Opendata, web and dolomites

MIGRATE SIGNED

MINERAL-SCALE HETEROGENEITY OF GRANITES: A NEW APPROACH INTEGRATING MICROCHEMICAL ANALYSIS AND THERMO-MECHANICAL MODELLING TO DISCLOSE THE THERMOCHEMICAL EVOLUTION OF THE CONTINENTAL CRUST

Total Cost €

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EC-Contrib. €

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Partnership

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 MIGRATE project word cloud

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

travale    productive    compositional    hafnium    crust    edge    constitutes    dated    revealed    heat    thermochemical    granitic    physico    incompatible    temperature    geochemical    zircons    numerical    expertise    producing    fluid    trace    performed    earth    continental    planet    characterised    isotopic    italy    emplacement    crustal    petrogenetic    technological    constrained    analytical    innovative    suitable    retrieve    period    life    below    valuable    techniques    enriched    stable    magmatism    water    secondment    evolution    precision    combines    data    reservoirs    replenishment    produces    resolved    energy    reservoir    chemical    geochronological    renewable    possibly    heterogeneity    granites    cutting    geothermal    zircon    temporally    perspective    mechanical    migration    relatively    larderello    temporal    mineral    dynamics    layer    radiogenic    thin    simulations    tempo    model    crystals    background    thermal    generate    permeability    buried    age    magma    thermo    corresponding    analysed    pb    bodies    time    physical    isotopes    outer    textural    rocks    combination    oxygen    shallow    volcanic    anomalies    conceptual    history    upper    thermally    decode    melts    complementing    magmatic   

Project "MIGRATE" data sheet

The following table provides information about the project.

Coordinator
UNIVERSITE DE GENEVE 

Organization address
address: RUE DU GENERAL DUFOUR 24
city: GENEVE
postcode: 1211
website: www.unige.ch

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 Switzerland [CH]
 Total cost 187˙419 €
 EC max contribution 187˙419 € (100%)
 Programme 1. H2020-EU.1.3.2. (Nurturing excellence by means of cross-border and cross-sector mobility)
 Code Call H2020-MSCA-IF-2015
 Funding Scheme MSCA-IF-EF-ST
 Starting year 2016
 Duration (year-month-day) from 2016-05-01   to  2018-04-30

 Partnership

Take a look of project's partnership.

# participants  country  role  EC contrib. [€] 
1    UNIVERSITE DE GENEVE CH (GENEVE) coordinator 187˙419.00

Map

 Project objective

Migration of granitic melts through the Earth’ crust enriched the upper continental crust in incompatible and heat-producing elements, making the thin outer layer of our planet suitable for life. The emplacement of granitic bodies produces thermal anomalies that, under specific conditions of water availability and permeability, may generate valuable geothermal reservoirs providing relatively low cost renewable energy. Recent technological advances have revealed that granites and their corresponding volcanic rocks are commonly characterised by compositional and temporal heterogeneity at the mineral-scale. In this project, textural information, mineral-scale geochemical-geochronological data and thermo-mechanical numerical modelling are integrated to decode the thermochemical evolution of granites buried below the productive Larderello-Travale geothermal field (Italy). Zircon crystals will be dated by U-Pb high-precision techniques and analysed for stable (oxygen) and radiogenic (hafnium) isotopes as well as for trace elements. These multi-analytical approach will allow defining the tempo of the chemical and isotopic evolution of the system. The age distribution of zircons will be used in combination with thermal modelling to retrieve the temperature-time history of the magmatic reservoir. Further numerical simulations will investigate the fluid-dynamics of magma replenishment and will be performed during a four month secondment period. Overall, the project combines cutting-edge techniques with an innovative conceptual approach to produce a temporally-resolved, thermally-constrained petrogenetic model for the Larderello-Travale granites and to define the physico-chemical evolution of a shallow-level magmatic reservoir. This information constitutes an essential background knowledge for the understanding and possibly exploitation of geothermal fields, complementing my current geochemical expertise with a physical perspective on crustal magmatism.

 Publications

year authors and title journal last update
List of publications.
2017 Farina F., Stevens G., Dini A., Schaltegger, U
Small-scale zircon age variability in the Monte Capanne pluton revealing the timescale of crustal melting and melt extraction.
published pages: , ISSN: , DOI:
Goldschmidt2017 Abstract 2019-06-13
2018 Farina, F., Montagna, C.P
Magma reservoir formation and evolution: insights from physical modelling.
published pages: , ISSN: , DOI:
Geophysical Research Abstracts Vol. 20, EGU2018-19712, 2018. 2019-06-13
2018 Federico Farina, Andrea Dini, Joshua H.F.L. Davies, Maria Ovtcharova, Nicolas D. Greber, Anne-Sophie Bouvier, Lukas Baumgartner, Alexey Ulianov, Urs Schaltegger
Zircon petrochronology reveals the timescale and mechanism of anatectic magma formation
published pages: 213-223, ISSN: 0012-821X, DOI: 10.1016/j.epsl.2018.05.021
Earth and Planetary Science Letters 495 2019-06-13
2018 Farina F., Dini, A., Ovtcharova, M., Davies, J.H.F.L., Greber, N.D., Bouvier, A-S., Baumgartner, L., Schaltegger, U
Zircon petrochronology reveals the mechanism of crustal anatectic magma formation
published pages: , ISSN: , DOI:
Geophysical Research Abstracts Vol. 20, EGU2018-6812, 2018 2019-06-13
2017 Farina, F.; Dini, A.; Ovtcharova, M.; Davies, J.; Bouvier, A. S.; Baumgartner, L. P.; Caricchi, L.; Schaltegger, U.
From Crustal Anatexis to Pluton Emplacement: High-Precision Zircon Geochronology Reveals the Thermal History of the Larderello-Travale Geothermal System (Italy)
published pages: , ISSN: , DOI:
American Geophysical Union, Fall Meeting 2017 2019-06-13

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