from paleomagnetic data obtained from both sedimentary and igneous r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::39a4890b245d6e5e6ac0e5bd538011ae
https://doi.org/10.5194/egusphere-egu21-9035
https://doi.org/10.5194/egusphere-egu21-9035
Autor:
Jerzy Nawrocki, Pavel Kabanov, Peter Königshof, Andrew J. Biggin, Richard Vandenberg, Mark W. Hounslow, Annique van der Boon, Tim de Backer, Sofie Gouwy, Mariusz Paszkowski, Kristyan Wójcik, Daniele Thallner, Richard K. Bono
The global polarity time scale (GPTS) is relatively unconstrained for the Paleozoic, particularly the Devonian. Constraining the GPTS and reversal frequency for the Devonian is crucial for the understanding of the behaviour of Earth’s magnetic fiel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8fb6507c25698f5aae4599138398209e
https://doi.org/10.5194/egusphere-egu21-9036
https://doi.org/10.5194/egusphere-egu21-9036
Autor:
Daniele Thallner, Andy Biggin, Mimi Hill, Henry Halls, Phil J. A. McCausland, Valentina V. Shcherbakova, Valeriy P. Shcherbakov, Vladimir G. Bakhmutov
Palaeomagnetic investigations from the Ediacaran period (635-541 Ma) give anomalous results, which might indicate unusual behaviour of Earth’s magnetic field. In contrast to the conventional geomagnetic dipole field, geocentric and aligned with Ear
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ea2129bc83be078f23b61bf1d0d413a2
https://doi.org/10.5194/egusphere-egu2020-9121
https://doi.org/10.5194/egusphere-egu2020-9121