Role of an extension of pre-Quaternary age for the evolution of the carbonate massifs in the occidental Betic Cordillera; the case of the Yunquera-Nieves Massif (southern Spain)
A simultaneous analysis of the fracture geometry and paleo-stress fields of the karstic Yunquera-Nieves massif in southern Spain (Malaga Province) has been carried out with microtectonic stations. It reveals polyphased tectonics linked to the structural position of this carbonate domain in the weste...
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| Veröffentlicht in: | Bulletin de la Société géologique de France 2002-01, Vol.173 (5), p.437-448 |
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| creator | Pistre, Séverin Liñán, Cristina Andreo, Bartolomé Carrasco, Francisco Drogue, Claude Martín-Algarra, Agustín |
| description | A simultaneous analysis of the fracture geometry and paleo-stress fields of the karstic Yunquera-Nieves massif in southern Spain (Malaga Province) has been carried out with microtectonic stations. It reveals polyphased tectonics linked to the structural position of this carbonate domain in the western Betic Cordillera. Among the tectonic regimes described in this domain appears a distensive stage with a radial trend probably of post-Tortonian to Quaternary age. Todate, it has seldom been described and is absent from geodynamic models though it seems to have had a regional importance. Furthermore, it played a major role for the acquisition of the hydrodynamic properties of the aquifer and its karstogenesis. This stage opened all fractures and allowed the development of karstic drains with NW-SE and N-S directions. Finally, the karstic network was shaped by more recent climatic and tectonic events. |
| doi_str_mv | 10.2113/173.5.437 |
| format | Article |
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It reveals polyphased tectonics linked to the structural position of this carbonate domain in the western Betic Cordillera. Among the tectonic regimes described in this domain appears a distensive stage with a radial trend probably of post-Tortonian to Quaternary age. Todate, it has seldom been described and is absent from geodynamic models though it seems to have had a regional importance. Furthermore, it played a major role for the acquisition of the hydrodynamic properties of the aquifer and its karstogenesis. This stage opened all fractures and allowed the development of karstic drains with NW-SE and N-S directions. 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It reveals polyphased tectonics linked to the structural position of this carbonate domain in the western Betic Cordillera. Among the tectonic regimes described in this domain appears a distensive stage with a radial trend probably of post-Tortonian to Quaternary age. Todate, it has seldom been described and is absent from geodynamic models though it seems to have had a regional importance. Furthermore, it played a major role for the acquisition of the hydrodynamic properties of the aquifer and its karstogenesis. This stage opened all fractures and allowed the development of karstic drains with NW-SE and N-S directions. Finally, the karstic network was shaped by more recent climatic and tectonic events.</description><subject>Andalusia Spain</subject><subject>aquifers</subject><subject>Betic Cordillera</subject><subject>carbonate rocks</subject><subject>Cenozoic</subject><subject>Earth Sciences</subject><subject>Earth, ocean, space</subject><subject>Europe</subject><subject>Exact sciences and technology</subject><subject>extension</subject><subject>fractured materials</subject><subject>fractures</subject><subject>ground water</subject><subject>histograms</subject><subject>hydraulic conductivity</subject><subject>Hydrogeology</subject><subject>Iberian Peninsula</subject><subject>IGCP</subject><subject>karst</subject><subject>karst hydrology</subject><subject>Malaga Spain</subject><subject>Marine</subject><subject>Miocene</subject><subject>Neogene</subject><subject>neotectonics</subject><subject>porosity</subject><subject>preferential flow</subject><subject>Sciences of the Universe</subject><subject>sedimentary rocks</subject><subject>Southern Europe</subject><subject>Spain</subject><subject>statistical analysis</subject><subject>stress</subject><subject>structural controls</subject><subject>Structural geology</subject><subject>tectonics</subject><subject>Tectonics. Structural geology. Plate tectonics</subject><subject>Tertiary</subject><subject>Yunquera-Nieves Massif</subject><issn>0037-9409</issn><issn>1777-5817</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2002</creationdate><recordtype>article</recordtype><recordid>eNp9ks2OFCEUhStGE9vRhW_ARjMTUy3ULYquuBo76pi0Gv8Wrsht6jLDhIEWqlp9LN9Q-kdn54rcez4OXA5V9VjweSMEPBcK5nLegrpTzYRSqpYLoe5WM85B1X3L-_vVg5yvS9mBFLPq96foiUXLMDD6OVLILoZdvUlUf5xwpBQw_WJ4SczGxMYrYrSNfhqP3K5hMK1jKCy7wZydzcyFvRCNcQOFET17SaMzbBnT4LynhC-OOzP9dfk2he9TUer3jraU2bu9FzvNcSpyCuzzBl04e1jds-gzPTquJ9XX16--LC_q1Yc3b5fnqxqh7cZa2NbCAJYjX7f90FuJrZALbq0yHLu9ZhBINdASqXWnrJIwrBtqOQzNAk6qs4PvFXq9Se6mPIOO6PTF-UrvehwAZNOJrSjs0wO7SbHMkEd947Ih7zFQnLIWCwnQAy_g6f9B2QhYNJ0Ut-ebFHNOZP9dQnC9y1qXrLXUJevCPjnaYjbobcJgXL7d0IKAvtl5PjtwlxSzcRQM_YjJD_o6TiVnn3VTfkaZTJXJ4A9fVbiQ</recordid><startdate>20020101</startdate><enddate>20020101</enddate><creator>Pistre, Séverin</creator><creator>Liñán, Cristina</creator><creator>Andreo, Bartolomé</creator><creator>Carrasco, Francisco</creator><creator>Drogue, Claude</creator><creator>Martín-Algarra, Agustín</creator><general>Société Géologique de France</general><general>Société géologique de France</general><general>Société géologique de France - EDP Sciences</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope><scope>1XC</scope><orcidid>https://orcid.org/0000-0002-6301-8801</orcidid></search><sort><creationdate>20020101</creationdate><title>Role of an extension of pre-Quaternary age for the evolution of the carbonate massifs in the occidental Betic Cordillera; the case of the Yunquera-Nieves Massif (southern Spain)</title><author>Pistre, Séverin ; Liñán, Cristina ; Andreo, Bartolomé ; Carrasco, Francisco ; Drogue, Claude ; Martín-Algarra, Agustín</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a346t-1f4f3d3f0a0b49d9f5a41580ff7c0a6f3d3fca3e7234ee7b67f753db2e403d283</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2002</creationdate><topic>Andalusia Spain</topic><topic>aquifers</topic><topic>Betic Cordillera</topic><topic>carbonate rocks</topic><topic>Cenozoic</topic><topic>Earth Sciences</topic><topic>Earth, ocean, space</topic><topic>Europe</topic><topic>Exact sciences and technology</topic><topic>extension</topic><topic>fractured materials</topic><topic>fractures</topic><topic>ground water</topic><topic>histograms</topic><topic>hydraulic conductivity</topic><topic>Hydrogeology</topic><topic>Iberian Peninsula</topic><topic>IGCP</topic><topic>karst</topic><topic>karst hydrology</topic><topic>Malaga Spain</topic><topic>Marine</topic><topic>Miocene</topic><topic>Neogene</topic><topic>neotectonics</topic><topic>porosity</topic><topic>preferential flow</topic><topic>Sciences of the Universe</topic><topic>sedimentary rocks</topic><topic>Southern Europe</topic><topic>Spain</topic><topic>statistical analysis</topic><topic>stress</topic><topic>structural controls</topic><topic>Structural geology</topic><topic>tectonics</topic><topic>Tectonics. Structural geology. Plate tectonics</topic><topic>Tertiary</topic><topic>Yunquera-Nieves Massif</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Pistre, Séverin</creatorcontrib><creatorcontrib>Liñán, Cristina</creatorcontrib><creatorcontrib>Andreo, Bartolomé</creatorcontrib><creatorcontrib>Carrasco, Francisco</creatorcontrib><creatorcontrib>Drogue, Claude</creatorcontrib><creatorcontrib>Martín-Algarra, Agustín</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Bulletin de la Société géologique de France</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Pistre, Séverin</au><au>Liñán, Cristina</au><au>Andreo, Bartolomé</au><au>Carrasco, Francisco</au><au>Drogue, Claude</au><au>Martín-Algarra, Agustín</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Role of an extension of pre-Quaternary age for the evolution of the carbonate massifs in the occidental Betic Cordillera; the case of the Yunquera-Nieves Massif (southern Spain)</atitle><jtitle>Bulletin de la Société géologique de France</jtitle><date>2002-01-01</date><risdate>2002</risdate><volume>173</volume><issue>5</issue><spage>437</spage><epage>448</epage><pages>437-448</pages><issn>0037-9409</issn><eissn>1777-5817</eissn><coden>BSGFAE</coden><abstract>A simultaneous analysis of the fracture geometry and paleo-stress fields of the karstic Yunquera-Nieves massif in southern Spain (Malaga Province) has been carried out with microtectonic stations. 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| ispartof | Bulletin de la Société géologique de France, 2002-01, Vol.173 (5), p.437-448 |
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| subjects | Andalusia Spain aquifers Betic Cordillera carbonate rocks Cenozoic Earth Sciences Earth, ocean, space Europe Exact sciences and technology extension fractured materials fractures ground water histograms hydraulic conductivity Hydrogeology Iberian Peninsula IGCP karst karst hydrology Malaga Spain Marine Miocene Neogene neotectonics porosity preferential flow Sciences of the Universe sedimentary rocks Southern Europe Spain statistical analysis stress structural controls Structural geology tectonics Tectonics. Structural geology. Plate tectonics Tertiary Yunquera-Nieves Massif |
| title | Role of an extension of pre-Quaternary age for the evolution of the carbonate massifs in the occidental Betic Cordillera; the case of the Yunquera-Nieves Massif (southern Spain) |
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