File:El Pedregal Formation.jpg
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Summary
| Description |
English: (A) Onlap stratal terminations of the El Pedregal Formation against the flank of a volcanic mound in the Camarena de la Sierra.3 outcrop (volcanic level V11). (B,C) The same in the Abejuela outcrop (volcanic level V13). (D) 3D geological mapping across the northern flank of the volcanic mound in the Caudiel outcrop (volcanic level V12). The El Pedregal, Moscardón, and Domeño formations progressively onlap the volcanic slope. Abbreviations: SCh: Sot de Chera Formation (yellow marls), Yat: Yátova Formation (wackestone–packstones with sponges), Arr: Arroyofrío Bed (wackestone–packstones with ferruginous ooids and pisoids), Dom: Domeño Formation (bioclastic–filaments–wackestone–packstones), Mos: Moscardón Formation (crinoidal packstones to grainstones), Ped: El Pedregal Formation (bioclastic wackestone–packstone with chert nodules), Cas: Casinos Formation (mudstones, bioclastic wackestones, locally packstones, and thin marly beds), Tur: Turmiel Formation (alternation of marls and mudstones to packstones), Bar: Barahona Formation (bioclastic wackestones to packstones, sometime grainstones, with occasional marly beds), CLa: Cuevas Labradas Formation (marls, peritidal mudstones, bioclastic wackestones to packstones, grainstones, and carbonate breccias). PLIENS.: Pliensbachian, TOAR.: Toarcian, AAL.: Aalenian, BAJ.: Bajocian, BATH.: Bathonian, CAL.: Callovian, OXF.: Oxfordian, KIM.: Kimmeridgian. |
| Date | |
| Source | Cortés, José Emilio (2023-06-12). "Dating volcanic materials through biochronostratigraphic methods applied to hosting strata (example from the Iberian Chain, eastern Spain)". Comptes Rendus. Géoscience 355 (G1): 175–202. DOI:10.5802/crgeos.220. ISSN 1778-7025. |
| Author | José Emilio Cortés |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
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| current | 18:28, 14 October 2024 | | 1,382 × 1,819 (2.44 MB) | Olmagon | Uploaded a work by José Emilio Cortés from {{Cite journal |last=Cortés |first=José Emilio |date=2023-06-12 |title=Dating volcanic materials through biochronostratigraphic methods applied to hosting strata (example from the Iberian Chain, eastern Spain) |url=https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.220/ |journal=Comptes Rendus. Géoscience |language=en |volume=355 |issue=G1 |pages=175–202 |doi=10.5802/crgeos.220 |issn=1778-7025}} with UploadWizard |
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