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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.

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

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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The information about "SLIP" are provided by the European Opendata Portal: CORDIS opendata.

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