Ti substitution mechanisms in hibonite and the determination of Ti3+/Ti4+ by X-ray absorption spectroscopy for use as an oxybarometer with application to early Solar System processes
Quantitative determination of element species is crucial for understanding geological processes, particularly changing redox conditions. As Ti3+ is stable under very reducing conditions, Ti3+/Ti4+ oxybarometers are suitable for investigating early Solar System processes. The systematics of Ti3+/Ti4+...
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Imperial College London
2012
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.544271 |