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Deformed marbles containing green metachert layers which are transected by multiple stylolites during oblique collision in the Zagros orogenic belt. Subhorizontal sylolites are overpinted by steep ones. It is unclear whether the displacement of layer fragments is solely due to dissolution on stylolites or if it is due to displacement in domino boudinage, with subsequent lateral shortening. PhotoID191

Faghih, A., 2008. Structural evolution of accretion and collision processes of the Zagros orogeny, Iran. Unpublished PhD thesis, Shiraz University,Shiraz , Iran.
Sarkarinejad, K., Faghih, A., Grasemann, B., 2008. Transpressional deformations within the Sanandaj-Sirjan Metamorphic Belt (Zagros Mountains, Iran). Journal of Structural Geology 30, 818–82

This is a Journal of Structural Geology Photograph of the Month

Deformed marbles containing green metachert layers which are transected by multiple stylolites during oblique collision in the Zagros orogenic belt. Subhorizontal sylolites are overpinted by steep ones. It is unclear whether the displacement of layer fragments is solely due to dissolution on stylolites or if it is due to displacement in domino boudinage, with subsequent lateral shortening. PhotoID191

Faghih, A., 2008. Structural evolution of accretion and collision processes of the Zagros orogeny, Iran. Unpublished PhD thesis, Shiraz University,Shiraz , Iran.
Sarkarinejad, K., Faghih, A., Grasemann, B., 2008. Transpressional deformations within the Sanandaj-Sirjan Metamorphic Belt (Zagros Mountains, Iran). Journal of Structural Geology 30, 818–82

This is a Journal of Structural Geology Photograph of the Month

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