Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Rolf H.C. Bruijn"'
Autor:
Rolf H.C. Bruijn, Bjarne Almqvist
Publikováno v:
Geological Society, London, Special Publications. 409:125-147
Experimental compaction curves for mud are key factors in sedimentary basin models but they are poor at predicting porosity evolution beyond 2.5 km depth, where chemical compac- tion dominates shale diagenesis. This study presents the results of expe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b3e5bc3048abb87c6d096d8932ac9fe5
https://doi.org/10.1144/sp409.3
https://doi.org/10.1144/sp409.3
Autor:
Philip Skemer, Rolf H.C. Bruijn
Publikováno v:
Geophysical Research Letters. 41:4894-4903
The grain-size sensitive rheology of orthopyroxene is investigated using data from rheological and microstructural studies. A deformation mechanism map is constructed assuming that orthopyroxene deforms by two independent mechanisms: dislocation cree
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6a2a01837acbac1e77b9f6021f5f6e33
https://doi.org/10.1002/2014gl060607
https://doi.org/10.1002/2014gl060607
Publikováno v:
Earth and Planetary Science Letters. 388:134-142
Article history: Ductile shear zones evolve through complex feedbacks between microstructure and rheology. In the mantle, shear zones often display mylonitic or ultramylonitic microstructures, characterized by extensive grain-size reduction and well-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e36fdd4b5164dd446e9d93bde7c61ce0
https://doi.org/10.1016/j.epsl.2013.11.037
https://doi.org/10.1016/j.epsl.2013.11.037
Publikováno v:
Geophysical Journal International. 192:975-985
Decoupling of paramagnetic and ferrimagnetic AMS development during the experimental chemical compaction of illite shale powder
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fee8d903bd60224e7ce483b4cc51561e
https://doi.org/10.1093/gji/ggs086
https://doi.org/10.1093/gji/ggs086
Publikováno v:
Geomorphology. :156-163
Buso della Rana and Buso della Pisatela are two karstic caves located in north-east Italy. They are part of the same karst system and are developed in the Castelgomberto calcarenitic marine sediments, which were deposited in a shallow Caribbean-type
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8c8467dd7e62bc869f15887cf0d01ff2
https://doi.org/10.1016/j.geomorph.2012.01.025
https://doi.org/10.1016/j.geomorph.2012.01.025