Authors:
Nagy, EA
Maluski, H
Lepvrier, C
Scharer, U
Thi, PT
Leyreloup, A
Thich, VV
Citation: Ea. Nagy et al., Geodynamic significance of the Kontum massif in central Vietnam: CompositeAr-40/Ar-39 and U-Pb ages from Paleozoic to Triassic, J GEOLOGY, 109(6), 2001, pp. 755-770
Authors:
Agrinier, P
Deutsch, A
Scharer, U
Martinez, I
Citation: P. Agrinier et al., Fast back-reactions of shock-released CO2 from carbonates: An experimentalapproach, GEOCH COS A, 65(15), 2001, pp. 2615-2632
Citation: F. Bodet et U. Scharer, Pb isotope systematics and time-integrated Th/U of SE-Asian continental crust recorded by single K-feldspar grains in large rivers, CHEM GEOL, 177(3-4), 2001, pp. 265-285
Authors:
Roger, F
Tapponnier, P
Arnaud, N
Scharer, U
Brunel, M
Xu, ZQ
Yang, JS
Citation: F. Roger et al., An Eocene magmatic belt across central Tibet: mantle subduction triggered by the Indian collision?, TERRA NOVA, 12(3), 2000, pp. 102-108
Citation: Ea. Nagy et al., Oligo-Miocene granitic magmatism in central Vietnam and implications for continental deformation in Indochina, TERRA NOVA, 12(2), 2000, pp. 67-76
Citation: F. Bodet et U. Scharer, Evolution of the SE-Asian continent from U-Pb and Hf isotopes in single grains of zircon and baddeleyite from large rivers, GEOCH COS A, 64(12), 2000, pp. 2067-2091
Authors:
Scharer, U
Girardeau, J
Cornen, G
Boillot, G
Citation: U. Scharer et al., 138-121 Ma asthenospheric magmatism prior to continental break-up in the North Atlantic and geodynamic implications, EARTH PLAN, 181(4), 2000, pp. 555-572
Citation: L. Kerschhofer et al., Evidence for crystals from the lower mantle: baddeleyite megacrysts of theMbuji Mayi kimberlite, EARTH PLAN, 179(2), 2000, pp. 219-225
Authors:
Faure, M
Lin, W
Shu, LS
Sun, Y
Scharer, U
Citation: M. Faure et al., Tectonics of the Dabieshan (eastern China) and possible exhumation mechanism of ultra high-pressure rocks, TERRA NOVA, 11(6), 1999, pp. 251-258
Authors:
Scharer, U
de Parseval, P
Polve, M
de Saint Blanquat, M
Citation: U. Scharer et al., Formation of the Trimouns talc-chlorite deposit (Pyrenees) from persistenthydrothermal activity between 112 and 97 Ma, TERRA NOVA, 11(1), 1999, pp. 30-37