Fabio Trippetta

TL;DR: In this paper, the structure of large displacement (>100 m) normal faults is given by 1) a zoned fault core with a wider portion of fault-parallel foliated Ca-sulphates (ductile deformation), overprinted by an inner fault core (IFC) of localized brittle deformation, and 2) wide (dolostones) to absent (Ca-sulas) damage zones of fault fracture patterns.

TL;DR: In this article, the pore system is a combination of depositional and diagenetic processes and the dominant porosity types include fracture, interparticle, intra-particle and moldic porosity; NMR indicates mesopores to macropores, and geochemical analysis indicates a self-sourced unconventional reservoir based on its organic richness characteristics unconventional resource opportunity as tight carbonate reservoir, and it is a potential conventional resource.

TL;DR: In this article, the Triassic Evaporites (TE) of the Umbria-Marche Apennines, a sedimentary succession made up of a sequence of alternating sulphates (anhydrites and gypsum) and dolostones, represent a key lithology in terms of sealing properties and earthquake triggering.

TL;DR: In this paper, the uniaxial compressive strength (UCS), Young's modulus and Poisson's ratio, both static and dynamic, of the seismogenic Triassic Evaporites of the Northern Apennines were reported.

TL;DR: In this article, the authors presented a multi-scale investigation of a normal fault exhumed from seismogenic depths, which extends for a length of 10 km with a maximum width of about 1.5 km and consists of five sub-parallel and interacting segments.