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• W1618446783 abstract "A close relationship of the kinematics and timing between low‐angle extensional faulting and upright folding is established for the Miocene detachment systems in the hinterland of the Betics in southeastern Spain. Folding accompanied tectonic denudation developing elongated domes with fold axes both parallel and perpendicular to the direction of extension. The geometry, kinematics, and tectonic evolution of two major sequentially developed extensional fault systems have been characterized in several E‐W elongated mountain ranges of the central Betics on the basis of new cartographic and structural data and a comprehensive revision of other available geological and geophysical observations. The extensional systems have an average WSW direction of extension and led to exhumation of the two lower metamorphic complexes of the Betics, the Nevado‐Filabride and the Alpujarride, during the middle and upper Miocene (Serravallian to Tortonian). The extended domain contains a core complex, with distal and proximal antiformal hinges separated by around 60 km and with a fold amplitude of ∼6 km (measured parallel to the direction of extension). The total amount of extension across the core complex is about 109–116 km, corresponding to a stretching factor (β) of 3.5–3.9, estimated using the distance between fold axial surfaces and a geometrical model accomplishing footwall deformation during tectonic denudation via subvertical simple shear. The elongated domal and basinal geometry of the detachments and their respective footwalls is due to the interference between two sets of orthogonal large‐scale open folds, trending N‐S and E‐W. Longitudinal, N‐S trending folds are interpreted as isostatic folds, i.e., folds that developed in response to differential unloading of the extensional detachment footwalls inducing ductile flow in the middle crust. These folds formed in a rolling‐hinge anticline in which rotation migrates westward through the footwall as it is progressively unroofed. In contrast, E‐W trending folds, being subparallel to the direction of extension, have a contractional origin and progressively affect to the west the isostatically readjusted segments of the detachments once they are inactive. Orthogonal folding occurred since the Serravallian to lower Pliocene. Extension is still active from the rolling‐hinge anticline in Sierra Nevada to the west. The middle Miocene to Pliocene tectonic evolution of the Sierra Nevada elongated dome at the core of the Betic hinterland is another example of the coexistence of extension and contraction during continued overall convergence and mountain‐building." @default.
• W1618446783 created "2016-06-24" @default.
• W1618446783 creator A5069384148 @default.
• W1618446783 creator A5075822798 @default.
• W1618446783 creator A5084771247 @default.
• W1618446783 date "2002-05-25" @default.
• W1618446783 modified "2023-10-14" @default.
• W1618446783 title "Orthogonal folding of extensional detachments: Structure and origin of the Sierra Nevada elongated dome (Betics, SE Spain)" @default.
• W1618446783 cites W1480950765 @default.
• W1618446783 cites W1507532200 @default.
• W1618446783 cites W1965601509 @default.
• W1618446783 cites W1968928752 @default.
• W1618446783 cites W1970159027 @default.
• W1618446783 cites W1970474278 @default.
• W1618446783 cites W1970957370 @default.
• W1618446783 cites W1972575957 @default.
• W1618446783 cites W1975633233 @default.
• W1618446783 cites W1976346293 @default.
• W1618446783 cites W1978217284 @default.
• W1618446783 cites W1982758111 @default.
• W1618446783 cites W1984706520 @default.
• W1618446783 cites W1986557952 @default.
• W1618446783 cites W1991310182 @default.
• W1618446783 cites W1996603428 @default.
• W1618446783 cites W1998029063 @default.
• W1618446783 cites W1998068180 @default.
• W1618446783 cites W1999074220 @default.
• W1618446783 cites W2000279899 @default.
• W1618446783 cites W2001762966 @default.
• W1618446783 cites W2002971217 @default.
• W1618446783 cites W2003897162 @default.
• W1618446783 cites W2006779810 @default.
• W1618446783 cites W2007595592 @default.
• W1618446783 cites W2008835745 @default.
• W1618446783 cites W2008948116 @default.
• W1618446783 cites W2013838554 @default.
• W1618446783 cites W2014911553 @default.
• W1618446783 cites W2019977269 @default.
• W1618446783 cites W2024972260 @default.
• W1618446783 cites W2025290470 @default.
• W1618446783 cites W2025372787 @default.
• W1618446783 cites W2025974824 @default.
• W1618446783 cites W2026017268 @default.
• W1618446783 cites W2027622532 @default.
• W1618446783 cites W2028684644 @default.
• W1618446783 cites W2029022716 @default.
• W1618446783 cites W2030562268 @default.
• W1618446783 cites W2036475527 @default.
• W1618446783 cites W2036490022 @default.
• W1618446783 cites W2040277244 @default.
• W1618446783 cites W2043484891 @default.
• W1618446783 cites W2043569118 @default.
• W1618446783 cites W2044042653 @default.
• W1618446783 cites W2044562894 @default.
• W1618446783 cites W2044920314 @default.
• W1618446783 cites W2049633774 @default.
• W1618446783 cites W2049975394 @default.
• W1618446783 cites W2050416465 @default.
• W1618446783 cites W2051704997 @default.
• W1618446783 cites W2051803722 @default.
• W1618446783 cites W2051822028 @default.
• W1618446783 cites W2052797159 @default.
• W1618446783 cites W2054290430 @default.
• W1618446783 cites W2055539911 @default.
• W1618446783 cites W2058834991 @default.
• W1618446783 cites W2059928531 @default.
• W1618446783 cites W2064387830 @default.
• W1618446783 cites W2064559765 @default.
• W1618446783 cites W2068924392 @default.
• W1618446783 cites W2069591283 @default.
• W1618446783 cites W2072385009 @default.
• W1618446783 cites W2072843794 @default.
• W1618446783 cites W2073818415 @default.
• W1618446783 cites W2075543137 @default.
• W1618446783 cites W2078823158 @default.
• W1618446783 cites W2078978679 @default.
• W1618446783 cites W2082356567 @default.
• W1618446783 cites W2086175305 @default.
• W1618446783 cites W2087506373 @default.
• W1618446783 cites W2088580377 @default.
• W1618446783 cites W2090562894 @default.
• W1618446783 cites W2091020871 @default.
• W1618446783 cites W2092995835 @default.
• W1618446783 cites W2093678814 @default.
• W1618446783 cites W2097671688 @default.
• W1618446783 cites W2101807500 @default.
• W1618446783 cites W2105848445 @default.
• W1618446783 cites W2106189585 @default.
• W1618446783 cites W2112434235 @default.
• W1618446783 cites W2113662488 @default.
• W1618446783 cites W2118326489 @default.
• W1618446783 cites W2120411618 @default.
• W1618446783 cites W2121733203 @default.
• W1618446783 cites W2126373657 @default.
• W1618446783 cites W2127129336 @default.
• W1618446783 cites W2127136348 @default.
• W1618446783 cites W2131822747 @default.
• W1618446783 cites W2135569168 @default.
• W1618446783 cites W2138049016 @default.
• W1618446783 cites W2143157714 @default.

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