e-mail: dweis@eoas.ubc.ca
phone / tél.: 1-604-822.1697
mobile: 778-386.4466

Vander Auwera J., Weis D., Duchesne J.-C., Marginal mafic intrusions as indicators of downslope draining dense residual liquids in anorthosite diapirs. Li

Vander Auwera J., Weis D., Duchesne J.-C., Marginal mafic intrusions as indicators of downslope draining dense residual liquids in anorthosite diapirs. Lithos, 89, 329-352, 2006.

 

Debaille V., Doucelance R., Weis D., Schiano P. Multi-stage mixing in subduction zones: Application to Merapi Volcano (Java island, Sunda arc. Geochim. Cosmochim. Acta, 70, 723-741, 2006.

 

Ionov D.A., Shirey S.B., Weis D., Brügmann G. Os-Hf-Sr-Nd isotope and PGE systematics of spinel xenoliths from Tok, SE Siberia craton: effects of pervasive metasomatism in shallow refractory mantle. Earth Planet. Sci. Lett, 241, vol. 1-2, 47-64, 2006.

Ionov D., Prikhodko V.S., Bodinier J.-L., Sobolev A.V., Weis D. Lithospheric mantle beneath the south-eastern Siberian craton: petrology of peridotite xenoliths in basa

Ionov D., Prikhodko V.S., Bodinier J.-L., Sobolev A.V., Weis D. Lithospheric mantle beneath the south-eastern Siberian craton: petrology of peridotite xenoliths in basalts from the Tokinsky Stanovik. Contr. Min. Petrol., 149, 647:665, 2005.

 

Nielsen P., Muchez P., Heijlen W., Fallick AET., Keppens E., Weis D., Swennen R. Columnar calcites as testimony of diagenetic overprinting at the boundary between Upper Tournaisian dolomites and limestones (Belgium): multiple origins for apparently similar features. Sedimentology, 52, 945-967, 2005.

 

Ionov D., Blichert-Toft J., Weis D.. Hf-isotopic compositions and HREE variations in off-craton garnet and spinel peridotite xenoliths from Vitim, Siberia. Geochim. Cosmochim. Acta, 69, 2399-2418, 2005.