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• W2155259712 abstract "The Calatayud Basin is an elongated NW-SE depression in northeastern Spain. It is filled with continental Miocene sediments resulting from erosion of Palaeozoic and Mesozoic rocks of the Castilian and Aragonese branches of the Iberian Range. Miocene series consist of lutitic, marly, carbonate and evaporitic levels characteristic of a short-lived salt lake or a low-salinity plays-lake depositional environment. The carbonates detected in the series were calcite, dolomite and magnesite. The calcites generally :;how micritic textures, anhedral to subhedral morphologies and contain from 0 to 1 mole% MgCO 3, and so can be considered low-Mg Their mean isotopic values are ~lSo = -7.8%0 (PDB) and 813C = --7.7%0 indicating precipitation in isotopic equilibrium with meteoric water and an extensive contribution of CO 2 of organic origin to the total dissolved C, respectively. The calcites present Mg/Ca, Sr/Ca and Na/Ca molar ratios that suggest precipitation from Na-enriched meteoric water. Dolomites are non-stoichiometric (44.5-47.7 mole% MgCO3), disordered, micfitic and anhedral to subhedral; their mean isotopic values [SlsO = + 0.4%0 (PDB) and 813C = --3.8%0] indicate that they precipitated from more evolved water and with a higher contribution of atmospheric CO 2 to the total dissolved C, respectively, than those of the calcites. Moreover, they present Mg/Ca, Sr/Ca and Na/Ca molar ratios suggesting precipitation from water with similar composition to seawater. The isotopic composition of magnesite [81So = +4.6%0 (PDB) and 513C = -4.0%~], together with the higher concentration in Sr and Na, indicates that this phase probably precipitated from more evolved water. The isotopic values and trace-element contents of carbonates appear to confirm the mineralogical trend from calcite to dolomite and to magnesite corresponding to the progressive increase of evaporitic concentration as the water, in a hydrologically closed system, was subjected to more acutely arid conditions." @default.
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• W2155259712 date "1996-08-01" @default.
• W2155259712 modified "2023-10-01" @default.
• W2155259712 title "Mineralogy and geochemistry of the carbonates in the Calatayud Basin (Zaragoza, Spain)" @default.
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• W2155259712 doi "https://doi.org/10.1016/0009-2541(95)00185-9" @default.
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