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[EN] The Middle Triassic in the NW of the Iberian Basin consists of both and terrigenous sediments. A new sedimentary model is proposed the clastic wedge of the Cuesta del Castillo Saudstones and Siltstones (CCSS) Formation (García-Gil, 1990), and its relationship with the Upper carbonate Formations. model will take account of the following characteristics: 1. Low depositional gradient being integrated in a homoclinal carbonate . 2. Combined tectonic, climatic aud eustatic controis. 3. Presence of continental and shallow marine facies associations. 4. Homogeneity of textural facies. sedimentation of the CCSS Formation took place during a relative sea rise (high stand system tract).
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Soledad García‐Gil (1991) studied this question.
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