Implicaciones paleoambientales deducidas del estudio geoquímico del transito mioceno-plioceno en la Cuenca de Sorbas (Almería)
DOI:
https://doi.org/10.3989/egeol.95513-4291Keywords:
Geochemistry, multivariant analysis, clay mineralogy, parent rocks, paleoenvironmental conditions, Miocene-Pliocene, Sorbas Basin, Betic CordillerasAbstract
The geochemistry of the < 2 µm fractions of the Mio-Pliocene sediments and the bulk sample of the surrounding metamorphic rocks was studied in arder to characterize the geochemical environment during the sedimentation and to trace the influence of the surrounding rocks on the sediments. After making the relationships among the chemical elements and the minerals or the rocks by Principal Component Analysis (PCA), it has been carried out a Hierarchical Ascending Classification (HAC) which regroups the samples with similar geochemical characteristics into 8 classes. Graphical comparison of mean geochemical composition among HAC groups provides a better identification of inherited similarities between sorne sediments and the metapellitic rocks in the eastern Betic Cordilleras. Gneises, carbonated and metabasic rocks influence is inexistent or very located. Finally B and MgO contents have allowed us to distinguish different types of deposit environments with a higher or lower degree of confinement and with influence of sea-ar continental waters.
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