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UK funding (782 110 £) : Imagerie passive de la frontière lithosphère asthénologie (PiLAB) Ukri01/02/2016 UK Research and Innovation, Royaume Uni
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Imagerie passive de la frontière lithosphère asthénologie (PiLAB)
| Abstract | Plate tectonics has been a fundamental tenet of Earth Science for nearly 50 years, but fundamental questions remain, such as where is the base of the plate and what makes a plate, "plate-like?" A better understanding of the transition from the rigid lithospheric plate to the weaker mantle beneath has important implications for the driving forces of plate tectonics, natural hazards, and climate change. There are many proxies used to estimate the depth and nature of the base of tectonic plates, but to date no consensus has been reached. For example, temperature is known to have a strong effect on the mechanical behaviour of rocks, and if this were the sole process governing the definition of the plate, then we would expect to see a thin plate near a mid ocean ridge and a very thick plate beneath old seafloor. However numerous geophysical studies observe what are interpreted as nearly constant thickness plate at all seafloor ages. This has led scientists to propose other mechanisms, such as dehydration of the mantle to strengthen the mantle to form a rigid plate. Similarly, observations of very strong anomalies have led others to suggest that melt might exist to weaken the mantle beneath the plates. However many of these observations come from only one ocean, the Pacific, from indirect, remote observations, at different areas and scales, and with different sensitivities to earth properties. Although results have been promising, comparisons among studies are challenging, hindering a complete understanding of the tectonic plate. We will systematically image the entire length of an oceanic plate, from its birth at the Mid Atlantic Ridge to its oldest formation on the African margin. This is a large-scale focused effort with multiple scales of resolution and sensitivity, from a metre to kilometre scale using seismic and electromagnetic methods. This scale, focus, and interdisciplinary approach will finally determine the processes and properties that make a plate strong and define it. The project will be accomplished through a large, focused international collaboration that involves EU partners (3.5 M euro) and industry (6.4M euro), both already funded. |
| Category | Research Grant |
| Reference | NE/M003507/1 |
| Status | Closed |
| Funded period start | 01/02/2016 |
| Funded period end | 10/10/2019 |
| Funded value | £782 110,00 |
| Source | https://gtr.ukri.org/projects?ref=NE%2FM003507%2F1 |
Participating Organisations
| University of Southampton | |
| University of Paris | |
| University of California, San Diego (UCSD) | |
| Helmholtz Association of German Research Centres | |
| GEOMAR Helmholtz Ctr for Ocean Res Kiel | |
| Institute of Earth Physics IPGP | |
| University of California, San Diego |
Cette annonce se réfère à une date antérieure et ne reflète pas nécessairement l’état actuel. L’état actuel est présenté à la page suivante : University of Southampton, Southampton, Royaume Uni.
