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The final processing step for a groundmass separates is hand picking under the microscope to remove any polymineral grains or any altered groundmass grains that survived the acid leaching process. Completed groundmass separate that is homogeneous and free of any of crystals. For tephra, pyroclastic and volcaniclastic deposits, samples are crushed, sieved, and washed using the samples methods as those for the groundmass.

After density separations, all minerals are ultrasonically rinsed in acetone and then mounted on glass slides so that mineral compositions can be evaluated using a scanning electron microscope SEM. All argon isotopic analyses were done using a Noblesse 5 collectors mass spectrometer following the procedures of A-InSAR processing for the descending and the ascending orbits were repeated for two different areas, resulting in a total of four processing: i a larger area, extending from the Tyrrhenian coast to the Tiber valley and comprising the sector affected by differential uplift since ka identified in a previous study 1 ; a smaller area corresponding to the MS.

The retrieved results were uploaded into a dedicated GIS, in order to perform an accurate analysis and comparison among the various outcomes. This methodology allows to detect ground displacements with millimeter accuracy by analyzing SAR image stacks, providing the mean ground velocities and the relative displacement time series along the sensor line of sight sensor-target direction, LOS for the coherent targets. The covered temporal period spans from September to March for the descending orbit 84 images and from January to January along the ascending orbit 99 images.

A series of differential interferograms with respect to a single master were generated by the adopted algorithm, aimed to initially select persistent scatterer candidates PSC. The time series of the amplitude values of each pixel were analyzed in order to identify stable targets in the area of interest. The APS contributions were estimated and resampled on the uniform image grid by interpolation. All differential interferograms were then compensated for the estimated atmospheric contribution.

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A joint estimation of both DEM errors and target velocity was then carried out on a pixel-by-pixel basis to obtain the optimized PS velocity estimation. Note that, due to the different angle of view Line of Sight of each orbit, the agreement in terms of sign between the retrieved deformation patterns on both ascending and descending orbits indicates a dominant vertical component of the movement i.

In contrast, the inversion of the retrieved velocities sign reveals a prevalent horizontal component of movement Marra, F. Trasatti, E. Peccerillo, A. Springer, Malinverno, A. Extension in the Tyrrhenian sea and shortening in the Apennines as results of arc migration driven by sinking of the lithosphere. Tectonics 5 , — Patacca, E. Post-Tortonian mountain building in the Apennines.

The role of the passive sinking of a relic lithospheric slab, in The Lithosphere in Italy, edited by A. Boriani, M. Bonafede, G. Vai, Advances in Earth Science Research. Rome, May Atti Conv. Lincei 80 , — Google Scholar.

Acocella, V. Transverse systems along the extensional Tyrrhenian margin of central Italy and their influence on volcanism. Barberi, F. Plio-Pleistocene geological evolution of the geothermal area of Tuscany and Latium. Carta Geol. Serri, G. Geochemical and Petrological evidence of the subduction of delaminated Adriatic continental lithosphere in the genesis of the Neogene-Quaternary magmatism of Central Italy.

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Tectonophysics , — Alfonsi, L. Structural and geochemical features of the Sabina strike-slip fault Central Apennines. Faccenna, C. Il Quaternario 6 , — Bollettino di Geofisica Teorica Applicata 36 , — Low-magnitude earthquakes in Rome: structural interpretation and implications for local stress-field. Frepoli, A. Rovida, A. Istituto Nazionale di Geofisica e Vulcanologia. Piccardi, L. Mapping capable faulting hazard in a moderate-seismicity, high heat-flow environment: the Tuscia province southern Tuscany-northern Latium, Italy.

Bartolucci, G. Il terremoto di Tuscania. Rassegna dei Lavori Pubblici 5 , — Console, R. Studio del terremoto di Tuscania. Annali di Geofisica 25 , — Tertulliani, A. Caldera structure, amount of collapse, and erupted volumes: the case of Bolsena caldera, Italy. Scognamiglio, L. Real-time determination of seismic moment tensor for italian region. Karner, D. The history of the Monti Sabatini and Alban Hills volcanoes: groundwork for assessing volcanic-tectonic hazards for Rome.

Sottili, G. Major explosive activity in the Sabatini Volcanic District central Italy over the ka interval: geochronological - geochemical overview and tephrostratigraphic implications. Quaternary Science Reviews 94 , 74— Scientific Reports 7 , Kuiper, K. Synchronizing rock clocks of Earth history. Jicha, B. Chemical Geology , 54—66 Valentine, G. Tephra ring interpretation in light of evolving maar-diatreme concepts: Stracciacappa maar central Italy. Mattias, P. La regione vulcanica dei monti Sabatini e Cimini.