Page 19 - Tondietall2015

Italian Journal of Geosciences Accepted manuscript

TONDI E., ANTONELLINI M., AYDIN A., MARCHEGIANI L. & CELLO G. (2006) - The role of
deformation bands, stylolites and sheared stylolites in fault development in carbonate grainstones
of Majella Mountain, Italy. Journal of Structural Geology, 28, 376-391.

TONDI E., CILONA A., AGOSTA F., AYDIN A., RUSTICHELLI A., RENDA P. & GIUNTA G. (2012) -
Growth processes, dimensional parameters and scaling relationships of two conjugate sets of
compactive shear bands in porous carbonate grainstones, Favignana Island, Italy. Journal of
Structural Geology, 37, 53-64.

WONG T.-F. & BAUD P. (2012) - The brittle-ductile transition in porous rock: A review. Journal
of Structural Geology, 44, 25-53.

ZHU, W., BAUD, P., WONG, T. F, (2010) - Micromechanics of cataclastic pore collapse in
limestone. Journal of Geophysical. Research 115, B04405.

FIGURE AND TABLE CAPTIONS
Table 1 - Mean values of measured permeability and relative standard deviation (uncertainty).

Fig. 1 - Location map and geological setting of Favignana Insland in the framework of western
Sicily (a) and the northern part of the Majella Mountain (b).

Fig. 2 - Outcrop and thin section images of the studied carbonate grainstones. a) Favignana
grainstones crosscut by oblique normal faults and compactive shear bands. c) Orfento grainstones
cut across by normal faults and compactive shear bands (note the displaced marker bed stained in
green). Favignana (b) and Majella (d) grainstones under an optical microscope (cross-polarized
light).

Fig. 3 - Box and whisker diagram displaying statistics on effective porosity values of
Favignana and Majella carbonate grainstones (a). Pore throat diameter distribution curves of
Favignana and Majella grainstones (b).