Figure F25. Close-up photograph of geopetal structure (interval 194-1199A-2R-3, 28-32 cm). The large void within a rhodolith has been partly filled with foraminiferal wackestone. The infill surface indicates the ancient horizontal plane, which makes an angle with respect to the core edges because of oblique drilling.

Figure F25. Close-up photograph of geopetal structure (interval 194-1199A-2R-3, 28-32 cm). The large void within a rhodolith has been partly filled with foraminiferal wackestone. The infill surface indicates the ancient horizontal plane, which makes an angle with respect to the core edges because of oblique drilling.