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.

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

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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