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Statements

Subject Item
n2:RIV%2F67985530%3A_____%2F12%3A00387104%21RIV13-AV0-67985530
rdf:type
n8:Vysledek skos:Concept
dcterms:description
This contribution presents a microstucutral study of samples from the Qum-Kuh salt glacier (central Iran) and a salt mine of Neuhof (Germany) representing the extruded part and the source layer of the salt diapiric system, respectively. The main objectives are to identify the active deformation mechanisms and to track the in-situ distribution of fluids, which is the key point to understand the interplay between deformation mechanisms. Intense deformation of the Neuhof rock salt was accommodate by coupled activity of Solution-Precipitation (SP), Grain Boundary (GB) sliding and microcracking of halite grains pointing to the enhancement of continuous SP creep by microcracking. For the salt fountain, GB microstructures and deformation experiments point both to effective GB healing indicating a paradox with microstructural studies of similar rock salts, with evidence for both active dislocation creep and SP creep during the deformation of salt fountains. This contribution presents a microstucutral study of samples from the Qum-Kuh salt glacier (central Iran) and a salt mine of Neuhof (Germany) representing the extruded part and the source layer of the salt diapiric system, respectively. The main objectives are to identify the active deformation mechanisms and to track the in-situ distribution of fluids, which is the key point to understand the interplay between deformation mechanisms. Intense deformation of the Neuhof rock salt was accommodate by coupled activity of Solution-Precipitation (SP), Grain Boundary (GB) sliding and microcracking of halite grains pointing to the enhancement of continuous SP creep by microcracking. For the salt fountain, GB microstructures and deformation experiments point both to effective GB healing indicating a paradox with microstructural studies of similar rock salts, with evidence for both active dislocation creep and SP creep during the deformation of salt fountains.
dcterms:title
The distribution of fluids in natural rock salt to understand deformation mechanisms The distribution of fluids in natural rock salt to understand deformation mechanisms
skos:prefLabel
The distribution of fluids in natural rock salt to understand deformation mechanisms The distribution of fluids in natural rock salt to understand deformation mechanisms
skos:notation
RIV/67985530:_____/12:00387104!RIV13-AV0-67985530
n8:predkladatel
n19:ico%3A67985530
n5:aktivita
n6:I
n5:aktivity
I
n5:dodaniDat
n12:2013
n5:domaciTvurceVysledku
n16:8374694
n5:druhVysledku
n9:C
n5:duvernostUdaju
n15:S
n5:entitaPredkladatele
n17:predkladatel
n5:idSjednocenehoVysledku
131605
n5:idVysledku
RIV/67985530:_____/12:00387104
n5:jazykVysledku
n7:eng
n5:klicovaSlova
deformation mechanisms; halite; fluid-assisted recrystallization
n5:klicoveSlovo
n13:halite n13:deformation%20mechanisms n13:fluid-assisted%20recrystallization
n5:kontrolniKodProRIV
[EF55D084FF44]
n5:mistoVydani
Boca Raton
n5:nazevZdroje
Mechanical behavior of salt VII
n5:obor
n14:DB
n5:pocetDomacichTvurcuVysledku
1
n5:pocetStranKnihy
512
n5:pocetTvurcuVysledku
4
n5:rokUplatneniVysledku
n12:2012
n5:tvurceVysledku
Závada, Prokop Desbois, G. Urai, J. L. Schmatz, J.
s:numberOfPages
10
n11:hasPublisher
CRC Press
n10:isbn
978-0-415-62122-9