Zobrazeno 1 - 10 of 27 pro vyhledávání: '"D. Livelybrooks"'
1
Fluid Transport and Storage in the Cascadia Forearc inferred from Magnetotelluric Data
Autor: Kerry Key, Bo Yang, Paul A. Bedrosian, Blake Parris, Anna Kelbert, D. Livelybrooks, Adam Schultz, Gary D. Egbert
Subduction of hydrated oceanic lithosphere can carry water deep into the Earth, with important consequences for a range of tectonic and magmatic processes. Most fluid is released at relatively shallow depths in the forearc where it is thought to play
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::07d4f39684dd9bb5e44351fe14a6b854
https://doi.org/10.21203/rs.3.rs-475649/v1
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2
Single station magnetotelluric impedance estimation: Coherence weighting and the regression M‐estimate
Autor: Gary D. Egbert, D. Livelybrooks
Publikováno v: GEOPHYSICS. 61:964-970
The first step in the interpretation of magnetotelluric (MT) data involves estimating [Formula: see text] frequency‐domain impedances, Z(w), from the raw electric and magnetic field time series e(t), h(t) (approx. [Formula: see text] real numbers/s
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::89b4fc6e74a234c76283c564f0f0d5e1
https://doi.org/10.1190/1.1444045
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3
Causes of high crustal conductivity beneath the Iapetus suture zone in Great Britain
Autor: R. J. Banks, P. Jones, D. Livelybrooks, R. Longstaff
Publikováno v: Geophysical Journal International. 124:433-455
SUMMARY Two magnetic variation anomalies in southern Scotland and northern England have been linked to the position of the Iapetus suture. Previous magnetotelluric measurements along a 140 km profile that crosses both anomalies have been supplemented
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::0fdb3b3a66202cdb0debd19a6d549af5
https://doi.org/10.1111/j.1365-246x.1996.tb07031.x
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4
Program 3Dfeem: a multidimensional electromagnetic finite element model
Autor: D. Livelybrooks
Publikováno v: Geophysical Journal International. 114:443-458
SUMMARY A suite of programs collectively referred to as 3Dfeem (3-D finite element electromagnetic model) has been developed to simulate the response of a given assemblage of conductors to a plane-wave or electric-dipole source. This application of t
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::b51028dabe5acfd0c82c643165279a69
https://doi.org/10.1111/j.1365-246x.1993.tb06978.x
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7
On: 'Magnetotelluric delineation of the Trillabelle massive sulfide body in Sudbury, Ontario' (D. Livelybrooks, M. Mareschal, E. Blais, and J. T. Smith, GEOPHYSICS, 61, 4, 971–986)
Autor: J. T. Smith, Charles E. Corry, D. Livelybrooks
Publikováno v: GEOPHYSICS. 62:1672-1673
Livelybrooks et al. (1996) propose that measuring magnetotelluric (MT) currents generated by naturally occurring electromagnetic fields can be used to locate deep, 2–4 km, ore bodies where other electrical methods fail. However, I find a number of
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::6d8a5a30f0395af260d373aa4a1c5b03
https://doi.org/10.1190/1.1444267
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8
Reply by the authors to the discussion by C. E. Corry
Autor: J. T. Smith, D. Livelybrooks
Publikováno v: GEOPHYSICS. 62:1673-1673
We would like to thank Dr. Corry for his provocative comments on our paper written with the late Marianne Mareschal (Livelybrooks et al., 1996). The problem of spatial aliasing addressed by Corry is, indeed, a very serious concern, as small‐scale i
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https://doi.org/10.1190/1.1487035
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10
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