Kopf, Achim (2001): Permeability variation across an active low-angle detachment fault, western Woodlark Basin (ODP Leg 180), and its implication for fault activation

Leg/Site/Hole:
ODP 180
ODP 180 1108
ODP 180 1114
Identifier:
2002-070910
georefid

Creator:
Kopf, Achim
GEOMAR, Kiel, Federal Republic of Germany
author

Identification:
Permeability variation across an active low-angle detachment fault, western Woodlark Basin (ODP Leg 180), and its implication for fault activation
2001
In: Holdsworth, Robert E. (editor), Strachan, Robert A. (editor), Magloughlin, Jerry F. (editor), Knipe, Robert J. (editor), The nature and tectonic significance of fault zone weakening
Geological Society of London, London, United Kingdom
186
23-41
In the western Woodlark Basin, off Papua New Guinea, the variation from continental rifting to sea-floor spreading has profound effects on the mechanical response of the lithosphere. The extension is well expressed in a seismically active, shallow-dipping detachment fault. Recent Ocean Drilling Program drilling (ODP Leg 180) in the area obtained cores from the hanging wall, detachment fault gouge, and footwall, of which samples underwent permeability testing in the laboratory. Permeability variation was found to be critically dependent on (1) flow direction, i.e. fabric anisotropy of the rocks, and (2) deformational structures in the hanging wall to the fault. Regarding the first, a slight but distinct increase in permeability has been recorded parallel to the fabric (compared with flow normal to this, as indicated by anisotropy indices of k (sub horizontal) /k (sub vertical) of >1.7). This phenomenon appears most profound directly above fault zones in the hanging-wall block, which are interpreted to represent splays to the main detachment fault plane at depth. Here, shear-enhanced compaction seals fluid flow to the sea floor, so that conductive flow parallel to the fault plane is favoured (in general one order of magnitude higher). The fault gouge, mainly consisting of highly serpentinized basalt and chlorite, exhibits an increase in permeability relative to the clay- and siltstones of the hanging-wall block. In the metamorphic basalt from the tectonic footwall, permeability decreases again by three orders of magnitude (k is c. 6e-17 to 5e-18 m (super 2) ). Consequently, the detachment and synthetic splays related to it are zones of enhanced fluid migration in the fault plane direction. Fluid overpressure, and hence fault activity, is suggested to be triggered by seal of the top of the fault zone, owing to both shear fabrics and cementation processes.
English
Serial
Coverage:Geographic coordinates:
North:-5.0000
West:150.0000East: 160.0000
South:-10.0000

Structural geology; anisotropy; clastic rocks; compaction; Coral Sea; cores; detachment faults; faults; hanging wall; lateral heterogeneity; Leg 180; Moresby Seamount; mudstone; Ocean Drilling Program; ODP Site 1108; ODP Site 1114; Pacific Ocean; permeability; physical properties; plate tectonics; reactivation; rifting; sea-floor spreading; sedimentary rocks; Solomon Sea; South Pacific; Southwest Pacific; West Pacific; Woodlark Basin;

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