Zobrazeno 1 - 10
of 385
pro vyhledávání: '"Hans Rudolf Wenk"'
Publikováno v:
Geophysical Journal International. 234:790-806
SUMMARYThe seismic anisotropy of the Earth's solid inner core has been the topic of much research. It could be explained by the crystallographic preferred orientation (CPO) developing during convection. The likely phase is hexagonal close-packed iron
Publikováno v:
Journal of Applied Crystallography. 56:135-142
Previously, synchrotron X-ray Laue microdiffraction has been used to measure the magnitudes of residual strain in materials. Recently the method was advanced to determine the orientation of the strain ellipsoid and applied to naturally deformed quart
Autor:
Xiang Wu, Jung-Fu Lin, Pamela Kaercher, Zhu Mao, Jin Liu, Hans-Rudolf Wenk, Vitali B. Prakapenka
Publikováno v:
Nature Communications, Vol 8, Iss 1, Pp 1-6 (2017)
The source of the anisotropic layer (D'' layer) at the bottom of the lower mantle remains unclear. Here, using high pressure and temperature experiments, the authors find that seismic anisotropy observed at the D'' layer is caused by 50% deformation
Externí odkaz:
https://doaj.org/article/d8982ddc235a46518ee587199935142e
Autor:
Robert E. Hermes, Hans-Rudolf Wenk, James P. Kennett, Ted E. Bunch, Christopher R. Moore, Malcolm A. LeCompte, Gunther Kletetschka, A. Victor Adedeji, Kurt Langworthy, Joshua J. Razink, Valerie Brogden, Brian Van Devener, Jesus Paulo Perez, Randy Polson, Matt Nowell, Allen West
Many studies of hypervelocity impact craters have described the characteristics of quartz grains shock-metamorphosed at high pressures of >10 GPa, but in contrast, few studies have investigated shock metamorphism at lower shock pressures. In this stu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::80aa48ddb40325bdcd25d52f6b47fc18
https://doi.org/10.20944/preprints202305.1728.v1
https://doi.org/10.20944/preprints202305.1728.v1
Publikováno v:
Geophysical Journal International. 227:1665-1681
SUMMARY The presence of seismic anisotropy at the base of the Earth's mantle is well established, but there is no consensus on the deformation mechanisms in lower mantle minerals that could explain it. Strong anisotropy in magnesium post-perovskite (
Autor:
Daniela Ushizima, Hans-Rudolf Wenk, Mary Scott, Ke Xu, Jiaqi Li, Panod Viseshchitra, Peter Ercius, Paulo J.M. Monteiro
Publikováno v:
Journal of the American Ceramic Society. 104:1852-1862
Author(s): Viseshchitra, P; Ercius, P; Monteiro, PJM; Scott, M; Ushizima, D; Li, J; Xu, K; Wenk, HR | Abstract: © 2020 American Ceramic Society (ACERS) Calcium silicate hydrate (C-S-H), is the principal hydration product of Portland cement that main
Autor:
Yao Li, Fengying Zhang, Nobumichi Tamura, Hans-Rudolf Wenk, Huijun Kang, Kai Chen, Ching-Shun Ku, Xiaofeng Dang
Publikováno v:
Journal of Applied Crystallography. 53:1392-1403
XtalCAMP is a software package based on the MATLAB platform, which is suitable for, but not limited to, the analysis and visualization of scanning Laue X-ray micro-/nanodiffraction data. The main objective of the software is to provide complementary
Publikováno v:
Geophysical Journal International. 222:1363-1378
Author(s): Wenk, HR; Chandler, BC; Chen, K; Li, Y; Tamura, N; Yu, R | Abstract: If a crystal lattice is subjected to a stress, it becomes distorted and no longer represents the ideal crystal symmetry, and if the stress introduces defects such as disl
Publikováno v:
Acta Materialia. 189:284-298
A bridgmanite/periclase aggregate is investigated due to its prevalence in the Earth’s lower mantle and its importance for understanding geodynamic processes. In dual-phase polycrystalline aggregates, both strength contrast between phases and singl
Publikováno v:
Journal of Structural Geology. 125:319-324
This report describes microstructures and preferred orientation of a Devonian slate from the Belgian Ardennes (La Fortelle quarry). The sample, composed largely of muscovite, chlorite, and quartz, displays extraordinary texture strength of muscovite,