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.

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

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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