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Passchier, Sandra (2000): Prominent deformation features and interpretation of sediment core CRP-2/2A (Table 1) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.144477, Supplement to: Passchier, S (2000): Soft-sediment deformation features in core from CRP-2/2A, Victoria Land Basin, Antarctica. Terra Antartica, 7(3), 401-412, hdl:10013/epic.28263.d001

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Abstract:
Sediment deformation features in CRP-2/2A were described during normal logging procedures and from core-scan images. In this paper the origin of soft-sediment folding, contorted bedding, microfaulting, clastic dykes, shear zones and intraformational breccias is discussed. The features have a stratigraphic distribution related to major unconformities and sequence boundaries. Hypotheses for the origins of sediment deformation include hydrofracturing, subglacial shearing, slumping, and gas hydrate formation. Shear zones, microfaults, clastic dykes and contorted bedding within rapidly deposited sediments, suggest that slumping in an ice-distal environment occurred in the early Oligocene. A till wedge beneath a diamictite at 364 mbsf the mid-Oligocene section represents the oldest evidence of grounded ice in CRP-2/2A. Shear zones with a subglacial origin in the early late Oligocene and early Miocene sections of the core are evidence of further grounding events. The interpretation of sediment deformation in CRP-2/2A is compared to other Antarctic stratigraphic records and global eustatic change between the late Eocenel/early Oligocene and the middle Miocene.
Project(s):
Coverage:
Latitude: -77.005980 * Longitude: 163.719450
Date/Time Start: 1998-10-16T07:30:00 * Date/Time End: 1998-11-25T14:20:00
Minimum Elevation: -177.9 m * Maximum Elevation: -177.9 m
Event(s):
CRP-2A (14.2 km at 096° true from Cape Roberts) * Latitude: -77.005980 * Longitude: 163.719450 * Date/Time Start: 1998-10-16T07:30:00 * Date/Time End: 1998-11-25T14:20:00 * Elevation: -177.9 m * Recovery: 624 m * Location: off Cape Roberts, Ross Sea, Antarctica * Campaign: CRP-2 * Basis: Sampling/drilling from ice * Method/Device: Core wireline system (CWS) * Comment: 921 m at 284° from CRP-1. Sea-ice thickness: 2.0 m (1 Oct) to 2.2 m (23 Nov). Sea riser embedded to 13.03 mbsf. Lateral ice movement: 9.87 m to east from 17 Oct to 23 Nov. HQ core to 199.31 mbsf. NQ core to 624.15 mbsf. 13.03 to 45.97 mbsf, 11.29 m (34%) partially following CRP-2. 45.07 to 624.15 mbsf, 548.67 m (95%) new hole. Deepest core-lithology: hard sandy siltstone. Deepest core-age: earliest Oligocene (ca. 33 Ma on diatoms, nannofossils and dinoflagellates)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Depth, top/minDepth topmPasschier, Sandra
Depth, bottom/maxDepth botmPasschier, Sandra
Deformation structure, typeDeformationPasschier, Sandra
Facies name/codeFaciesPasschier, SandraFacies association
Geology, commentGeo commPasschier, SandraInterpretation
Size:
218 data points

Data

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Depth top [m]

Depth bot [m]

Deformation

Facies

Geo comm
12.0016.00crackle breccia ?bottom of diamictite?
44.9147.87chaotic breccias, cataclastic, thrustsabove diamictiteproglacial ice-push
50.0071.00breccias, cataclastic shaer zonesbelow diamictitesubglacial shaer
90.6792.86soft-sediment deformarmationbelow diamictitesubglacial shaer?
93.8598.64crackle brecciabetween diamictitesin situ fracturing
99.00foldingwithin diamictitemass-gravity flow
131.00132.00crackle brecciabelow diamictitein situ fracturing
145.00151.00brecciated sandstone dykestop of clast-poor unithydrofracturing
176.20176.30microfaults, soft-sediment foldingwithin mudstone?
183.35185.95folds, rotated claststop of sandstonemass-gravity flow
245.00vertical fracturesbelow diamictite?
297.40clastic dyke through cemented patchabove diamictite?
297.00306.00folds (D), faults and breccia (sst)within diamictitecollapse?
306.00intraclast, boudinage, clast rotationbottom of diamictitesubglacial shaer
307.00fault with large displacementbelow diamictite?
307.00308.00rubble and crackle brecciabelow diamictitesubglacial shaer
311.00315.00matrix-supported brecciawithin clast-poor unitcollapse?
315.00326.00fault and clastic dykesinterbeddet lithologies?
328.00clastic dyke, coarse stratified fillbelow diamictitesubglacial shaer
329.00clastic dyke?below diamictitesubglacial shaer
331.90matrix-supported brecciawithin mudstonemass-gravity flow
332.00clastic dyke, calcified and pyritizedwithin mudstone?
334.00clastic dyke, faultedwithin mudstone?
337.00clastic dyke, faulted and faultedwithin mudstone?
362.78363.03shaer zone, folding, faultingbetween diamictitessubglacial shaer
363.22363.63clastic wedgebetween diamictitessubglacial shaer
364.00clastic dykebetween diamictitessubglacial shaer
381.00384.00microfaults, soft-sediment foldingstratified diamictitemass-gravity flow
447.00pyritized clastic dikes, planar marginswithin mudstonetectonic?
468.70fault cross-cuts calcite patchwithin mudstonetectonic?
501.00503.00contorted bedding, foldinglaminated sandstoneslumping
504.00506.00local mosaic brecciasinterbedded lithologiesgas-hydratre formation?
512.00516.00contorted bedding, foldinggradet bedsslumping
520.00523.00clastic dykes, microfaultingsandy conglomeratedebris flow
524.00527.00faults, pyritised clastic dykesbelow congomeratedebris flow
525.80mosaic brecciaabove gradet bedsgas-hydratre formation?
535.00540.00faulted clastic dykesbelow congomeratedebris flow
543.00552.00faults, pyritised clastic dykeswithin mudstonetectonic?
577.00579.00contorted bedding, foldinginterbedded lithologiesslumping
579.02580.99anastomosing networksinterbedded lithologiesslumping
581.00585.00contorted bedding, foldingabove conglomerateslumping
587.00mosaic brecciaabove gradet bedsgas-hydratre formation?
594.97595.03mosaic brecciabelow clastgas-hydratre formation?
608.70anastomosing dilated laminaebelow straitfied sandstslumping
608.00608.14contorted bedding, foldingwithin sandstoneslumping
612.00612.07microfaulting cuts foldingabove conglomerateslumping
614.00614.20anastomosing dilated laminaeabove conglomerateslumping