Hans-Rudolf Wenk
University of California, Berkeley
427 Papers
4.9K Citations
Hans-Rudolf Wenk is an academic researcher from University of California, Berkeley. The author has contributed to research in topics: Slip (materials science) & Texture (crystalline). The author has an hindex of 75, co-authored 423 publications. Previous affiliations of Hans-Rudolf Wenk include Los Alamos National Laboratory & Princeton University.
Chat about Author
Papers
Texture and Anisotropy
TL;DR: A review of the literature on preferred orientation of olivine deformation can be found in this paper, where the authors highlight some of the issues with the prevailing view that seismic fast directions align with the flow direction.
1.2K
•Book
Texture and Anisotropy: Preferred Orientations in Polycrystals and their Effect on Materials Properties
U.F. Kocks,Carlos N. Tomé,Hans-Rudolf Wenk +2 more
- 28 Jul 1998
TL;DR: Mecking et al. as mentioned in this paper described the representation of orientations and textures of textured polycrystals, and showed the elastic inclusion problem can be solved with a texture model.
1.1K
Combined texture and structure analysis of deformed limestone from time-of-flight neutron diffraction spectra
TL;DR: In this paper, the orientation distribution of a textured polycrystalline material has been traditionally determined from a few individual pole figures of lattice planes hkl, measured by x-ray or neutron diffraction.
855
•Book
Preferred orientation in deformed metals and rocks : an introduction to modern texture analysis
Hans-Rudolf Wenk
- 01 Jan 1985
TL;DR: In this article, Wenk et al. describe the symmetry of pole figures and textures and their relationship to the texture of the textured surfaces of a porphyrias.
735
Exhumation of ultrahigh-pressure continental crust in east central China: Late Triassic-Early Jurassic tectonic unroofing
Bradley R. Hacker,Lothar Ratschbacher,Laura E. Webb,Michael McWilliams,Trevor Ireland,Andrew J. Calvert,Shuwen Dong,Hans-Rudolf Wenk,Daniel Chateigner +8 more
TL;DR: The largest tract of ultrahigh pressure rocks, the Dabie-Hong'an area of China, was exhumed from 125 km depth by a combination of normal-sense shear from beneath the hanging wall Sino-Korean craton, southeastward thrusting onto the footwall Yangtze craton and orogen-parallel eastward extrusion as discussed by the authors.
714