Ciclos deltaicos en el Jurásico Superior del flanco oeste del diapiro de Caldas da Rainha, Portugal
Three litoestratigraphic unites have been identified in the São Martinho do Porto sea cliffs, which correspond with three deltaic cycles. The paleocurrents analysis show that for the first two cycles, the sediments come from the Berlengas Massif situated in the SW; while the third come from the NE,...
| Authors: | , , |
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| Format: | article |
| Publication Date: | 1989 |
| Country: | España |
| Institution: | Universidad de Huelva (UHU) |
| Repository: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Language: | Spanish |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/18287 |
| Online Access: | http://hdl.handle.net/10272/18287 |
| Access Level: | Open access |
| Keyword: | Portuguese occidental basin Upper Jurassic Deltas |
| Summary: | Three litoestratigraphic unites have been identified in the São Martinho do Porto sea cliffs, which correspond with three deltaic cycles. The paleocurrents analysis show that for the first two cycles, the sediments come from the Berlengas Massif situated in the SW; while the third come from the NE, controlled by the diapiric relief of the Caldas da Rainha |
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