Fabric variability within layered Fe-oxide deposits in Mid-late Miocene sedimentary formations, NW Borneo: impact on facies architectural interpretations
Iron (Fe) can accumulate in various forms in sedimentary environments that experience alternating moisture conditions, hydration and dehydration processes and redox processes. It has been pointed out that there is a major gap in the understanding of the composition of mixed solid-phase minerals, the...
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| Format: | Conference Paper |
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Geological Society of Malaysia
2008
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| Online Access: | http://hdl.handle.net/20.500.11937/32576 |