Consolidation patterns during initiation and evolution of a plate-boundary decollement zone: northern Barbados accretionary prism

J. Casey Moore; Adam Klaus; Nathan L. Bangs; Barbara Bekins; Christian J. Bücker; Warner Brückmann; Stephanie N. Erickson; Olav Hansen; Thomas Horton; Peter Ireland; Candace Olson Major; Gregory F. Moore; Sheila Peacock; Saneatsu Saito; Elizabeth J. Screaton; John W. Shimeld; Philip Henry Stauffer; Tuncay Taymaz; Philip A. Teas; Tomochika Tokunaga

doi:10.1130/0091-7613(1998)026<0811:CPDIAE>2.3.CO;2

Consolidation patterns during initiation and evolution of a plate-boundary decollement zone: northern Barbados accretionary prism

J. Casey Moore^*
, Adam Klaus
, Nathan L. Bangs
, Barbara Bekins
, Christian J. Bücker
, Warner Brückmann
, Stephanie N. Erickson
, Olav Hansen
, Thomas Horton
, Peter Ireland
, Candace Olson Major
, Gregory F. Moore
, Sheila Peacock
, Saneatsu Saito
, Elizabeth J. Screaton
, John W. Shimeld
, Philip Henry Stauffer
, Tuncay Taymaz
, Philip A. Teas
, Tomochika Tokunaga

^*Bu çalışma için yazışmadan sorumlu yazar

Jeofizik Mühendisliği Bölümü

University of California at Santa Cruz
Texas A&M University
University of Texas at Austin
United States Geological Survey
Leibniz Institute for Applied Geophysics
Helmholtz Centre for Ocean Research Kiel
University of Utah
Equinor ASA
Schlumberger
Columbia University
University of Hawai'i at Mānoa
University of Birmingham
The University of Tokyo
University of Florida
Dalhousie University

Araştırma sonucu: Dergiye katkı › Makale › bilirkişi

81 Atıf (Scopus)

Özet

Borehole logs from the northern Barbados accretionary prism show that the plate-boundary decollement initiates in a low-density radiolarian claystone. With continued thrusting, the decollement zone consolidates, but in a patchy manner. The logs calibrate a three-dimensional seismic reflection image of the decollement zone and indicate which portions are of low density and enriched in fluid, and which portions have consolidated. The seismic image demonstrates that an underconsolidated patch of the decollement zone connects to a fluid-rich conduit extending down the decollement surface. Fluid migration up this conduit probably supports the open pore structure in the underconsolidated patch.

Orijinal dil	İngilizce
Sayfa (başlangıç-bitiş)	811-814
Sayfa sayısı	4
Dergi	Geology
Hacim	26
Basın numarası	9
DOI'lar	https://doi.org/10.1130/0091-7613(1998)026<0811:CPDIAE>2.3.CO;2
Yayın durumu	Yayınlandı - 1998

Belgeye Erişim

10.1130/0091-7613(1998)026<0811:CPDIAE>2.3.CO;2

Diğer Dosyalar ve Linkler

Link to publication in Scopus

Alıntı Yap

Moore, J. C., Klaus, A., Bangs, N. L., Bekins, B., Bücker, C. J., Brückmann, W., Erickson, S. N., Hansen, O., Horton, T., Ireland, P., Major, C. O., Moore, G. F., Peacock, S., Saito, S., Screaton, E. J., Shimeld, J. W., Stauffer, P. H., Taymaz, T., Teas, P. A., & Tokunaga, T. (1998). Consolidation patterns during initiation and evolution of a plate-boundary decollement zone: northern Barbados accretionary prism. Geology, 26(9), 811-814. https://doi.org/10.1130/0091-7613(1998)026<0811:CPDIAE>2.3.CO;2

@article{ce9ca9e49bf34adbb18e8762c759c2f1,

title = "Consolidation patterns during initiation and evolution of a plate-boundary decollement zone: northern Barbados accretionary prism",

abstract = "Borehole logs from the northern Barbados accretionary prism show that the plate-boundary decollement initiates in a low-density radiolarian claystone. With continued thrusting, the decollement zone consolidates, but in a patchy manner. The logs calibrate a three-dimensional seismic reflection image of the decollement zone and indicate which portions are of low density and enriched in fluid, and which portions have consolidated. The seismic image demonstrates that an underconsolidated patch of the decollement zone connects to a fluid-rich conduit extending down the decollement surface. Fluid migration up this conduit probably supports the open pore structure in the underconsolidated patch.",

author = "Moore, \{J. Casey\} and Adam Klaus and Bangs, \{Nathan L.\} and Barbara Bekins and B{\"u}cker, \{Christian J.\} and Warner Br{\"u}ckmann and Erickson, \{Stephanie N.\} and Olav Hansen and Thomas Horton and Peter Ireland and Major, \{Candace Olson\} and Moore, \{Gregory F.\} and Sheila Peacock and Saneatsu Saito and Screaton, \{Elizabeth J.\} and Shimeld, \{John W.\} and Stauffer, \{Philip Henry\} and Tuncay Taymaz and Teas, \{Philip A.\} and Tomochika Tokunaga",

year = "1998",

doi = "10.1130/0091-7613(1998)026<0811:CPDIAE>2.3.CO;2",

language = "English",

volume = "26",

pages = "811--814",

journal = "Geology",

issn = "0091-7613",

publisher = "Geological Society of America",

number = "9",

}

Moore, JC, Klaus, A, Bangs, NL, Bekins, B, Bücker, CJ, Brückmann, W, Erickson, SN, Hansen, O, Horton, T, Ireland, P, Major, CO, Moore, GF, Peacock, S, Saito, S, Screaton, EJ, Shimeld, JW, Stauffer, PH, Taymaz, T, Teas, PA & Tokunaga, T 1998, 'Consolidation patterns during initiation and evolution of a plate-boundary decollement zone: northern Barbados accretionary prism', Geology, hac. 26, no. 9, pp. 811-814. https://doi.org/10.1130/0091-7613(1998)026<0811:CPDIAE>2.3.CO;2

TY - JOUR

T1 - Consolidation patterns during initiation and evolution of a plate-boundary decollement zone

T2 - northern Barbados accretionary prism

AU - Moore, J. Casey

AU - Klaus, Adam

AU - Bangs, Nathan L.

AU - Bekins, Barbara

AU - Bücker, Christian J.

AU - Brückmann, Warner

AU - Erickson, Stephanie N.

AU - Hansen, Olav

AU - Horton, Thomas

AU - Ireland, Peter

AU - Major, Candace Olson

AU - Moore, Gregory F.

AU - Peacock, Sheila

AU - Saito, Saneatsu

AU - Screaton, Elizabeth J.

AU - Shimeld, John W.

AU - Stauffer, Philip Henry

AU - Taymaz, Tuncay

AU - Teas, Philip A.

AU - Tokunaga, Tomochika

PY - 1998

Y1 - 1998

N2 - Borehole logs from the northern Barbados accretionary prism show that the plate-boundary decollement initiates in a low-density radiolarian claystone. With continued thrusting, the decollement zone consolidates, but in a patchy manner. The logs calibrate a three-dimensional seismic reflection image of the decollement zone and indicate which portions are of low density and enriched in fluid, and which portions have consolidated. The seismic image demonstrates that an underconsolidated patch of the decollement zone connects to a fluid-rich conduit extending down the decollement surface. Fluid migration up this conduit probably supports the open pore structure in the underconsolidated patch.

AB - Borehole logs from the northern Barbados accretionary prism show that the plate-boundary decollement initiates in a low-density radiolarian claystone. With continued thrusting, the decollement zone consolidates, but in a patchy manner. The logs calibrate a three-dimensional seismic reflection image of the decollement zone and indicate which portions are of low density and enriched in fluid, and which portions have consolidated. The seismic image demonstrates that an underconsolidated patch of the decollement zone connects to a fluid-rich conduit extending down the decollement surface. Fluid migration up this conduit probably supports the open pore structure in the underconsolidated patch.

UR - https://www.scopus.com/pages/publications/84879882884

U2 - 10.1130/0091-7613(1998)026<0811:CPDIAE>2.3.CO;2

DO - 10.1130/0091-7613(1998)026<0811:CPDIAE>2.3.CO;2

M3 - Article

AN - SCOPUS:84879882884

SN - 0091-7613

VL - 26

SP - 811

EP - 814

JO - Geology

JF - Geology

IS - 9

ER -

Consolidation patterns during initiation and evolution of a plate-boundary decollement zone: northern Barbados accretionary prism

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Diğer Dosyalar ve Linkler

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