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10 items by relevance
1 Conference paper

Porosity in Chalk

Fabricius, Ida Lykke

Year: 2017

Language: English

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2 Master Thesis

Porosity preservation effects in chalk (translated: Porøsitetsbevarelse i kalk)

Sommer-Larsen, Peter

DTU Department of Civil Engineering — 2011

Year: 2011

Language: Undetermined

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3 Conference paper

Porosity effects of electrostatic forces in chalk powder

Meireles, Leonardo T.P.; Storebø, Einar M.; Fabricius, Ida L.

Year: 2020

Language: English

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4 Journal article

Porosity in chalk – roles of elastic strain and plastic strain

Fabricius, Ida Lykke

Sedimentology — 2020, Volume 67, Issue 7, pp. 3451-3470

, and because chalks have a simple mineralogy (low magnesium calcite, silica and clays), they are ideal for the study of diagenetic processes including the depth-related decrease of porosity. It is the aim of this study to illustrate how the evaluation of in situ elastic strain can help in understanding

Year: 2020

Language: English

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5 Conference paper

The biot factor: A key to porosity-depth trends in chalk

Fabricius, Ida Lykke; Olsen, Casper; Christensen, H.F.

Sound of Geology. Workshop in Bergen, Norway April 26th - 28th, 2006 — 2006

Year: 2006

Language: English

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6 Conference paper

Porosity loss in chalk facies sediments by physical compaction or by cementation - consequences for P-wave modulus

Fabricius, Ida Lykke

Our Heritage - Key To Global Discovery — 2002

Year: 2002

Language: English

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7 Journal article

ABSTRACT: Porosity Loss in Chalk Facies Sediments by Physical Compaction or by Cementation - Consequences for P-wave Modulus

Ida Lykke Fabricius1

Aapg Bulletin — 2002, Volume 86

Year: 2002

Language: English

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8 Journal article

Stylolites, porosity, depositional texture, and silicates in chalk facies sediments: Ontong Java Plateau - Gorm and Tyra fields, North Sea

Fabricius, Ida Lykke; Borre, Mai K.

Sedimentology — 2007, Volume 54, Issue 1, pp. 183-205

Comparison of chalk on the Ontong Java Plateau and chalk in the Central North Sea indicates that, whereas pressure dissolution is controlled by effective burial stress, pore-filling cementation is controlled by temperature. Effective burial stress is caused by the weight of all overlying water

Year: 2007

Language: English

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9 Book chapter

Poroelasticity of high porosity chalk under depletion

Andreassen, Katrine Alling; Fabricius, Ida Lykke

Poromechanics V — 2013, pp. 2423-2430

levels of pore pressure. The chalk is oil-saturated Lixhe chalk from a quarry near Liège, Belgium, with a general porosity of 45%. Additionally, we compare the theoretical lateral stress to the experimentally determined lateral stress at the onset of pore collapse. The static Biot coefficient based

Year: 2013

Language: English

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10 Conference paper

Mineralogical and textural control on chalk background velocity and porosity

Fabricius, Ida Lykke; Gommesen, L.; Olsen, D.; Springer, N.; Japsen, P.; Jakobsen, F.; et al. (1 more)

Challenge of Discovery — 2005

Year: 2005

Language: English

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