Facies, microfacies, and diagenesis of late Callovian-early Oxfordian carbonates (La Manga Formation) in the West Central Argentinean high andes
At 32° 40′ south latitude the Andean orogen shows a typical thin-skinned fold and thrust belt that exposes the Mesozoic back-arc basin fill. The late Callovian - early Oxfordian limestones of the La Manga Formation were studied based on lithofacies, microfacies, and diagenetic processes in order to...
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2002
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| Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08912556_v17_n1_p1_LoForte http://hdl.handle.net/20.500.12110/paper_08912556_v17_n1_p1_LoForte |
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