References of "Vander Auwera, Jacqueline"
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See detailThe jotunitic and the acidic igneous rocks
Vander Auwera, Jacqueline ULg; Bolle, Olivier ULg; Duchesne, Jean-Clair ULg

in Duchesne, Jean-Clair (Ed.) The Rogaland Intrusive Massifs: an excursion guide (2001)

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See detailThe Rogaland intrusive massifs: eastern part
Duchesne, Jean-Clair ULg; Demaiffe, Daniel; Vander Auwera, Jacqueline ULg et al

in Duchesne, Jean-Clair (Ed.) The Rogaland intrusive massifs: an excursion guide (2001)

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See detailTi deposits in anorthosite; geochemical constraints on the economic value
Duchesne, Jean-Clair; Vander Auwera, Jacqueline ULg

in Proceedings of the Biennial SGA Meeting (2001), 6

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See detailPetrology and geochemistry of rapakivi-type granites from the crystalline basement of NE Poland
Baginski, Boguslaw; Duchesne, Jean-Clair ULg; Vander Auwera, Jacqueline ULg et al

in Geological Quarterly (2001), 45(1), 33-52

The collection of 80 rock samples coming from drillcores of 8 localities from the Mazury Complex (Polish part of the crystalline East European Craton) and representing different rock types from ... [more ▼]

The collection of 80 rock samples coming from drillcores of 8 localities from the Mazury Complex (Polish part of the crystalline East European Craton) and representing different rock types from monzodiorites to leucogranites, were studied for major, trace and REE elements by XRF and ICP-MS methods. The range in composition of investigating rocks varies from 46% to 76% SiO2 contents. All of them show similar REE distributions, what suggests that they are genetically linked. They also plot along a major trend with many similarities to the jotunitic liquid line of descent (LLD) defined in AMCG rocks from Rogaland (Norway). Each group of rocks has however its own characteristics considering specific elements, such as REE, Sr or Zr. [less ▲]

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See detailGeochemical constraints on the petrogenesis of the O'okiep intrusive rocks (Namaqualand, S. Africa) : a lower crustal mafic source
Duchesne, Jean Clair; Vander Auwera, Jacqueline ULg; Clifford, Tom

in Journal of Conference Abstracts (2001), 6

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See detailDyke swarms in the Pan-African basement from the Alpine Danubian window : new field and geochemical investigation in southern Carpathians (Romania)
Femenias, Olivier; Demaiffe, Daniel; Liégeois, Jean-Paul ULg et al

in Journal of Conference Abstracts (2001), 6

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See detailGeochemistry of Upper Cretaceous high-K calc-alkaline post-collisional intrusions in the Banat Province (western south Carpathians, Romania)
Dupont, Alain; Vander Auwera, Jacqueline ULg; Pin, Christian et al

in Journal of Conference Abstracts (2001), 6

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See detailExperimental determination of phase equilibria of the Lyngdal granodiorite (southern Norway)
Bogaerts, Michel; Scaillet, Bruno; Vander Auwera, Jacqueline ULg

in Journal of Conference Abstracts (2001), 6

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See detailGeochemistry of granitoids from the south Carpathians: A review
Berza, Tudor; Andar, Petre; Tatu, Mihai et al

in Anuarul Institutului Geologic al României (2000), 71

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See detailThe effect of pressure on DSr (plag/melt) and DCr (opx/melt): implications for anorthosite petrogenesis
Vander Auwera, Jacqueline ULg; Longhi, John; Duchesne, Jean-Clair ULg

in Earth & Planetary Science Letters (2000), 178

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See detailSome phase equilibrium constraints on the origin of Proterozoic Massif anorthosites and related rocks
Longhi, John; Vander Auwera, Jacqueline ULg; Fram, Miranda et al

in Journal of Conference Abstracts (1999), 41

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See detailThe crustal tongue melting model and the origin of massive anorthosites
Duchesne, Jean-Clair ULg; Liégeois, Jean-Paul ULg; Vander Auwera, Jacqueline ULg et al

in Terra Nova (1999), 11

Recent detailed field studies in several anorthosite complexes have shown that anorthosites are frequently linked with weakness zones in the crust which favour their emplacement at mid-crust levels ... [more ▼]

Recent detailed field studies in several anorthosite complexes have shown that anorthosites are frequently linked with weakness zones in the crust which favour their emplacement at mid-crust levels. Recent experimental data have also shown that the parent magma compositions of various anorthosite massifs lie on thermal highs in the relevant phase diagrams, indicating that these magmas cannot be derived by fractionation of peridotitic mantle melts but rather are produced by melting of gabbronoritic sources. In the Sveconorwegian province terrane boundaries have been traced in deep seismic profiles to Moho offsets or to tongues of lower crustal material underthrust to depths of 40-50 km. We therefore suggest that the parent magmas of anorthosite massifs are produced by melting of gabbronoritic rocks from the lower crust that had been thrust into the mantle by collision of terranes. [less ▲]

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See detailCharnockites: the lower crust connection
Duchesne, Jean Clair; Vander Auwera, Jacqueline ULg; Bolle, Olivier ULg

in Documents du BRGM (1999), 290

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See detailSome phase equilibrium constraints on the origin of Proterozoic (massif) anorthosites and related rocks
Longhi, John ULg; Vander Auwera, Jacqueline ULg; Fram, Miranda S. et al

in Journal of Petrology (1999), 40

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See detailPyrométamorphisme induit par la gézéification souterraine de niveaux charbonneux du Westphalien dans le Bassin de Mons (Belgique)
Nzali, Timothée; Duchesne, Jean-Clair ULg; Jacquemin, Christiane et al

in Geologica Belgica (1999), 2(3-4), 221-234

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See detailPotassic and ultrapotassic dikes around the plutons of Biella and Traversella
Bogaerts, Michel; Vander Auwera, Jacqueline ULg

in Documents du BRGM (1999), 290

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See detailPan-african acidic magmatism in the south Carpathians (Romania): from calc-alkaline to shoshonitic and back
Berza, Tudor; Duchesne, Jean Clair; Vander Auwera, Jacqueline ULg et al

in Documents du BRGM (1999), 290

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