Results 11 to 20 of about 217 (106)
Prediction of Stress-Strain Curves Based on Hydric Non-Destructive Tests on Sandstones. [PDF]
This research received no external funding.The study of the mechanical behavior of building stones is traditionally supported by destructive compression tests carried out on representative specimens. However, in order to respect the monuments' integrity,
Ludovico-Marques M, Chastre C.
europepmc +3 more sources
Abstract The evolution of the Apennine wedge has seen the time‐space migration of the forebulge, foredeep, thrust wedge, and back‐arc extension phases in the wake of the Eastward rollback of the subducting Adria slab. In this framework, thrusting and post‐orogenic extensional faulting have occurred in two parallel forelandward‐migrating ribbons, with ...
S. Tavani +11 more
wiley +1 more source
Tectono‐stratigraphic evolution of the central‐southern Apennine foreland basin system. The shape and migration rate of the foreland basin is constrained by a new high‐resolution regional dataset of Sr‐isotope dating for the base of the time‐transgressive shallow‐water carbonate unit at the bottom of the foreland basinal megasequence sealing the ...
Monia Sabbatino +8 more
wiley +1 more source
Abstract The Tyrrhenian back‐arc basin developed at the rear of the E‐ward migrating Apennine fold‐and‐thrust belt, with northward decreasing rollback of the subducting Adria slab leading to northward fading of back‐arc extension. The northern portion of the Tyrrhenian basin is made of thinned continental crust, whereas in the central/southern portion ...
S. Tavani +8 more
wiley +1 more source
Abstract Fluid‐rock interaction in ultramafic rocks considerably affects the chemical and isotopic composition of the oceanic lithosphere. We present a geochemical and petrological study of serpentinites and ophicalcites of the Northern Apennine ophiolite, Italy.
Esther M. Schwarzenbach +3 more
wiley +1 more source
Geochemical Modeling of Water‐Rock Interaction Processes in the Pollino National Park
This work is aimed at reconstructing the water‐rock interaction processes controlling the geochemical characteristics of the shallow or relatively shallow groundwaters of the Pollino National Park, based on the data acquired for 105 water samples from local springs.
C. Apollaro +7 more
wiley +1 more source
Fluid inclusion study of the Boccassuolo VMS-related stockwork deposit (Northern-Apennine ophiolites, Italy) [PDF]
Several Cyprus-type volcanogenic massive sulphide (VMS) deposits are found in the Jurassic ophiolitic series of the Northern Apennines. Stratabound, stratiform and stockwork deposits were formed in the western limb of the Neotethys (Ligurian Ocean) and ...
Federica Zaccarini +2 more
core +5 more sources
Gravity modelling along CROP04 seismic profile [PDF]
The processing and interpretation of seismic lines, together with the analysis of surficial geological data and hydrocarbon wells data, are powerful tools for the investigation of crust structures. Nevertheless, for depths exceeding that portion of crust
Aguilera, A. R. +17 more
core +1 more source
The architecture of the European-Mediterranean lithosphere: A synthesis of the Re-Os evidence [PDF]
Rhenium-depletion model ages (TRD) of sulfi des in peridotite xenoliths from the subcontinental mantle beneath central Spain (the Calatrava volcanic fi eld) reveal that episodes of mantle magmatism and/or metasomatism in the Iberia microplate were ...
Ancochea Soto, Eumenio +9 more
core +2 more sources
Petrology, geochemistry and origin of the sierra de baza ophiolites (Betic cordillera, Spain) [PDF]
In this work we present for the first time a petrological-geochemical and genetic study of the Sierra de Baza ophiolites, which represent one of the ophiolitic occurrences of the Betic Cordillera (Southern Spain).
Lozano Rodríguez J. A. +4 more
core +1 more source

