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In-situ observation of the crystallization kinetics and texture evolution of basalts

Subject Area Mineralogy, Petrology and Geochemistry
Term from 2009 to 2018
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 129863361
 
Final Report Year 2017

Final Report Abstract

The crystallization kinetics of different basaltic melts (K-rich basalt, MORB, alkali basalt) was studied by in-situ observation in a moissanite cell at 1 bar. Main observations made in all systems are: (1) Nucleation of new phases (e.g. olivine, clinopyroxene) always occurs only in short events; (2) growth rates of crystals are size-dependent (proportionate growth); (3) Ostwald ripening removes small crystal fractions. Overall, these observations show that the interpretation of igneous textures by conventional CSD (crystal size distribution) theory is severely flawed and needs revision. In the course of this study, it was observed that the moissanite cell is very well suited for observing processes of bubble nucleation and growth in silicate melts. Therefore, these processes were studied in a range of rhyolitic to basaltic systems, first at 1 bar with the conventional moissanite cell; later, a new “hydrothermal” moissanite cell was developed, which allows precise control of pressure and temperature. With this new cell, a number of novel experiments were carried out that allowed the direct observation of the behavior of bubbles both during periodic (sinusoidal) pressure fluctuations and during decompression. The experiments suggest that bubble nucleation in silicate melts requires less supersaturation than previously thought. The importance of Ostwald ripening for the evolution of bubble size distributions was directly demonstrated.

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