Zobrazeno 1 - 10
of 46
pro vyhledávání: '"K. H. Brodie"'
Autor:
G. T. R. Droop, K. H. Brodie
Publikováno v:
Journal of Metamorphic Geology. 30:843-864
Pelitic hornfelses within the inner thermal aureole of the Etive igneous complex underwent limited partial melting, generating agmatic micro-stromatic migmatites. In this study, observed volume proportions of vein leucosomes in the migmatites are com
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e61dd634223d547cfeaa567eea18db1c
https://doi.org/10.1111/j.1525-1314.2012.01001.x
https://doi.org/10.1111/j.1525-1314.2012.01001.x
Publikováno v:
Geological Society, London, Special Publications. 360:329-336
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0dd4c043527493c01af24242fb3f6ad5
https://doi.org/10.1144/sp360.19
https://doi.org/10.1144/sp360.19
Publikováno v:
Journal of the Geological Society. 165:639-649
Experimental deformation of hot-pressed powders of lizardite serpentinite was carried out to study the effect of the dehydration reaction to olivine + talc + water under controlled pore water pressure. Use of a porous aggregate ensured free movement
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c143994e2f042c5b764e555111325507
https://doi.org/10.1144/0016-76492007-119
https://doi.org/10.1144/0016-76492007-119
Publikováno v:
Journal of Structural Geology. 29:1315-1326
The Karakoram fault shows a full range of fault rocks from ductile (deformation by intracrystalline plasticity) mylonites to low temperature brittle fault rocks along the trace of the fault in the Eastern Karakoram, Ladakh, NW India. The Karakoram fa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f1cf748e158cfd7276edbbd0e5f236fa
https://doi.org/10.1016/j.jsg.2007.05.001
https://doi.org/10.1016/j.jsg.2007.05.001
Publikováno v:
Journal of Metamorphic Geology. 25:423-438
A series of dehydration experiments was carried out on both intact rock and cold-pressed powdered samples of serpentinite at temperatures in the range 535-610 � C, 100-170 � C above the onset of the breakdown temperature of 435 � C. Pore water
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0a4eb48013bb6a03238b89201c619937
https://doi.org/10.1111/j.1525-1314.2007.00703.x
https://doi.org/10.1111/j.1525-1314.2007.00703.x
Publikováno v:
Journal of Structural Geology. 29:1-17
New geological mapping has led to a new interpretation of the large-scale superimposed folding in the upper part of the Ivrea-Verbano zone, Italian Alps. The region is widely held to represent an upended section through lower continental crust of nor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e419b64835ef34db52b12bbf88059208
https://doi.org/10.1016/j.jsg.2006.08.013
https://doi.org/10.1016/j.jsg.2006.08.013
Publikováno v:
Journal of Structural Geology. 28:1569-1587
Layers of fine-grained muscovite were hot-pressed then sheared between alumina sliders to shear strains up to 2, at temperatures between 300 and 700 °C, confining pressures of 206 MPa and various pore water pressures. High pore water pressures helpe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3766957e5958cb0a7ae9e6a8a07c80b4
https://doi.org/10.1016/j.jsg.2006.06.009
https://doi.org/10.1016/j.jsg.2006.06.009
Autor:
Ernest H. Rutter, K. H. Brodie
Publikováno v:
Journal of Structural Geology. 26:2011-2023
Grain size-sensitive flow may be of particular importance in the flow of rocks in natural high-strain zones. Hot-pressed aggregates of synthetic, ultrafine-grained Brazilian quartz of nominal grain sizes 0.4, 1.3 and 4.5 μm were deformed at 300 MPa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a43f1bbe707e2fe0fd2aad2062f2d21d
https://doi.org/10.1016/j.jsg.2004.04.006
https://doi.org/10.1016/j.jsg.2004.04.006
Autor:
Ernest H. Rutter, K. H. Brodie
Publikováno v:
Journal of Structural Geology. 26:259-270
Samples of synthetic, ultrafine-grained quartzite were prepared by hot-pressing aggregates of crushed, clear Brazilian quartz of mean grain size 0.4 μm at 300 MPa and 1373 and 1473 K. The samples displayed rapid grain-growth to ca. 12–20 μm with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e5281c7564aa1ea634781ad05cb71e33
https://doi.org/10.1016/s0191-8141(03)00096-8
https://doi.org/10.1016/s0191-8141(03)00096-8
Autor:
K. H. Brodie, Ernest H. Rutter
Publikováno v:
Journal of the Geological Society. 157:1093-1096
When deformed together in nature, calcite rocks invariably appear weaker and more ductile than quartz rocks. This can be reconciled with experimental flow data only by taking into account grain-size-sensitive (GSS) flow in calcite rocks, which is pre
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dd23cd69d7cecd869dcfbbc0453599c2
https://doi.org/10.1144/jgs.157.6.1093
https://doi.org/10.1144/jgs.157.6.1093