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GeoRef Categories
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Availability
Basilicata Italy
Remobilization of inverted normal faults drives active extension in the axial zone of the southern Apennine mountain belt (Italy) Open Access
Deciphering the Interplay between Reservoir Loading and Dynamic Stresses at the Pertusillo Reservoir Available to Purchase
Fluids‐Triggered Swarm Sequence Supported by a Nonstationary Epidemic‐Like Description of Seismicity Available to Purchase
Geological map of the San Giuliano Lake (Southern Italy): new stratigraphic and sedimentological data Available to Purchase
Fracture stratigraphy of Mesozoic platform carbonates, Agri Valley, southern Italy Available to Purchase
Structural investigation of background features and normal faults affecting the Calcari con Selce formation, Southern Apennines, Italy Available to Purchase
Rift inheritance controls the switch from thin- to thick-skinned thrusting and basal décollement re-localization at the subduction-to-collision transition Available to Purchase
Self-constrained inversion of potential fields through a 3D depth weighting Available to Purchase
Syn-kinematic strata influence the structural evolution of emergent fold–thrust belts Open Access
Abstract Whether thrusts are ramp-dominated and form imbricate fans or run out onto the syn-orogenic surface, forming ‘thrust-allochthons’, is governed by the activity of secondary ‘upper’ detachments along the syn-orogenic surface, activations of which are inhibited by syn-kinematic sedimentation at the thrust front. In the northern Apennines, where thrust systems are ramp-dominated and form an emergent imbricate fan, syn-kinematic sedimentation was abundant and accumulated ahead and above each thrust. In the southern Apennines, the far-travelled Lagronegro allochthon achieved its high displacements (>65 km) while the foredeep basin received little sediment. The imbricate fan at the front of the main Himalayan arc developed within a foredeep that experienced high rates of syn-kinematic sedimentation. In contrast, further west, the Salt Range Thrust emerged into a distal, weakly developed foredeep with significantly reduced rates of sediment accumulation. Displacements were strongly localized onto this thrust (c. 25 km displacement) which activated an upper detachment along the syn-orogenic surface. It is an arrested thrust-allochthon. Lateral variations into the adjacent, ramp-dominated but still salt-detached, Jhelum fold-belt are marked by increases in syn-kinematic sedimentation. As sedimentation styles can vary in space and time, individual thrusts and thrust systems can evolve from being allochthon prone to imbricate dominated.
Naturally Occurring Asbestiform Minerals in Italian Western Alps and in Other Italian Sites Available to Purchase
U-Pb detrital zircon ages and compositional features of Bifurto quartz-rich sandstones from Southern Apennines (Southern Italy): comparison with Numidian Flysch sandstones to infer source area Available to Purchase
Different stacking patterns along an active fold-and-thrust belt—Acerenza Bay, Southern Apennines (Italy) Open Access
1:5,000 geological map of the upper Cretaceous intraplatform-basin succession in the “Gravina di Matera” canyon (Apulia Carbonate Platform, Basilicata, southern Italy) Open Access
Variations of attenuation and V P / V S ratio in the vicinity of wastewater injection: A case study of Costa Molina 2 well (High Agri Valley, Italy) Available to Purchase
REE partition among zircon, orthopyroxene, amphibole and garnet in a high-grade metabasic system Available to Purchase
New insights on the structural setting of the Monte Alpi area, Basilicata, Italy Available to Purchase
Cenozoic tectonic evolution of the northern Apulian carbonate platform (southern Italy) Available to Purchase
Natural CO 2 sites in Italy show the importance of overburden geopressure, fractures and faults for CO 2 storage performance and risk management Available to Purchase
Abstract: The study of natural analogues can inform the long-term performance security of engineered CO 2 storage. There are natural CO 2 reservoirs and CO 2 seeps in Italy. Here, we study nine reservoirs and establish which are sealed or are leaking CO 2 to surface. Their characteristics are compared to elucidate which conditions control CO 2 leakage. All of the case studies would fail current CO 2 storage site selection criteria, although only two leak CO 2 to surface. The factors found to systematically affect seal performance are overburden geopressure and proximity to modern extensional faults. Amongst our case studies, the sealing reservoirs show elevated overburden geopressure whereas the leaking reservoirs do not. Since the leaking reservoirs are located within <10 km of modern extensional faults, pressure equilibration within the overburden may be facilitated by enhanced crustal permeability related to faulting. Modelling of the properties that could enable the observed CO 2 leakage rates finds that high-permeability pathways (such as transmissive faults or fractures) become increasingly necessary to sustain leak rates as CO 2 density decreases during ascent to surface, regardless of the leakage mechanism into the overburden. This work illustrates the value of characterizing the overburden geology during CO 2 storage site selection to inform screening criterion, risk assessment and monitoring strategy. Correction notice: The original version was incorrect. This was due to an error in the Acknowledgements and Funding section, which omitted to list the funding bodies of RSH.