Rifting of a passive margin and development of a lower-crustal detachment zone: Evidence from marine magnetotellurics-Reference-Cited by-同舟云学术

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Rifting of a passive margin and development of a lower-crustal detachment zone: Evidence from marine magnetotellurics

Published:2005-06 Issue:12 Volume:32 Page:n/a-n/a
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Heinson Graham¹,White Antony²,Lilley F. E. M.³

Affiliation:

1. Continental Evolution Research Group, School of Earth and Environmental Sciences; University of Adelaide; Adelaide, South Australia Australia

2. School of Chemistry, Physics and Earth Sciences; Flinders University of South Australia; Adelaide, South Australia Australia

3. Research School of Earth Sciences; Australian National University; Canberra, A. C. T. Australia

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference22 articles.

1. Modes of continental lithospheric extension;Buck;J. Geophys. Res.,1991

2. Some comments on magnetotelluric response function estimation;Chave;J. Geophys. Res.,1989

3. The electrical conductivity of an isotropic olivine mantle;Constable;J. Geophys. Res.,1992

4. Occam's inversion to generate smooth, two-dimensional models from magnetotelluric data;DeGroot-Hedlin;Geophysics,1990

5. Lower crustal extension across the Northern Carnarvon Basin, Australia: Evidence for an eastward dipping detachment;Driscoll;J. Geophys. Res.,1998

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