Stratigraphic context and timing of sand supply to deep-marine Ainsa-Jaca basin, middle Eocene, Spanish Pyrenees : constraints from geochemistry and sedimentology
The sediment flux to a basin is controlled by a complex combination of tectonics, climatic variability and stochastic events, thereby creating a cryptic geological record. Deconvolving the effects of individual factors controlling sedimentation can often be challenging, due to a variety of reasons i...
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University College London (University of London)
2012
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.565601 |