Middle-Upper Triassic successions in the eastern Iberian Chain (Alt Palància and Manzanera areas)Stratigraphic precisions

  1. F. Ortí 1
  2. J. Guimerà 1
  3. C. Benedicto 2
  4. A. Pérez-López 3
  1. 1 Universitat de Barcelona
    info

    Universitat de Barcelona

    Barcelona, España

    ROR https://ror.org/021018s57

  2. 2 Ilustre Colegio Oficial de Geólogos (ICOG)
  3. 3 Universidad de Granada
    info

    Universidad de Granada

    Granada, España

    ROR https://ror.org/04njjy449

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Journal:
Geotemas (Madrid)

ISSN: 1576-5172

Year of publication: 2021

Issue Title: X Congreso Geológico de España

Issue: 18

Pages: 174-177

Type: Article

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More publications in: Geotemas (Madrid)

Abstract

Cartographic, stratigraphic and structural studies in the Alt Palància and Manzanera areas indicate that the Middle-Upper Triassic successions entirely belong to the ‘Mediterranean type of Triassic’. The two carbonate units of the Muschelkalk facies have carbonate-marl alternations both at the base and at the top. The palynological study of claystones and marls allows dating the Röt facies and the three Mus-chelkalk units. The isotopic study of gypsum samples allows distin- guishing the middle Muschelkalk unit from the Keuper unit despite the facies similarity and tectonic disruption.

Data source: Dialnet