Zobrazeno 1 - 10
of 56
pro vyhledávání: '"William M. Lamb"'
Publikováno v:
Communications Earth & Environment, Vol 4, Iss 1, Pp 1-12 (2023)
Abstract Coal balls are carbonate concretions that preserve peat in cellular detail. Despite their importance to paleobotany, the salinity of coal-ball peat remains controversial. Pennsylvanian coal balls from the Midland and Illinois basins contain
Externí odkaz:
https://doaj.org/article/578847a055e4418eae476ac35504f189
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 19, Iss 10, Pp 3844-3869 (2018)
Abstract Assessing water contents of subduction zone mantle peridotites can gain insight into the compositions of slab‐derived fluids/melts and the active margin water cycle. Here eight mantle xenoliths from Alligator Lake (northern Canadian Cordil
Externí odkaz:
https://doaj.org/article/da751ea82c7d4cbbbb14dec230b3a143
Autor:
Julie Newman, Vasileios Chatzaras, Basil Tikoff, Jan R. Wijbrans, William M. Lamb, Martyn R. Drury
Publikováno v:
Minerals, Vol 11, Iss 12, p 1351 (2021)
We present results from a natural deformed shear zone in the Turon de Técouère massif of the French Pyrenees that directly addresses the processes involved in strain localization, a topic that has been investigated for the last 40 years by structur
Externí odkaz:
https://doaj.org/article/1d46881ca5d74ed9ba0f5f5e93f27a01
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
Autor:
William M. Lamb, Lindsey E. Hunt
Publikováno v:
American Mineralogist. 104:333-347
Publikováno v:
Geological Society, London, Memoirs. 49:75-92
The mantle and crustal sections of the Permian Dun Mountain ophiolite (DMO) in New Zealand9s South Island have similar and potentially related tectonic histories. The mantle section records a four-part sequence of mid-ocean ridge basalt, and boninite
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:
Geological Society of America Abstracts with Programs.
Publikováno v:
Geochemistry, Geophysics, Geosystems. 19:3844-3869
Publikováno v:
Journal of Petrology. 57:751-776