Dynamic and static elastic moduli of North Sea and deep sea chalk

Publication: Research - peer-review › Journal article – Annual report year: 2001

Standard

Dynamic and static elastic moduli of North Sea and deep sea chalk. / Gommesen, Lars; Fabricius, Ida Lykke.

In: Physics and Chemistry of the Earth Part A: Solid Earth & Geodesy, Vol. 26, No. 2, 2001, p. 63-68.

Publication: Research - peer-review › Journal article – Annual report year: 2001

Harvard

Gommesen, L & Fabricius, IL 2001, 'Dynamic and static elastic moduli of North Sea and deep sea chalk' Physics and Chemistry of the Earth Part A: Solid Earth & Geodesy, vol 26, no. 2, pp. 63-68. DOI: 10.1016/S1464-1895(01)00024-2

APA

Gommesen, L., & Fabricius, I. L. (2001). Dynamic and static elastic moduli of North Sea and deep sea chalk. Physics and Chemistry of the Earth Part A: Solid Earth & Geodesy, 26(2), 63-68. DOI: 10.1016/S1464-1895(01)00024-2

CBE

Gommesen L, Fabricius IL. 2001. Dynamic and static elastic moduli of North Sea and deep sea chalk. Physics and Chemistry of the Earth Part A: Solid Earth & Geodesy. 26(2):63-68. Available from: 10.1016/S1464-1895(01)00024-2

MLA

Gommesen, Lars and Ida Lykke Fabricius. "Dynamic and static elastic moduli of North Sea and deep sea chalk". Physics and Chemistry of the Earth Part A: Solid Earth & Geodesy. 2001, 26(2). 63-68. Available: 10.1016/S1464-1895(01)00024-2

Vancouver

Gommesen L, Fabricius IL. Dynamic and static elastic moduli of North Sea and deep sea chalk. Physics and Chemistry of the Earth Part A: Solid Earth & Geodesy. 2001;26(2):63-68. Available from, DOI: 10.1016/S1464-1895(01)00024-2

Author

Gommesen, Lars; Fabricius, Ida Lykke / Dynamic and static elastic moduli of North Sea and deep sea chalk.

In: Physics and Chemistry of the Earth Part A: Solid Earth & Geodesy, Vol. 26, No. 2, 2001, p. 63-68.

Publication: Research - peer-review › Journal article – Annual report year: 2001

Bibtex

@article{3cac643ef3e047379f9ab88cbfedd0b6,
title = "Dynamic and static elastic moduli of North Sea and deep sea chalk",
abstract = "We have established an empirical relationship between the dynamic and the static mechanical properties of North Sea and deep sea chalk for a large porosity interval with respect to porosity, effective stress history and textural composition. The chalk investigated is from the Tor and Hod Formations of the Valhall and Hod fields with reference to calcareous ooze and chalk of the Ontong Java Plateau, ODP Site 807. The acoustic properties of carbonate rock depend primarily on porosity. The main additional parameters are maximum paleo effective stress and inhomogeneity in texture. By correlating the acoustic data of the studied North Sea area with the Ontong Java Plateau data, the paleo effective stress of the studied North Sea area is estimated, and from oedometer modulus and porosity a compaction trend is established. 0 2001 Elsevier Science Ltd. All rights reserved.",
author = "Lars Gommesen and Fabricius, {Ida Lykke}",
year = "2001",
doi = "10.1016/S1464-1895(01)00024-2",
volume = "26",
pages = "63--68",
journal = "Physics and Chemistry of the Earth Part A: Solid Earth & Geodesy",
issn = "1464-1895",
publisher = "Pergamon Press",
number = "2",

}

RIS

TY - JOUR

T1 - Dynamic and static elastic moduli of North Sea and deep sea chalk

AU - Gommesen,Lars

AU - Fabricius,Ida Lykke

PY - 2001

Y1 - 2001

N2 - We have established an empirical relationship between the dynamic and the static mechanical properties of North Sea and deep sea chalk for a large porosity interval with respect to porosity, effective stress history and textural composition. The chalk investigated is from the Tor and Hod Formations of the Valhall and Hod fields with reference to calcareous ooze and chalk of the Ontong Java Plateau, ODP Site 807. The acoustic properties of carbonate rock depend primarily on porosity. The main additional parameters are maximum paleo effective stress and inhomogeneity in texture. By correlating the acoustic data of the studied North Sea area with the Ontong Java Plateau data, the paleo effective stress of the studied North Sea area is estimated, and from oedometer modulus and porosity a compaction trend is established. 0 2001 Elsevier Science Ltd. All rights reserved.

AB - We have established an empirical relationship between the dynamic and the static mechanical properties of North Sea and deep sea chalk for a large porosity interval with respect to porosity, effective stress history and textural composition. The chalk investigated is from the Tor and Hod Formations of the Valhall and Hod fields with reference to calcareous ooze and chalk of the Ontong Java Plateau, ODP Site 807. The acoustic properties of carbonate rock depend primarily on porosity. The main additional parameters are maximum paleo effective stress and inhomogeneity in texture. By correlating the acoustic data of the studied North Sea area with the Ontong Java Plateau data, the paleo effective stress of the studied North Sea area is estimated, and from oedometer modulus and porosity a compaction trend is established. 0 2001 Elsevier Science Ltd. All rights reserved.

U2 - 10.1016/S1464-1895(01)00024-2

DO - 10.1016/S1464-1895(01)00024-2

M3 - Journal article

VL - 26

SP - 63

EP - 68

JO - Physics and Chemistry of the Earth Part A: Solid Earth & Geodesy

T2 - Physics and Chemistry of the Earth Part A: Solid Earth & Geodesy

JF - Physics and Chemistry of the Earth Part A: Solid Earth & Geodesy

SN - 1464-1895

IS - 2

ER -

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