Fault interactions and reactivation within a normal-fault network at Milne Point, Alaska
Fault interactions and reactivation within a normal-fault network at Milne Point, Alaska
A normal-fault network from Milne Point, Alaska, is investigated focusing on characterizing geometry, displacement, strain, and different fault interactions. The network, constrained from three-dimensional seismic reflection data, comprises two generations of faults: Cenozoic north-northeast–trending faults and Jurassic west-northwest–trending faults, which highly compartmentalize Upper Triassic to Lower Cretaceous reservoirs. The west-northwest–trending faults are influenced by a similarly oriented underlying structural grain. This influence is characterized by increases in throw on several faults, strain localization, reorientation of faults and an increase in linkage maturity.
Reconstructing fault plane geometries and mapping spatial variations in throw identified key characteristic features in their interactions and reactivation of pre-existing structures. Faults are divided into isolated, abutting, and splaying faults. Isolated faults exhibit a range of displacement profiles depending on the degree of restriction at fault tips. Fault splays accommodate step-like decreases in throw along larger main faults with a throw maximum at the intersection with the main fault. Throw profiles of abutting faults are divided into two groups: early stage abutting faults with throw minima at both the isolated and abutting tips, and developed abutting faults with throw maxima near the abutting tip.
Developed abutting faults accumulate throw after initial abutment, locally reactivating and transferring throw onto the pre-existing fault. Two abutting faults can link kinematically by reactivating a segment of the pre-existing fault forming a trailing fault. The motion sense of the trailing fault can be synthetic or antithetic to the reactivated pre-existing fault, producing increases or decreases in the throw of the pre-existing fault, respectively.
2081-2107
Nixon, Casey W.
757fe329-f10f-4744-a28e-0ccc92217554
Sanderson, David J.
5653bc11-b905-4985-8c16-c655b2170ba9
Dee, Stephen J.
3c87de83-42cc-475f-87ff-1c762c60ac2d
Bull, Jonathan M.
974037fd-544b-458f-98cc-ce8eca89e3c8
Humphreys, Robert J.
77da8c7d-d9d9-4601-be4a-59e80161d54b
Swanson, Mark H.
0305d0d7-792f-400c-a293-d1f1911edec0
October 2014
Nixon, Casey W.
757fe329-f10f-4744-a28e-0ccc92217554
Sanderson, David J.
5653bc11-b905-4985-8c16-c655b2170ba9
Dee, Stephen J.
3c87de83-42cc-475f-87ff-1c762c60ac2d
Bull, Jonathan M.
974037fd-544b-458f-98cc-ce8eca89e3c8
Humphreys, Robert J.
77da8c7d-d9d9-4601-be4a-59e80161d54b
Swanson, Mark H.
0305d0d7-792f-400c-a293-d1f1911edec0
Nixon, Casey W., Sanderson, David J., Dee, Stephen J., Bull, Jonathan M., Humphreys, Robert J. and Swanson, Mark H.
(2014)
Fault interactions and reactivation within a normal-fault network at Milne Point, Alaska.
AAPG Bulletin, 98 (10), .
(doi:10.1306/04301413177).
Abstract
A normal-fault network from Milne Point, Alaska, is investigated focusing on characterizing geometry, displacement, strain, and different fault interactions. The network, constrained from three-dimensional seismic reflection data, comprises two generations of faults: Cenozoic north-northeast–trending faults and Jurassic west-northwest–trending faults, which highly compartmentalize Upper Triassic to Lower Cretaceous reservoirs. The west-northwest–trending faults are influenced by a similarly oriented underlying structural grain. This influence is characterized by increases in throw on several faults, strain localization, reorientation of faults and an increase in linkage maturity.
Reconstructing fault plane geometries and mapping spatial variations in throw identified key characteristic features in their interactions and reactivation of pre-existing structures. Faults are divided into isolated, abutting, and splaying faults. Isolated faults exhibit a range of displacement profiles depending on the degree of restriction at fault tips. Fault splays accommodate step-like decreases in throw along larger main faults with a throw maximum at the intersection with the main fault. Throw profiles of abutting faults are divided into two groups: early stage abutting faults with throw minima at both the isolated and abutting tips, and developed abutting faults with throw maxima near the abutting tip.
Developed abutting faults accumulate throw after initial abutment, locally reactivating and transferring throw onto the pre-existing fault. Two abutting faults can link kinematically by reactivating a segment of the pre-existing fault forming a trailing fault. The motion sense of the trailing fault can be synthetic or antithetic to the reactivated pre-existing fault, producing increases or decreases in the throw of the pre-existing fault, respectively.
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Accepted/In Press date: 30 April 2014
e-pub ahead of print date: October 2014
Published date: October 2014
Organisations:
Geology & Geophysics
Identifiers
Local EPrints ID: 372115
URI: http://eprints.soton.ac.uk/id/eprint/372115
ISSN: 0149-1423
PURE UUID: 54798787-aecd-4689-8ff6-6fb00feb4378
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Date deposited: 25 Nov 2014 13:09
Last modified: 15 Mar 2024 03:30
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Contributors
Author:
Casey W. Nixon
Author:
Stephen J. Dee
Author:
Robert J. Humphreys
Author:
Mark H. Swanson
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