TIMPANI · Timescales of Igneous and Metamorphic Processes - Accessing new Information
6РП — Действия „Мария Кюри“
- Период
- 2006-02-01 → 2007-01-31
- Финансиране от ЕС
- 158 786 €
- Участници
- 1
- Схема
- EIF
Линиите свързват координатора с партньорите.
Накратко на български
Компютърен модел анализира химичния състав на минерални зърна във вулканични скали и метеорити. Това помага да се определят времевите рамки на процеси преди вулканични изригвания или при формирането на небесни тела.
Кратко обяснение, генерирано от езиков модел по текста на CORDIS. Оригиналът е по-долу.
Резултати накратко
Final Activity Report Summary - TIMPANI (Timescales of Igneous and Metamorphic Processes - Accessing new Information)
Project TIMPANI has been concerned with the development of a computer model for analysing compositional profiles within mineral grains. The model allows the timescales of high-temperature processes to be constrained within a variety of geological materials, including volcanic, metamorphic and meteorite samples. This has great use for examining the timescales of processes occurring before volcanic eruptions; rates of processes in metamorphic settings or the timescales of assembly and destruction of meteorite parent bodies.
Текст от CORDIS, на английски · Данни: CORDIS, © Европейски съюз
Цел на проекта
To investigate the timescales of plutonism, metamorphism and textural ripening through the integration of crystal size distributions (CSD), micro-beam analysis (micro XRF, microprobe, SEM), intra- and extra-crystalline diffusion based upon that data, geothermobarometry, and general petrology/ textural development as well as computer modelling of re-crystallisation regimes in contact metamorphic settings. The project will look at samples from the aureole of the Mt. Capanne pluton, Elba, which encompasses a wide variety of metamorphic protoliths (pelites, carbonates, flysch and igneous rocks), allowing the effects of the same temperature-time path on different lithology to be investigated and quantified. Spatially well-constrained samples will be taken from any lithology during fieldwork and the patterns of metamorphic and textural development of each suite will be related to a modelled temperature field constrained by geothermometric data. It is hoped that a toolbox of techniques based upon intra-crystall ine diffusion will be developed for accessing temperature-time information during the course of this work, based upon simpler techniques the applicant has devised for igneous settings. Progress permitting; the techniques developed during this investigatio n may be then extended to the more complicated case of regional metamorphic settings.
Оригинален текст от CORDIS (на английски).
Участници
- UNIVERSITE JOSEPH FOURIER - GRENOBLE 1 · GRENOBLEКоординаторФранция
Връзки
Данни: CORDIS, © Европейски съюз