Article ID Journal Published Year Pages File Type
4733110 Journal of Structural Geology 2014 11 Pages PDF
Abstract

•Ancient Roman marble slabs were analysed to visualize their internal fold structure.•3D images of numerous meter-scale sheath and curtain folds were produced.•Sheath folds were generated by a single phase of constrictional non-coaxial flow.•Cross-section geometry is not a precise indicator of a sheath fold's 3D orientation.

Archaeological excavations and restoration of a palatial Roman housing complex in Ephesos, Turkey yielded 40 wall-decorating plates of folded mylonitic marble (Cipollino verde), derived from the internal Hellenides near Karystos, Greece. Cipollino verde was commonly used for decoration purposes in Roman buildings. The plates were serial-sectioned from a single quarried block of 1,25 m3 and provided a research opportunity for detailed reconstruction of the 3D geometry of meterscale folds in mylonitized marble. A GOCAD model is used to visualize the internal fold structures of the marble, comprising curtain folds and multilayered sheath folds. The sheath folds are unusual in that they have their intermediate axis normal to the parent layering. This agrees with regional tectonic studies, which suggest that Cipollino verde structures formed by local constrictional non-coaxial flow. Sheath fold cross-section geometry, exposed on the surface of a plate or outcrop, is found to be independent of the intersection angle of the fold structure with the studied plane. Consequently, a single surface cannot be used as an indicator of the three-dimensional geometry of transected sheath folds.

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Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology
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