Zobrazeno 1 - 10
of 55
pro vyhledávání: '"Andreas K. Kronenberg"'
Autor:
Joseph W. Millard, Caleb W. Holyoke, Rachel K. Wells, Cole Blasko, Andreas K. Kronenberg, Paul Raterron, Casey Braccia, Nicholas Jackson, Caleb A. McDaniel, Leif Tokle
Publikováno v:
Geosciences, Vol 9, Iss 10, p 420 (2019)
We determined the activation volumes (V*) for polycrystalline magnesite with grain sizes of 2 and 80 µm deforming by low temperature plasticity (LTP) mechanisms (kinking and dislocation glide), diffusion creep, and dislocation creep at temperatures
Externí odkaz:
https://doaj.org/article/2a53d01077af41b6bc4351299a494636
Autor:
Abhishek Prakash, Caleb W. Holyoke, Peter B. Kelemen, Stephen H. Kirby, Andreas K. Kronenberg, William M. Lamb
Publikováno v:
Proceedings of the National Academy of Sciences. 120
A model for intermediate-depth earthquakes of subduction zones is evaluated based on shear localization, shear heating, and runaway creep within thin carbonate layers in an altered downgoing oceanic plate and the overlying mantle wedge. Thermal shear
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c56a1e76ed0cdf532268290d1e75397f
https://doi.org/10.1073/pnas.2219076120
https://doi.org/10.1073/pnas.2219076120
Autor:
Andreas K. Kronenberg, Stephen H. Kirby, Abhishek Prakash, Caleb W. Holyoke, William M. Lamb, Peter B. Kelemen
Seismicity of subduction zones at upper-mantle depths is commonly explained by dehydration reactions of serpentine and hydrous silicates and reductions in effective pressure. However, the conditions of Wadati-Benioff zone seismicity do not strictly c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::febf69453f6e6ef736c6baf83f00b2a9
https://doi.org/10.5194/egusphere-egu2020-12631
https://doi.org/10.5194/egusphere-egu2020-12631
Publikováno v:
Journal of Geophysical Research: Solid Earth. 123:4676-4696
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::63e85be0b4bd3db77ad3ba54bbfa0744
https://doi.org/10.1029/2017jb015133
https://doi.org/10.1029/2017jb015133
Autor:
Andreas K. Kronenberg, Thomas van der Werf, Leo M. Kriegsman, Vasileios Chatzaras, Basil Tikoff, Martyn R. Drury
Publikováno v:
Solid Earth, Vol 8, Pp 1211-1239 (2017)
Solid Earth, 8(6), 1211. Elsevier
Solid Earth, 8(6), 1211. Elsevier
The rheology of lower crust and its transient behavior in active strike-slip plate boundaries remain poorly understood. To address this issue, we analyzed a suite of granulite and lherzolite xenoliths from the upper Pleistocene–Holocene San Quintí
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e134d2d5bf41b5b1bc2f2cc88d437988
https://www.solid-earth.net/8/1211/2017/se-8-1211-2017.pdf
https://www.solid-earth.net/8/1211/2017/se-8-1211-2017.pdf
Autor:
Caleb W. Holyoke, Andreas K. Kronenberg, Hasnor F. B. Hasnan, Zhenxian Liu, Richard D. Law, Jay B. Thomas
Publikováno v:
Solid Earth, Vol 8, Pp 1025-1045 (2017)
Previous measurements of water in deformed quartzites using conventional Fourier transform infrared spectroscopy (FTIR) instruments have shown that water contents of larger grains vary from one grain to another. However, the non-equilibrium variation
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::74839a68454c1f9515c1f17e2ad73afd
https://doi.org/10.5194/se-8-1025-2017
https://doi.org/10.5194/se-8-1025-2017
Publikováno v:
Journal of Geophysical Research: Solid Earth. 121:3278-3299
Small-scale shear zones within the Permian Truzzo meta-granite developed during the Alpine orogeny at amphibolite facies conditions. In these shear zones magmatic quartz deformed by dislocation creep and recrystallized dynamically by grain boundary m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3361c090f6484c6f0a65dc4e231ae67c
https://doi.org/10.1002/2015jb012771
https://doi.org/10.1002/2015jb012771
Publikováno v:
Journal of Structural Geology. 69:449-464
Dolomite aggregates deformed by dislocation creep over a wide range of conditions (T = 700–1000 °C, effective pressure of 900 MPa, strain rates of 10−7 – 10−4/s) strain weaken by up to 75% of the peak differential stress. Microstructural stu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ce6132a910274541b9602e4d21b7afd1
https://doi.org/10.1016/j.jsg.2014.04.008
https://doi.org/10.1016/j.jsg.2014.04.008
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cf7a2769aefc672f09e3b9bc021a032d
https://doi.org/10.1130/abs/2017am-300920
https://doi.org/10.1130/abs/2017am-300920
Autor:
Leif Tokle, Cole Blasko, Andreas K. Kronenberg, Paul Raterron, Caleb W. Holyoke, Nicholas Jackson
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a80c4a054c321a046798a69c43d1627b
https://doi.org/10.1130/abs/2017ne-290651
https://doi.org/10.1130/abs/2017ne-290651