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Facies architecture of the fluvial Missão Velha Formation (Late Jurassic-Early Cretaceous), Araripe Basin, Northeast Brazil : paleogeographic and tectonic implications

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Abstrakty
EN
Sedimentological analysis of the Missão Velha Formation (Araripe Basin, northeast Brazil) is the aim of this paper through detailed facies analysis, architectural elements, depositional systems and paleocurrent data. The main facies recognized were: (i) coarse-grained conglomeratic sandstones, locally pebbly conglomerates, with abundant silicified fossil trunks and several large-to-medium trough cross-stratifications and predominantly lenticular geometry; (ii) lenticular coarse-to-medium sandstones with some granules, abundant silicified fossil wood, and large-to-medium trough cross-stratifications, cut-and fill features and mud drapes on the foresets of cross-strata, (iii) poorly sorted medium-grained sandstones with sparse pebbles and with horizontal stratification, (iv) fine to very fine silty sandstones, laminated, interlayered with (v) decimetric muddy layers with horizontal lamination and climbing-ripple cross-lamination. Nine architectural elements were recognized: CH: Channels, GB: Gravel bars and bed forms, SB: Sand bars and bedforms, SB (p): sand bedform with planar cross-stratification, OF: Overbank flow, DA: Downstream-accretion macroforms, LS: Laminated sandsheet, LA: Lateral-accretion macroforms and FF: Floodplain fines. The lithofacies types and facies associations were interpreted as having been generated by alluvial systems characterized by (i) high energy perennial braided river systems and (ii) ephemeral river systems. Aeolian sand dunes and sand sheets generated by the reworking of braided alluvial deposits can also occur. The paleocurrent measurements show a main dispersion pattern to S, SE and SW, and another to NE/E. These features imply a paleodrainage flowing into the basins of the Recôncavo-Tucano-Jatobá.
Rocznik
Strony
515--545
Opis fizyczny
Bibliogr. 102 poz., rys., tab.
Twórcy
  • Department of Geology, Federal University of Pernambuco, 52-740-030, Recife, PE, Brazil
  • Department of Geology, Federal University of Pernambuco, 52-740-030, Recife, PE, Brazil
  • Research Fellow of Conselho Nacional de Desenvolvimento Científico e Tecnológico – CNPq, Brazil
  • Post-graduation Program, Federal University of Pernambuco, Brazil
  • Department of Geology, Federal University of Ceará, Brazil
  • Department of Geology, Federal University of Pernambuco, 52-740-030, Recife, PE, Brazil
  • Research Fellow of Conselho Nacional de Desenvolvimento Científico e Tecnológico – CNPq, Brazil
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Uwagi
PL
Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę (zadania 2017).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-2e84ab8f-15c5-4fa3-9a2b-daeed1ff83cf
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