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Published byEsmond Juniper Greene Modified over 8 years ago
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En echelon extension fractures as precursors for a shear fracture
En echelon extension fractures as precursors for a shear fracture. Staining of K-feldspar by fluid-rock interaction as fluids flowed along incipient fractures, Øygarden, Norway © Haakon Fossen
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Stylolite, bed-parallel, UT
© Haakon Fossen
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Stylolites in carbonate sandstone, San Rafael Reef, Utah
© Haakon Fossen
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Stylolite, tectonic, normal to bedding, formed during Laramide layer-parallel shortening, San Rafael Reef, Utah © Haakon Fossen
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Single cataclatic deformation band, Goblin Valley, Utah
© Haakon Fossen
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Cataclastic deformation bands (left) and non-cataclastic (disaggregation) bands (larger offsets), Chimney Rock, Utah © Haakon Fossen
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Shear-enhanced compaction band, Valley of Fire
© Haakon Fossen
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Pure compaction band, Chevron-type,Valley of Fire.
© Haakon Fossen
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Pure compaction bands and shear-enhanced compaction bands, Utah
© Haakon Fossen
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Cataclastic deformation band, Nubian Sst, Sinai
© Haakon Fossen
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Deformation band cluster zone, Goblin Valley, Utah
© Haakon Fossen
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Conjugate normal deformation bands, Goblin Valley, Utah
© Haakon Fossen
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Conjugate normal deformation bands and deformation band zones, Provence
© Haakon Fossen
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Conjugate reverse deformation bands, Arroy Grande, California
© Haakon Fossen
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Reverse deformation band cluster bounding hydrocarbon filled compartment in sandstone, ArroyGrande, California © Haakon Fossen
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