Magnetotelluric evidence for layered mafic intrusions beneath the Voring and Exmouth rifted margins

Citation:
Myer, D, Constable S, Key K.  2013.  Magnetotelluric evidence for layered mafic intrusions beneath the Voring and Exmouth rifted margins. Physics of the Earth and Planetary Interiors. 220:1-10.

Date Published:

7/2013

Keywords:

continental margins, crustal structure, deep-structure, drilling program ktb, electrical-conductivity, exmouth plateau, magnetite, marine magnetotellurics, norwegian margin, rifted margins, seaward-dipping reflectors, transition, Voring Plateau, western-australia

Abstract:

Marine magnetotelluric (MT) surveys at two volcanic passive margins have revealed an enigmatic layer of extremely high conductivity (<= 0.1 Omega m) at similar to 10 km depth. At the Voring Plateau off the northwest shelf of Norway, 2D inversion of data from nine sites along a 54 km line resolves a layer with a conductance of similar to 10(4) S. At the Exmouth Plateau off the northwest shelf of Australia, 2D inversion of 122 sites in 17 lines finds a similar layer at similar depth but an order of magnitude higher conductance. At both plateaus, the depth of the high conductivity layer coincides roughly with what seismic studies have identified as an assemblage of sills. We propose that the extremely high conductance is due to well-connected conductive cumulates (e.g. magnetite) precipitated in layered mafic intrusions. In contrast to sill emplacement, the nature of layered intrusion formation requires connection to a magma source over time. Such a connection would not be likely during rifting when the rift provides a preferential pathway for pressure release. This implies emplacement prior to or during a pause in the early stage of continental breakup. (c) 2013 Elsevier B.V. All rights reserved.

Notes:

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DOI:

10.1016/j.pepi.2013.04.007