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Terminologie et interdisciplinarité
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ISSN: 07791666 ISBN: 9068319493 2877233464 9789068319491 Year: 1997 Volume: 93 Publisher: Louvain-la-Neuve : Peeters,


Book
Word 4 et 5 avancé : les macro-commandes
Authors: ---
ISBN: 2501013298 Year: 1991 Volume: 929 Publisher: Bruxelles Marabout

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Word pour Windows : programmation et macro-commandes : versions 2 et 6
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ISBN: 2501019849 Year: 1994 Publisher: Bruxelles Marabout

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Étude comparée de dictionnaires électroniques et de banques de termes
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Year: 1995 Publisher: Bruxelles: Centre de Terminologie de Bruxelles,

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Des termes et des choses : questions de terminologie
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ISBN: 2856081509 9782856081501 Year: 2000 Publisher: Paris : la Maison du dictionnaire,

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Anglais-français, français-anglais
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ISBN: 2501005600 Year: 1984 Publisher: Bruxelles Les nouvelles éditions Marabout

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Elsevier's dictionary of office automation
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ISBN: 0444880658 9780444880659 Year: 1991 Publisher: Amsterdam : Elsevier,


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Français-néerlandais, néerlandais-français
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ISBN: 2501006712 Year: 1985 Publisher: Bruxelles Les nouvelles éditions Marabout

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Théories sémantiques et métaphore : réflexions critiques
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Year: 1977 Publisher: Louvain-la-Neuve: UCL,

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Dissertation
Quantitative assessment of the dolomitizing potential arising from interaction of seawater with igneous dikes and carbonate host-rock
Authors: --- ---
Year: 2016 Publisher: Leuven KU Leuven. Faculteit Wetenschappen

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Dolomitization is the process of altering calcite (CaCO3) into dolomite (CaMg(CO3)2), for this a fluid with a high enough Mg content relative to its Ca content is needed. The oil industry especially is interested in dolomitization since it often results in an increase in porosity, which means that it can provide better oil reservoirs. Several models exist to explain dolomitization. The KU Leuven has developed a new model based on the Latemar platform (northern Italy). In the Latemar platform ferroan dolomite and dolomite is found adjacent to the dikes (ferroan dolomite is dolomite where some of its Mg is replaced by Fe). Based on this a model was developed where seawater first interacted with mafic, igneous dikes, resulting in an increase in the Fe and possibly the Mg content of the seawater. Then this modified seawater flowed into the carbonate (calcite) country rock and induced dolomitization. This thesis explored the same concept by performing geochemical modelling. With geochemical software packages the interaction between the fluid and the rocks was studied. The influence of the seawater and dike composition on the subsequent dolomitization was investigated. One part of this was replacing the Latemar composition, which consists of the rare shoshonite, with the most common magma type on earth: mid-ocean ridge basalt (MORB). The influence of the dike composition was investigated by varying the plagioclase, olivine and clinopyroxene content. The highest dolomitizing potential, defined by the saturation index of dolomite or the Mg/Ca ratio, is obtained at low plagioclase and clinopyroxene contents and a high olivine content. To investigate the influence of the seawater composition, tests were performed with Triassic seawater and with modern seawater. Additionally, the pe, SO4-2, pCO2, HCO3- and Mg+2 contents were varied. These tests showed that the highest dolomitizing potential is obtained at reducing conditions, high HCO3-, high Mg+2, intermediate pCO2 and intermediate to high SO4-2 contents and that the dolomitizing potential of modern seawater is higher than that of Triassic seawater. When compared to the unmodified seawater the fluid resulting from the seawater-MORB dike interaction had a lower dolomitizing potential. This is because the alteration of the dikes acts as a Mg sink, Mg-bearing minerals like chlorite and talc are precipitated. However, calculations showed that there was little difference in the amount of dolomite formed by modified and unmodified seawater. Unlike in the Latemar system, interaction with MORB didn’t result in stabilization of ferroan dolomite, to accomplish this an extra Fe source is needed.

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