J. Duyster

发表

Crustal evolution of the KTB drill site: From oldest relics to the Late Hercynian granites

B. Stöckhert, P. O'Brien, K. Weber, 1997 .

Post‐Variscan thermal and tectonic evolution of the KTB site and its surroundings

B. Stöckhert, G. Wagner, F. Henjes-Kunst, 1997 .

Grain boundary energies in olivine derived from natural microstructures

B. Stöckhert, J. Duyster, 2001 .

H T-deformation of garnet: an EBSD study on granulites from Sri Lanka, India and the Ivrea Zone

R. Kleinschrodt, J. Duyster, 2002 .

Microdiamond daughter crystals precipitated from supercritical COH + silicate fluids included in garnet, Erzgebirge, Germany

H. Massonne, B. Stöckhert, C. Trepmann, 2001 .

Discontinuous grain growth in recrystallised vein quartz — implications for grain boundary structure, grain boundary mobility, crystallographic preferred orientation, and stress history

B. Stöckhert, Bernhard Stöckhert, Johannes Duyster, 1999 .

Supracrustal intraplate thickening of Variscan basement due to Alpine foreland compression: Results from the superdeep well KTB (Bohemian Massif, Germany)

J. Duyster, G. Zulauf, 1997 .

Calcmylonites and solution transfer in a Devonian reef at Warstein, Germany

J. D. Roo, J. Duyster, K. Weber, 1992 .

Faults and veins in the superdeep well KTB: constraints on the amount of Alpine intra-plate thrusting and stacking of Variscan basement (Bohemian Massif, Germany)

J. Duyster, G. Zulauf, 1997 .

Quartz dislocation microstructure between 7000 m and 9100 m depth from the Continental Deep Drilling Program KTB

G. Dresen, B. Stöckhert, R. Wirth, 1997 .

229 35 O 300 I Time ( Ma ) 250 200 150 100 50 I I I I I Apatite

G. Wagner, F. Henjes-Kunst, H. Ahrendt, 2007 .