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Hyperpycnal littoral deltas:A case of study from the Lower Cretaceous Agrio Formation in the neuquén basin,Argentina

引用

Journal of Palaeogeography 2021年第4期10卷 550-570页

作者： Ainara Irastorza Carlos Zavala Debora Mical Campetella Martín Turienzo Daniela Olivera Florencia Peralta Maite Irastorza Paula Martz Dpto.de Geología Universidad Nacional Del Sur(UNS)Bahía Blanca 8000Argentina Instituto Geologico Del Sur(InGEOSUR) Universidad Nacional Del Sur(UNS)-CONICETBahía Blanca 8000Argentina GCS Argentina SRL Molina Campos 150Bahía Blanca 8000Argentina Universidad nacional Del Sur Bahía Blanca 8000Argentina Universidad nacional de Río negro.Instituto de Investigacion de Paleobiología y Geología General Roca 8332Río NegroArgentina Consejo nacional de Investigaciones Científicas y Tecnicas(COnICET) Instituto de Investigaciones en Paleobiología y GeologíaGeneral Roca 8332Río NegroArgentina

Recent advances in the understanding of deltaic deposits provide new tools for the study and analysis of deltaic deposits in shallow epicontinental *** the introduction of sequence stratigraphic concepts,meter-scale coarsening and thickening upward successions have been considered as“parasequences”originated by high-frequency sea-level ***,recent studies enhanced the importance of wave-aided low-dense hyperpycnal flows in transporting fine-grained sediments in shallow shelfal *** poorly-known(and at the same time very common)types of delta,known as hyperpycnal littoral deltas(HLD),develop very low gradient progradational units,controlled by changes in the sediment supply instead of sea level *** small-scale progradational units are very common in shallow epicontinental seas like the Lower Cretaceous Agrio Formation in the neuquén *** study provides a first detailed analysis of hyperpycnal littoral deltas from the Agua de la Mula Member(upper Hauterivian-lower Barremian)of the Agrio *** unit has been studied in three locations near Bajada del Agrio locality in the central part of the neuquén basin,*** sandy facies,three heterolithic facies,three muddy facies and four calcareous facies were *** facies analysis,three facies associations could be determined,corresponding to offshore/prodelta,distal ramp delta and proximal ramp *** three stratigraphic sections discussed in this study are internally composed of several small-scale sequences showing a coarsening and thickening upward pattern,transitionally going from muddy to sandy wave-dominated facies,and ending with calcareous bioclastics levels on *** small-scale sequences are interpreted as delta front deposits of wave-influenced hyperpycnal littoral deltas,punctuated by calcareous intervals accumulated during periods of low sediment *** is interpreted that the development of hyperpycnal littoral deltas could have been

关键词： Deltas Hyperpycnal littoral deltas Prograding sequences Agua de la Mula Member neuquén basin

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