FN Archimer Export Format
PT J
TI Grain Deformation Processes in Porous Quartz Sandstones – Insight from the Clusters of Cataclastic Deformation Bands
BT 
AF Philit, Sven
   Soliva, Roger
   Ballas, Gregory
   Fossen, Haakon
AS 1:1;2:1;3:2;4:3,4;
FF 1:;2:;3:PDG-REM-GM-LAD;4:;
C1 Université de Montpellier, France
   Ifremer (Brest), France
   University of Bergen, Norway
   Universidade de São Paulo, Brazil
C2 UNIV MONTPELLIER, FRANCE
   IFREMER, FRANCE
   UNIV BERGEN, NORWAY
   UNIV SAO PAULO, BRAZIL
SI BREST
SE PDG-REM-GM-LAD
TC 0
UR https://archimer.ifremer.fr/doc/00471/58269/60789.pdf
LA English
DT Article
AB Porous sandstones represent classical reservoirs for water or hydrocarbons. Deformation in such granular material is due to tectonic events and occurs through the process of cataclasis, implying the crushing of the grains to a diversity of smaller clasts. Cataclasis is generally accompanied by porosity and permeability decrease. Although it is known that cataclastic deformation localizes to form individual bands and clusters of bands, the parameters controlling the distribution of this deformation were not well understood until recently. We used scanline measurements to show a favoured localization and clustering of the deformation on the case of normal-fault stress regime and potentially in strike-slip fault regime. The reverse regime favours the formation of distributed networks of conjugate deformation bands. At the scale of a cluster, field data reveals that the minimum modal grain size value of the host sandstone(s) controls the band density. Finally, microscopic cathodoluminescence analysis reveals enhanced quartz cementation for high degree of cataclasis. Hence, because band clustering, high degree of cataclasis and band cementation are favoured in normal-fault stress regime, tectonic extension appears to be favourable conditions for the formation of efficient barriers to fluid-flow in porous sandstone reservoirs. 
PY 2017
SO EPJ Web of Conferences
SN 2100-014X
PU EDP Sciences
VL 140
DI 10.1051/epjconf/201714007002
ID 58269
ER

EF