Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7830
AuthorsZhu, W. 
Baud, P. 
Vinciguerra, S. 
Wong, T. 
TitleMicromechanics of brittle faulting and cataclastic flow in Alban Hills tuff
Issue Date2011
Series/Report no./116(2011)
DOI10.1029/2010JB008046
URIhttp://hdl.handle.net/2122/7830
KeywordsAlban Hills
Subject Classification04. Solid Earth::04.08. Volcanology::04.08.99. General or miscellaneous 
AbstractAn understanding of how tuff deforms and fails is of importance in the mechanics of volcanic eruption as well as geotechnical and seismic applications related to the integrity of tuff structures and repositories. Previous rock mechanics studies have focused on the brittle strength. We conducted mechanical tests on nominally dry and water-saturated tuff samples retrieved from the Colli Albani drilling project, in conjunction with systematic microstructural observations on the deformed samples so as to elucidate the micromechanics of brittle failure and inelastic compaction. The phenomenological behavior was observed to be qualitatively similar to that in a porous sedimentary rock. Synthesizing published data, we observe a systematic trend for both uniaxial compressive strength and pore collapse pressure of nonwelded tuff to decrease with increasing porosity. To interpret the compaction behavior in tuff, we extended the cataclastic pore collapse model originally formulated for a porous carbonate rock to a dual porosity medium made up of macropores and micropores or microcracks.
Appears in Collections:Papers Published / Papers in press

Files in This Item:
File Description SizeFormat 
40.pdf2.78 MBAdobe PDFView/Open    Request a copy
Show full item record

Page view(s)

37
checked on May 25, 2017

Download(s)

12
checked on May 25, 2017

Google ScholarTM

Check

Altmetric