Sedimentology and diagenetic evolution of the Neogene ‘Intermediate Sandstone Unit’ in the halite deposits of the Granada Basin (SE Spain): the turning point in the change from marine to continental sedimentation

Author:

López-Quirós AdriánORCID,Barbier Mickael,Martín José M.,Guichet Xavier

Funder

IFP Energies Nouvelles

Ministerio de Economía y Competitividad

Publisher

Springer Science and Business Media LLC

Subject

Stratigraphy,Geology

Reference113 articles.

1. Aldaya, F., Vera, J. A., & Fontboté, J. M. (1980). Memoria Mapa Geológico de la Hoja nº 83 (Granada-Málaga). Mapa Geológico de España Escala 1:200.000. Segunda Serie (MAGNA), Primera edición. Instituto Geológico y Minero de España (Madrid).

2. Antler, G., Turchyn, A. V., Rennie, V., Herut, B., & Sivan, O. (2013). Coupled sulfur and oxygen isotope insight into bacterial sulfate reduction in the natural environment. Geochimica et Cosmochimica, 118, 98–117.

3. Arbey, F. (1980). Les formes de la silica et l’identification des évaporites dans les formations silicifies; in Les évaporites, méchanismes, diagenese et applications: Centre de la Recherche, Exploration et Production Elf-Aquitaine. Bulletin, 4, 309–365.

4. Aref, M. A. M., Attia, O. E. A., & Wali, A. M. A. (1997). Facies and depositional environment of the Holocene evaporites in the Ras Shukeir area, Gulf of Suez, Egypt. Sedimentary Geology, 110, 123–145.

5. Ayora, C., Cendón, D. I., Taberner, C., & Pueyo, J. J. (2001). Brine-mineral reactions in evaporite basins: Implications for the composition of ancient oceans. Geology, 29, 251–254.

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