Opendata, web and dolomites

RIFT-O-MAT SIGNED

Magma-Assisted Tectonics: two-phase dynamics of oceanic and continental rifts

Total Cost €

0

EC-Contrib. €

0

Partnership

0

Views

0

 RIFT-O-MAT project word cloud

Explore the words cloud of the RIFT-O-MAT project. It provides you a very rough idea of what is the project "RIFT-O-MAT" about.

seismic    frictional    consistent    governed    understand    crust    mid    source    rock    modelled    functioning    tectonics    interact    innately    transform    fuca    dikes    continua    outreach    continental    divergent    variation    continents    lithosphere    interpenetrating    basic    integral    mass    consistently    constraints    lacking    boundaries    bathymetric    plate    dynamics    mechanical    observation    supply    inherent    tomography    force    stress    momentum    there    conservation    deformation    fundamental    suggests    ridges    tectonic    sufficiently    rifts    unresolved    ridge    incorporate    east    thorough    mathematics    crustal    models    recorded    viscoelastic    strength    phenomena    modest    magmatic    magmatism    chemical    rift    lithospheric    context    decades    flow    faulting    breaks    magma    recognition    plastic    weaken    assisted    surface    careful    intrusion    plates    validated    liquid    almost    theory    solid    hence    juan    african    africa    thermal    code    distinguished    rheology    ocean    tensile    lavas    excluded    single    relief    central    emplacement    energy    rifting    ground    diverse    de    faults    geochemistry    indicates   

Project "RIFT-O-MAT" data sheet

The following table provides information about the project.

Coordinator
THE CHANCELLOR, MASTERS AND SCHOLARS OF THE UNIVERSITY OF OXFORD 

Organization address
address: WELLINGTON SQUARE UNIVERSITY OFFICES
city: OXFORD
postcode: OX1 2JD
website: www.ox.ac.uk

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 United Kingdom [UK]
 Total cost 2˙000˙000 €
 EC max contribution 2˙000˙000 € (100%)
 Programme 1. H2020-EU.1.1. (EXCELLENT SCIENCE - European Research Council (ERC))
 Code Call ERC-2017-COG
 Funding Scheme ERC-COG
 Starting year 2019
 Duration (year-month-day) from 2019-03-01   to  2024-02-29

 Partnership

Take a look of project's partnership.

# participants  country  role  EC contrib. [€] 
1    THE CHANCELLOR, MASTERS AND SCHOLARS OF THE UNIVERSITY OF OXFORD UK (OXFORD) coordinator 2˙000˙000.00

Map

 Project objective

There is widespread recognition of the central role of magma at divergent plate boundaries. However in almost all models, magmatism is treated as a by-product and is excluded from the dynamics. A thorough understanding of continental rifts and mid-ocean ridges, which are fundamental to plate tectonics, requires consistent models of magma intrusion into the lithosphere and crust. This is a proposal to develop models in which magmatism is an integral thermal, chemical, and mechanical component, and hence to better understand the basic functioning of plate tectonics.

Diverse insight and constraints on divergent boundaries come from decades of careful observation. But lacking adequate models of magmatism, old and new issues remain unresolved. For continents, a comparison of available tectonic force to inherent lithospheric strength indicates that magmatic intrusion is required to weaken plates sufficiently for rifting. For mid-ocean ridges, bathymetric analysis suggests that modest variation in the magma supply may be recorded by crustal emplacement and faulting. These phenomena cannot be understood and modelled in the context of single-phase flow. The proposed work breaks new ground in applying a theory that is innately two-phase; one where interpenetrating liquid and solid continua are governed by conservation of mass, momentum, and energy.

This theory will incorporate a viscoelastic-plastic/frictional rheology, modelling rock failure under tensile effective stress. Hence it will allow for dikes that interact consistently with faults. The open-source code will be validated by comparison with measurements of surface deformation/relief, products of seismic tomography, and geochemistry of lavas. In collaboration with distinguished project partners, models will be tailored to investigate the East African Rift System and Juan de Fuca ridge. Outreach will support mathematics in Africa. The proposed research will transform our understanding of magma-assisted tectonics.

Are you the coordinator (or a participant) of this project? Plaese send me more information about the "RIFT-O-MAT" project.

For instance: the website url (it has not provided by EU-opendata yet), the logo, a more detailed description of the project (in plain text as a rtf file or a word file), some pictures (as picture files, not embedded into any word file), twitter account, linkedin page, etc.

Send me an  email (fabio@fabiodisconzi.com) and I put them in your project's page as son as possible.

Thanks. And then put a link of this page into your project's website.

The information about "RIFT-O-MAT" are provided by the European Opendata Portal: CORDIS opendata.

More projects from the same programme (H2020-EU.1.1.)

CHIPTRANSFORM (2018)

On-chip optical communication with transformation optics

Read More  

QUAMAP (2019)

Quasiconformal Methods in Analysis and Applications

Read More  

OAlipotherapy (2018)

Long-retention liposomic drug-delivery for intra-articular osteoarthritis therapy

Read More