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Open AccessArticle

Pyrometamorphic Rocks in the Molinicos Basin (Betic Cordillera, SE Spain): Insights into the Generation of Cordierite Paralavas

1
Departamento de Geología and CEACTierra, Universidad de Jaén, Campus Las Lagunillas s/n, 23071 Jaén, Spain
2
Departamento de Geología and CEACTierra, Campus Científico Tecnológico de Linares, Universidad de Jaén, 23700 Linares, Jaén, Spain
*
Author to whom correspondence should be addressed.
Minerals 2019, 9(12), 748; https://doi.org/10.3390/min9120748
Received: 27 September 2019 / Revised: 15 November 2019 / Accepted: 26 November 2019 / Published: 30 November 2019
(This article belongs to the Special Issue Mineral Formation in Pyrometamorphic Process)
A singular thermal anomaly occurred in the Molinicos Miocene, lacustrine, intramontane basin (Betic Cordillera). This gave place to vitreous vesicular materials (paralavas) and baked rocks (clinker) inside of a sequence of marly diatomites and limestones. The chemical composition of the paralavas (SiO2 = 52–57, Al2O3 ≈ 20, Fe2O3 = 10–20, K2O + Na2O < 2.5, CaO < 4.5, and MgO < 1.5, % in weight), which is very different from typical igneous rocks, and their high-T mineralogy (cordierite, sillimanite, anorthite, mullite, and high-T silica polymorphs) suggest that they formed during a pyrometamorphic event. The occurrence of dry intervals in the lacustrine depositional system, the high Total Organic Carbon contents (>4% in weight) of dark clay layers and the existence of tectonic fractures give the right context for a combustion process. Short-term heating favoured the generation of paralavas, clinker and marbles. Thermodynamic modelling constrains the onset of melting at 870–920 °C for <10 MPa at equilibrium conditions. However, the presence of tridymite and/or cristobalite in clinker and paralavas and the compositional variation in both rock types suggests that the temperature at which first melting occurred ranged between 870 °C and 1260 °C due to melt fractionation processes. View Full-Text
Keywords: cordierite; clinker; combustion metamorphism; Molinicos Basin; paralava; melt fractionation; P-T pseudosection; SEM cordierite; clinker; combustion metamorphism; Molinicos Basin; paralava; melt fractionation; P-T pseudosection; SEM
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MDPI and ACS Style

Abad, I.; Sánchez-Gómez, M.; Reolid, M.; López Sánchez-Vizcaíno, V. Pyrometamorphic Rocks in the Molinicos Basin (Betic Cordillera, SE Spain): Insights into the Generation of Cordierite Paralavas. Minerals 2019, 9, 748.

AMA Style

Abad I, Sánchez-Gómez M, Reolid M, López Sánchez-Vizcaíno V. Pyrometamorphic Rocks in the Molinicos Basin (Betic Cordillera, SE Spain): Insights into the Generation of Cordierite Paralavas. Minerals. 2019; 9(12):748.

Chicago/Turabian Style

Abad, Isabel; Sánchez-Gómez, Mario; Reolid, Matías; López Sánchez-Vizcaíno, Vicente. 2019. "Pyrometamorphic Rocks in the Molinicos Basin (Betic Cordillera, SE Spain): Insights into the Generation of Cordierite Paralavas" Minerals 9, no. 12: 748.

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