Zobrazeno 1 - 10
of 48
pro vyhledávání: '"J. Zulauf"'
Publikováno v:
Zeitschrift der Deutschen Gesellschaft für Geowissenschaften. 173:167-191
Publikováno v:
Journal of Structural Geology. 172:104890
Akademický článek
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Publikováno v:
Journal of Structural Geology. 118:324-339
Dome-in-dome structures are frequent in salt provinces and in high-grade rocks of orogens. Their origin is only poorly understood. In the present study we have modelled dome-in-dome structures, which result from constrictional (radial) in-plane short
Autor:
G. Zulauf, J. Zulauf, J. Linckens, A. Gerdes, E. Hattingen, F. Loeckle, H.R. Marschall, L. Steckenreiter
Publikováno v:
Journal of Structural Geology. 155:104525
Publikováno v:
Journal of Structural Geology. 100:120-129
The geometrical parameters of natural folds are used by structural geologists to estimate finite strain and rheological properties of deformed rocks. The relation between geometry and rheology is well understood in cases of cylindrical folds, but is
Autor:
Gernold Zulauf, H.R. Marschall, Rainer Petschick, Harro Schmeling, Thomas Reischmann, J. Zulauf, Axel Gerdes, F. Loeckle, E. Hattingen, Heinz-Dieter Nesbor, H.E. Hoefer
Publikováno v:
Tectonophysics. 805:228774
We present geochronological, thermobarometric and computertomographic data from a composite sill exposed in the Weschnitz pluton of the Variscan Odenwald. The wall rock consists of quartzmonzodiorite, which intruded at deep structural levels (P = ca.
Publikováno v:
Journal of Structural Geology. 145:104303
We present results of scaled analogue modelling, which show the influence of varying single-layer inclination on the geometry of folds produced by high coaxial plane strain (eZ = −70%). The initial angle (θX(i)) between the competent layer and the
Publikováno v:
Journal of Structural Geology. 141:104217
We carried out scaled analogue modelling to show the influence of varying layer obliquity on the geometry of single-layer folds and boudins, which developed simultaneously under coaxial plane strain. The initial angle (θZ(i)) between the competent l
Publikováno v:
Journal of Structural Geology. 90:1-14
Dome and basin folds are structures with circular or slightly elongate outcrop patterns, which can form during single- and polyphase deformation in various tectonic settings. We used power-law viscous rock analogues to simulate single-phase dome-and-