UGIJAR AND CANJAYAR NEOGENE BASINS (SE SPAIN): AN EXAMPLE OF STRIKE-SLIP BASIN EVOLUTION IN TRANSPRESSIVE REGIME
The present study has been carried out in the eastern part of the Alpujarran corridor (Betic Chain), an E-W trending basin, 80 km long, of Neogene-Quaternary age. In particular, the Ugijar and Canjayar basins (respectively named Basin 1 and Basin 2), controlled by an E-W trending left stepping right...
| Main Authors: | , , , , |
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| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Milano University Press
1990
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| Subjects: | |
| Online Access: | https://riviste.unimi.it/index.php/RIPS/article/view/9034 https://doi.org/10.13130/2039-4942/9034 |
| _version_ | 1829937826468200448 |
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| author | BOCCALETTI, M. GELATI, R. MORATTI, G. PAPANI, G. VISMARA SCHILLING, A. |
| author_facet | BOCCALETTI, M. GELATI, R. MORATTI, G. PAPANI, G. VISMARA SCHILLING, A. |
| author_sort | BOCCALETTI, M. |
| collection | University of Milan: Riviste UNIMI |
| description | The present study has been carried out in the eastern part of the Alpujarran corridor (Betic Chain), an E-W trending basin, 80 km long, of Neogene-Quaternary age. In particular, the Ugijar and Canjayar basins (respectively named Basin 1 and Basin 2), controlled by an E-W trending left stepping right lateral strikeslip system, associated with NE-SW trending thrust faults, have been investigated. The stratigraphic sequence of the forementioned two basins, which can be up to 2000 m thick, is mainly due to tectonic subsidence and is here interpreted in terms of Sequence Stratigraphy. The age of the whole sequence, dated by means of planktonic foraminifera, is Late Serravallian-Pliocene. |
| format | Article in Journal/Newspaper |
| genre | Planktonic foraminifera |
| genre_facet | Planktonic foraminifera |
| id | ftunivmilriv:oai:ojs.riviste.unimi.it:article/9034 |
| institution | Open Polar |
| language | English |
| op_collection_id | ftunivmilriv |
| op_doi | https://doi.org/10.13130/2039-4942/9034 |
| op_relation | https://riviste.unimi.it/index.php/RIPS/article/view/9034/8579 https://riviste.unimi.it/index.php/RIPS/article/view/9034 |
| op_rights | Copyright (c) 2017 M. BOCCALETTI, R. GELATI, G. MORATTI, G. PAPANI, A. VISMARA SCHILLING |
| op_source | RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA Vol. 96 No. 2-3 (1990) Rivista italiana di Paleontologia e Stratigrafia; V. 96 N. 2-3 (1990) 2039-4942 0035-6883 |
| publishDate | 1990 |
| publisher | Milano University Press |
| record_format | openpolar |
| spelling | ftunivmilriv:oai:ojs.riviste.unimi.it:article/9034 2025-04-20T14:43:44+00:00 UGIJAR AND CANJAYAR NEOGENE BASINS (SE SPAIN): AN EXAMPLE OF STRIKE-SLIP BASIN EVOLUTION IN TRANSPRESSIVE REGIME BOCCALETTI, M. GELATI, R. MORATTI, G. PAPANI, G. VISMARA SCHILLING, A. 1990-08-31 application/pdf https://riviste.unimi.it/index.php/RIPS/article/view/9034 https://doi.org/10.13130/2039-4942/9034 eng eng Milano University Press https://riviste.unimi.it/index.php/RIPS/article/view/9034/8579 https://riviste.unimi.it/index.php/RIPS/article/view/9034 Copyright (c) 2017 M. BOCCALETTI, R. GELATI, G. MORATTI, G. PAPANI, A. VISMARA SCHILLING RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA Vol. 96 No. 2-3 (1990) Rivista italiana di Paleontologia e Stratigrafia; V. 96 N. 2-3 (1990) 2039-4942 0035-6883 Strike-slip basin Betic Chain Transpressive regime Neogene info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1990 ftunivmilriv https://doi.org/10.13130/2039-4942/9034 2025-04-09T03:31:12Z The present study has been carried out in the eastern part of the Alpujarran corridor (Betic Chain), an E-W trending basin, 80 km long, of Neogene-Quaternary age. In particular, the Ugijar and Canjayar basins (respectively named Basin 1 and Basin 2), controlled by an E-W trending left stepping right lateral strikeslip system, associated with NE-SW trending thrust faults, have been investigated. The stratigraphic sequence of the forementioned two basins, which can be up to 2000 m thick, is mainly due to tectonic subsidence and is here interpreted in terms of Sequence Stratigraphy. The age of the whole sequence, dated by means of planktonic foraminifera, is Late Serravallian-Pliocene. Article in Journal/Newspaper Planktonic foraminifera University of Milan: Riviste UNIMI |
| spellingShingle | Strike-slip basin Betic Chain Transpressive regime Neogene BOCCALETTI, M. GELATI, R. MORATTI, G. PAPANI, G. VISMARA SCHILLING, A. UGIJAR AND CANJAYAR NEOGENE BASINS (SE SPAIN): AN EXAMPLE OF STRIKE-SLIP BASIN EVOLUTION IN TRANSPRESSIVE REGIME |
| title | UGIJAR AND CANJAYAR NEOGENE BASINS (SE SPAIN): AN EXAMPLE OF STRIKE-SLIP BASIN EVOLUTION IN TRANSPRESSIVE REGIME |
| title_full | UGIJAR AND CANJAYAR NEOGENE BASINS (SE SPAIN): AN EXAMPLE OF STRIKE-SLIP BASIN EVOLUTION IN TRANSPRESSIVE REGIME |
| title_fullStr | UGIJAR AND CANJAYAR NEOGENE BASINS (SE SPAIN): AN EXAMPLE OF STRIKE-SLIP BASIN EVOLUTION IN TRANSPRESSIVE REGIME |
| title_full_unstemmed | UGIJAR AND CANJAYAR NEOGENE BASINS (SE SPAIN): AN EXAMPLE OF STRIKE-SLIP BASIN EVOLUTION IN TRANSPRESSIVE REGIME |
| title_short | UGIJAR AND CANJAYAR NEOGENE BASINS (SE SPAIN): AN EXAMPLE OF STRIKE-SLIP BASIN EVOLUTION IN TRANSPRESSIVE REGIME |
| title_sort | ugijar and canjayar neogene basins (se spain): an example of strike-slip basin evolution in transpressive regime |
| topic | Strike-slip basin Betic Chain Transpressive regime Neogene |
| topic_facet | Strike-slip basin Betic Chain Transpressive regime Neogene |
| url | https://riviste.unimi.it/index.php/RIPS/article/view/9034 https://doi.org/10.13130/2039-4942/9034 |