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SLIP SIGNED

exhumed foSsiL shear zones: a key to Investigate Present middle-crustal seismicity

Total Cost €

0

EC-Contrib. €

0

Partnership

0

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 SLIP project word cloud

Explore the words cloud of the SLIP project. It provides you a very rough idea of what is the project "SLIP" about.

scanning    fabrics    microstructures    fossil    northern    interpreting    optical    thermodynamic    unravel    fluids    spectroscopy    rheology    action    aseismically    patterns    hypothesis    interaction    seismotectonic    mass    portions    analyser    model    levels    orogen    seismically    microscope    na    dating    rheological    precursors    odds    pressure    exhumed    micro    creep    slip    temperature    multidisciplinary    raman    brittle    localization    seismic    designed    derive    earthquakes    active    seismicity    viscous    spectrometry    frictional    latter    reconstruct    rock    electron    external    laser    steering    italy    inner    conceptual    relies    time    shed    metamorphic    deformation    probe    models    central    mechanisms    localize    faults    constraints    predicting    evolution    ablation    tectonic    histories    apennines    zones    shallow    assist    behave    shear    classic    age    light    explanation    provenance    reactions    crust    cycles    depths    upper    ductile    transient    remarkably    mid    behaviours    fluid    crustal   

Project "SLIP" data sheet

The following table provides information about the project.

Coordinator
ALMA MATER STUDIORUM - UNIVERSITA DI BOLOGNA 

Organization address
address: VIA ZAMBONI 33
city: BOLOGNA
postcode: 40126
website: www.unibo.it

contact info
title: n.a.
name: n.a.
surname: n.a.
function: n.a.
email: n.a.
telephone: n.a.
fax: n.a.

 Coordinator Country Italy [IT]
 Total cost 183˙473 €
 EC max contribution 183˙473 € (100%)
 Programme 1. H2020-EU.1.3.2. (Nurturing excellence by means of cross-border and cross-sector mobility)
 Code Call H2020-MSCA-IF-2018
 Funding Scheme MSCA-IF-EF-ST
 Starting year 2019
 Duration (year-month-day) from 2019-06-03   to  2021-06-02

 Partnership

Take a look of project's partnership.

# participants  country  role  EC contrib. [€] 
1    ALMA MATER STUDIORUM - UNIVERSITA DI BOLOGNA IT (BOLOGNA) coordinator 183˙473.00

Map

 Project objective

Deformation zones may localize seismicity not only at upper crustal levels along brittle faults, but also at greater depth along ductile shear zones. The latter is at odds to classic rheological models predicting shear zones to creep and behave aseismically. Cycles of frictional and viscous deformation and brittle precursors to ductile deformation have been proposed as possible explanation. The “SLIP” action will contribute to better constrain seismic localization at mid-crustal depths along ductile shear zones by studying key areas of the Northern Apennines of Italy (NA). SLIP relies on the hypothesis that exhumed brittle-ductile shear zones of the inner NA represent the fossil analogue of the still seismically active deformation zones in the central and external portions of the orogen. SLIP will investigate microstructures in a multidisciplinary action to derive constraints upon the seismic deformation mechanisms steering the orogen seismic activity. The objectives of this proposal are to: 1) Unravel the pressure-temperature-time-deformation histories of exhumed fossil shear zones; 2) Define the role of fluids in triggering metamorphic reactions, enhancing deformation and steering the transient rheology of the shear zones; 3) Determine the provenance of the metamorphic fluids; 4) Reconstruct the tectonic evolution and the conceptual seismotectonic model of the NA. To achieve the above defined specific objectives, a multidisciplinary approach has been designed including fieldwork, optical and scanning electron microscope analyses, Raman spectroscopy, electron probe micro-analyser, laser ablation mass spectrometry, thermodynamic modelling, and age dating of deformation fabrics. SLIP will contribute to our understanding of shallow to mid-crustal earthquakes and its results will remarkably assist in better interpreting current seismic patterns and crustal behaviours. It will also shed new light on the fluid pathways and fluid-rock interaction processes in the crust.

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