The nature of a serpentinite-hosted detachement fault underlying the Cretaceous proto-Atlantic: evidence from the Iberia non-volcanic rifted margin
The nature of a serpentinite-hosted detachement fault underlying the Cretaceous proto-Atlantic: evidence from the Iberia non-volcanic rifted margin
ODP LEG 193, SERPENTINITE, FAULT ZONES, IBERIA, GEOLOGY
p.F1261
Hopkinson, L.
bd4c65de-14e5-4e90-8ca5-4c6986dc87f3
Beard, J.S.
85cd87e2-f07f-4e50-bf28-0851d9155ba8
Mortimore, R.N.
412acc6a-58d8-42c3-9632-64c6484add6f
2001
Hopkinson, L.
bd4c65de-14e5-4e90-8ca5-4c6986dc87f3
Beard, J.S.
85cd87e2-f07f-4e50-bf28-0851d9155ba8
Mortimore, R.N.
412acc6a-58d8-42c3-9632-64c6484add6f
Hopkinson, L., Beard, J.S. and Mortimore, R.N.
(2001)
The nature of a serpentinite-hosted detachement fault underlying the Cretaceous proto-Atlantic: evidence from the Iberia non-volcanic rifted margin.
EOS: Transactions American Geophysical Union, 82 (47, Supplement), .
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Published date: 2001
Keywords:
ODP LEG 193, SERPENTINITE, FAULT ZONES, IBERIA, GEOLOGY
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Local EPrints ID: 6143
URI: http://eprints.soton.ac.uk/id/eprint/6143
ISSN: 0096-3941
PURE UUID: 464aca69-76bb-44a5-a6e5-0f2b72b67e54
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Date deposited: 30 Jun 2004
Last modified: 11 Dec 2021 13:22
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Contributors
Author:
L. Hopkinson
Author:
J.S. Beard
Author:
R.N. Mortimore
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