Zobrazeno 1 - 10
of 51
pro vyhledávání: '"Muxworthy AR"'
Greigite forms as an intermediate phase along the pyrite reaction pathway. Despite being considered metastable, it is observed in numerous shallow natural systems, suggesting it could be a unique proxy for diagenetic and environmental conditions. We
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1032::ee0f2939561dda4035a1927db00cf750
http://hdl.handle.net/10044/1/105308
http://hdl.handle.net/10044/1/105308
Publikováno v:
Frontiers in Earth Science. 10
Determining the position and thickness of the oil-water transition zone (OWTZ) in hydrocarbon reservoirs is important to reserve estimation and production planning. This paper describes a magnetic method of identifying this zone. High temperature sus
Autor:
Valdez-Grijalva, MA, Muxworthy, AR, Williams, W, ó Conbhui, P, Nagy, L, Roberts, AP, Heslop, D
Publikováno v:
Valdez-Grijalva, M A, Muxworthy, A R, Williams, W, Ó Conbhuí, P, Nagy, L, Roberts, A P & Heslop, D 2018, ' Magnetic vortex effects on first-order reversal curve (FORC) diagrams for greigite dispersions ', Earth and Planetary Science Letters . https://doi.org/10.1016/j.epsl.2018.08.027
First-order reversal curve (FORC) diagrams are used increasingly in geophysics for magnetic domain state identification. The domain state of a magnetic particle is highly sensitive to particle size, about which FORC diagrams provide valuable informat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::3c3854da4ed6bd98991b7eba5741ff8e
https://hdl.handle.net/20.500.11820/21621266-aa9c-4ac7-a3de-09fa206520c6
https://hdl.handle.net/20.500.11820/21621266-aa9c-4ac7-a3de-09fa206520c6
Autor:
Valdez-Grijalva, MA, Muxworthy, AR
First-order reversal curve (FORC) diagrams are increasingly used as a material’s magnetic domain state fingerprint. FORC diagrams of noninteracting dispersions of single-domain (SD) particles with uniaxial magnetocrystalline anisotropy (MCA) are we
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1032::0a54d4c4b5e2941ce3ffc2cbe847c6d3
http://hdl.handle.net/10044/1/65027
http://hdl.handle.net/10044/1/65027
Publikováno v:
Ó conbhuí, P, Williams, W, Fabian, K, Ridley, P, Nagy, L & Muxworthy, A R 2018, ' MERRILL: Micromagnetic Earth Related Robust Interpreted Language Laboratory ', Geochemistry, Geophysics, Geosystems . https://doi.org/10.1002/2017GC007279
Complex magnetic domain structures and the energy barriers between them are responsible for pseudo‐single domain phenomena in rock magnetism, and contribute significantly to the magnetic remanence of paleomagnetic samples. This article introduces M
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::1f8f5a0e5bc53c2192b16140b34ea395
https://www.pure.ed.ac.uk/ws/files/53270669/merrill_paper.pdf
https://www.pure.ed.ac.uk/ws/files/53270669/merrill_paper.pdf
publisher: Elsevier articletitle: Long-lived magnetism on chondrite parent bodies journaltitle: Earth and Planetary Science Letters articlelink: http://dx.doi.org/10.1016/j.epsl.2017.07.035 content_type: article copyright: © 2017 The Authors. Publis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3592::fd1f1f5ae9178d0cfa6093f428356fef
http://hdl.handle.net/10141/622267
http://hdl.handle.net/10141/622267
We present evidence for both early- and late-stage magnetic activity on the CV and L/LL parent bodies respectively from chondrules in Vigarano and Bjurböle. Using micro-CT scans to re-orientate chondrules to their in-situ positions, we present a new
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1032::064966f223af3b6beea7ec11c07ef83f
http://hdl.handle.net/10044/1/51605
http://hdl.handle.net/10044/1/51605
We conducted a paleomagnetic study of the matrix of Allende CV3 chondritic meteorite, isolating the matrix’s primary remanent magnetization, measuring its magnetic fabric and estimating the ancient magnetic field intensity. A strong planar magnetic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______1032::819c661b33ee1f7528be0db985075070
http://hdl.handle.net/10044/1/48604
http://hdl.handle.net/10044/1/48604
The study of the palaeomagnetic signal recorded by rocks allows scientists to understand the Earth’s past magnetic field and the formation of the geodynamo. The magnetic recording fidelity of this signal is dependent on the magnetic domain state it
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::c26dbf8bfe3370fcfb024c9c21f7d95e
http://hdl.handle.net/10044/1/32746
http://hdl.handle.net/10044/1/32746