ExpresSedGrowth and demise of Late Carboniferous carbonate platforms in the eastern Cantabrian Zone, Asturias, northwestern Spain
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Cited by (51)
Facies analysis of a Bartonian–Aquitanian siliciclastic‑carbonate system, Costa Rica
2021, Sedimentary GeologyCitation Excerpt :That kind of deposit is apparently rare in the Eocene record. However, cm–dm-scale breccias and calciturbidites are common in the geological record and are generally linked to exportation of platform margin (i.e., inner, middle, outer) or slope deposits (Bahamonde et al., 1997, 2000; Bábek et al., 2007; Reijmer et al., 2012; Chesnel et al., 2016). Additionally, the intercalation of marls typically evidences a deep outer ramp to basin setting (Ielpi and Cornamusini, 2013).
Spatial and temporal distribution of microbial carbonates, skeletal and non-skeletal grains in a Pennsylvanian carbonate platform (Valdorria, Northern Spain)
2017, Palaeogeography, Palaeoclimatology, PalaeoecologyCitation Excerpt :The Cantabrian Zone is the foreland fold-and-thrust belt of the arc-shaped Variscan orogen in the North of Spain (Fig. 1A; Pérez-Estaún et al., 1988; Gutiérrez-Alonso et al., 2004). Prior to the tectonic deformation and during most of the Carboniferous, the zone formed part of a marine foreland basin several hundreds of kilometres wide in which microbial-dominated high-rising carbonate platforms developed (Eichmüller, 1985; Bahamonde et al., 1997a, 1997b, 2000, 2007, 2015; Della Porta et al., 2002a, 2002b, 2003, 2004, 2005; Kenter et al., 2002, 2005; Merino-Tomé et al., 2014; Chesnel et al.., 2016a). The Valdorria carbonate platform forms part of the Valdeteja Formation (Wagner et al., 1971; see also Eichmüller, 1985) and developed during most of the Bashkirian in the southern branch of the Cantabrian Zone, in the Bodón-Ponga Unit (Fig. 1A; Alonso et al., 2009).
Component-specific petrographic and geochemical characterization of fine-grained carbonates along Carboniferous and Jurassic platform-to-basin transects
2014, Sedimentary GeologyCitation Excerpt :Two settings, representing end-members in several aspects, were examined for this project. One is an extensively studied, steep-flanked Carboniferous (Moscovian) platform in Asturias, Northern Spain (Bahamonde et al., 1997, 2004; Della Porta et al., 2004; Immenhauser et al., 2002, 2008; Kenter et al., 2003, 2005; van der Kooij et al., 2007, 2009). The well-constrained data set available is used to place our findings in a larger sedimentological and palaeoceanographic context.