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In conclusion, our InSAR-based subsidence analysis demonstrates that the area subject to future large-scale collapse is delineated by zones of stable and unstable rock. Areas of stable subsidence are located differentially within the deltaic trough and include subsidence that is offset from the center of the chamber, which can only be determined by the combination of SAR and seismic data. Such areas might include the extension of the lithostratigraphic zones of stability in the sedimentary infill, and might be amenable to the triggering of dynamic events with important implications for the safety of the underground complex. Acknowledgements

We gratefully acknowledge the technical assistance provided by G. Zerr, S.P. Devidze, and D. Di Marzo. This study was conducted as part of the SOPAS project and the Seismohol project (Joint Research Organisation (JRO) and Ministry of National Defence). Our results are based on data selected from the Regional Earth Observation Satellites (REOS) 2-European Seismic Network (ESN) and IKONOS/PALSAR data, which have been processed by the Italian Space Agency and the French space agency, CNES; we are indebted to the Italian Space Agency and the French agency, CNES, for releasing these data for scientific research. We also acknowledge the support of IOVASIS (Italy) and its project SOPAS2. Finally, we thank the reviewers for their comments leading to the improved edition of this manuscript.

Acevedo-Rodriguez, M., Cucakas, S., Badaracco, R., Grassini, L., Aigner, B., and Knez, M. (2014). Fabre's tectonic window: a study of the exhumation of the central Adriatic area on the basis of a continuous 4.0 mm Sesmic device. Advances in Earth Sciences, 46, 122–130.

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