Soft-Sediment deformation features in core from CRP-2/2A, Victoria Land Basin, Antarctica

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12 Citations (Scopus)

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 in 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 Eocene/early Oligocene and the middle Miocene.

Original languageEnglish
Pages (from-to)401-412
Number of pages12
JournalTerra Antarctica
Volume7
Issue number3
StatePublished - 1 Dec 2000

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Ice
Antarctica
basins
Oligocene
sediments
shears
shear zone
basin
slumping
sediment
Gases
ice
Miocene
diamictite
sequence boundary
gas hydrate
geological record
global change
unconformity
logging

Cite this

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title = "Soft-Sediment deformation features in core from CRP-2/2A, Victoria Land Basin, Antarctica",
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 in 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 Eocene/early Oligocene and the middle Miocene.",
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Soft-Sediment deformation features in core from CRP-2/2A, Victoria Land Basin, Antarctica. / Passchier, Sandra.

In: Terra Antarctica, Vol. 7, No. 3, 01.12.2000, p. 401-412.

Research output: Contribution to journalArticleResearchpeer-review

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