Evidence for an active sinistral shear zone in the western Alboran region
A compilation of gravity, seismicity, neotectonics, geology, tomography and topography data from the Alboran region reveals distinctive differences between the eastern and western part of the Alboran region and Betic Cordillera. Calculated profiles of integrated crustal strength reveal that lateral...
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Published in | Terra nova (Oxford, England) Vol. 13; no. 1; pp. 44 - 50 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Oxford UK
Blackwell Science Ltd
01.02.2001
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Online Access | Get full text |
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Summary: | A compilation of gravity, seismicity, neotectonics, geology, tomography and topography data from the Alboran region reveals distinctive differences between the eastern and western part of the Alboran region and Betic Cordillera. Calculated profiles of integrated crustal strength reveal that lateral differences in mechanical behaviour are caused by marked inherited differences in crustal make‐up. The two domains with different tectonic behaviour are separated by a N025°‐trending lineament in the western Alboran and central Betic Cordillera. This lineament can be interpreted as an upper mantle – lower crustal sinistral shear zone accommodating a large part of the convergence between Africa and Iberia. |
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Bibliography: | istex:91174E591A5EAF7E1E54638E22D503C8AB707D7B ark:/67375/WNG-W81VVVW3-K ArticleID:TER314 |
ISSN: | 0954-4879 1365-3121 |
DOI: | 10.1046/j.1365-3121.2001.00314.x |