Matches in SemOpenAlex for { <https://semopenalex.org/work/W1986593675> ?p ?o ?g. }
Showing items 1 to 62 of
62
with 100 items per page.
- W1986593675 endingPage "42" @default.
- W1986593675 startingPage "25" @default.
- W1986593675 abstract "Abstract Jurassic studies in the Internal Zones of the Betic Cordillera are scarce since this zone is composed mainly of pre-Jurassic metamorphic rocks. Only the “Dorsal” and the Malaguide domains include fossiliferous Jurassic successions, as in Sierra Espuna (SE Spain), which is one of the bigger and well-exposed Jurassic outcrops of the Internal Zones. Collected Ammonite assemblages update and improve the precision of previous biostratigraphic data by the recognition of: the Domerian (= Upper Pliensbachian, in the Mediterranean Domain) Lavinianum (Cornacaldense Subzone), Algovianum (Ragazzoni, Bertrandi, Accuratum and Levidorsatum Subzones) and Emaciatum (Solare and Elisa Subzones) Zones; the Lower Toarcian Polymorphum and Serpentinum Zones; the Middle Toarcian, Bifrons and Gradata Zone; the Upper Toarcian Reynesi Zone; the Lower/Upper Bajocian, the Lower Callovian Bullatus and Gracilis Zones; the Middle/Upper Oxfordian Transversarium, Bifurcatus, Bimammatum and Planula Zones; and the Lower and Upper Kimmeridgian Platynota, Strombecki, Divisum and Beckeri Zones. The paleoenvironmental evolution of the Malaguide Jurassic at Sierra Espuna shows similarities with other Mediterranean Tethyan paleomargins. The biostratigraphic precision along with the litho- and biofacies analyses has enabled the interpretation that the Malaguide paleomargin evolved as a passive margin, developing shallow carbonate platforms, until the Domerian (Lavinianum Zone). Then, the platform broke up (Domerian, Lavinianum Zone–Upper Toarcian, Reynesi Zone) with the beginning of the rifting stage, beginning the development of horst–graben systems and the coeval drowning of the area. This stage ended in the upper Lower Callovian (Gracilis Zone) to the Middle Oxfordian (Transversarium Zone) interval, starting the drifting stage, which accentuated the horst–graben systems, leading to the deposition of condensed nodular limestones in the raised sea bottom." @default.
- W1986593675 created "2016-06-24" @default.
- W1986593675 creator A5011356085 @default.
- W1986593675 creator A5042220643 @default.
- W1986593675 creator A5055399124 @default.
- W1986593675 creator A5063854084 @default.
- W1986593675 creator A5067202370 @default.
- W1986593675 date "2006-01-01" @default.
- W1986593675 modified "2023-09-26" @default.
- W1986593675 title "Jurassic biostratigraphy and paleoenvironmental evolution of the Malaguide complex from Sierra Espuña (Internal Betic Zone, SE Spain)" @default.
- W1986593675 cites W1501467746 @default.
- W1986593675 cites W2083839833 @default.
- W1986593675 cites W2114440458 @default.
- W1986593675 cites W4212875885 @default.
- W1986593675 doi "https://doi.org/10.1016/j.geobios.2004.09.002" @default.
- W1986593675 hasPublicationYear "2006" @default.
- W1986593675 type Work @default.
- W1986593675 sameAs 1986593675 @default.
- W1986593675 citedByCount "12" @default.
- W1986593675 countsByYear W19865936752012 @default.
- W1986593675 countsByYear W19865936752013 @default.
- W1986593675 countsByYear W19865936752016 @default.
- W1986593675 countsByYear W19865936752017 @default.
- W1986593675 countsByYear W19865936752019 @default.
- W1986593675 countsByYear W19865936752021 @default.
- W1986593675 crossrefType "journal-article" @default.
- W1986593675 hasAuthorship W1986593675A5011356085 @default.
- W1986593675 hasAuthorship W1986593675A5042220643 @default.
- W1986593675 hasAuthorship W1986593675A5055399124 @default.
- W1986593675 hasAuthorship W1986593675A5063854084 @default.
- W1986593675 hasAuthorship W1986593675A5067202370 @default.
- W1986593675 hasConcept C127313418 @default.
- W1986593675 hasConcept C151730666 @default.
- W1986593675 hasConcept C40616122 @default.
- W1986593675 hasConcept C61721801 @default.
- W1986593675 hasConcept C6494504 @default.
- W1986593675 hasConceptScore W1986593675C127313418 @default.
- W1986593675 hasConceptScore W1986593675C151730666 @default.
- W1986593675 hasConceptScore W1986593675C40616122 @default.
- W1986593675 hasConceptScore W1986593675C61721801 @default.
- W1986593675 hasConceptScore W1986593675C6494504 @default.
- W1986593675 hasIssue "1" @default.
- W1986593675 hasLocation W19865936751 @default.
- W1986593675 hasOpenAccess W1986593675 @default.
- W1986593675 hasPrimaryLocation W19865936751 @default.
- W1986593675 hasRelatedWork W1758396658 @default.
- W1986593675 hasRelatedWork W2093776561 @default.
- W1986593675 hasRelatedWork W2350284515 @default.
- W1986593675 hasRelatedWork W2357676215 @default.
- W1986593675 hasRelatedWork W2789304626 @default.
- W1986593675 hasRelatedWork W2895595942 @default.
- W1986593675 hasRelatedWork W3144680029 @default.
- W1986593675 hasRelatedWork W1968527135 @default.
- W1986593675 hasRelatedWork W2740801233 @default.
- W1986593675 hasRelatedWork W3110989845 @default.
- W1986593675 hasVolume "39" @default.
- W1986593675 isParatext "false" @default.
- W1986593675 isRetracted "false" @default.
- W1986593675 magId "1986593675" @default.
- W1986593675 workType "article" @default.