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• W2078435752 endingPage "129" @default.
• W2078435752 startingPage "107" @default.
• W2078435752 abstract "An integrated analysis of subsidence and sequence stratigraphy of the Cretaceous successions of the Jumilla–Yecla Region (Betics, SE Spain) is supported by abundant stratigraphical, sedimentological and palaeontological data, with the aim to document and explain the accommodation changes that controlled the evolution and architecture of the carbonate platforms generated during that time on the southern continental margin of Iberia. The Cretaceous shallow marine carbonates and clastics that extensively crop out in the Jumilla–Yecla Region are divided into 11 sequence sets (major stratigraphic units bounded by tectonically induced unconformities), which can be subdivided into several third order depositional sequences and their constituent system tracts. All these genetic units build up a regional chronostratigraphic framework, which is herein used to support subsidence calculations. From the results of the subsidence analysis, seven intervals with characteristic tectonosedimentary patterns were distinguished for Cretaceous time. From these intervals, the first three (respectively early Tithonian–early late Berriasian, late Berriasian–late Hauterivian, and latest Hauterivian to earliest late Albian) were controlled by extensional tectonics, strong enough to mask, during most part of the time, the long-term thermal subsidence inherent to the continental margin. This tectonism was related to the Iberia–Africa divergence and the opening of the North Atlantic. Later, the fourth interval (late Albian–mid Cenomanian) and the sixth interval (late Coniacian to late Santonian) were characterised regionally by, overall, homogeneous subsidence patterns controlled by thermal subsidence, sediment loading and a relative tectonic quiescence. Finally, the fifth and the seventh intervals (respectively latest Cenomanian–early Coniacian and Campanian–Maastrichtian) were characterised by strong tectonic movements and complex subsidence patterns which were related to changes in intraplate stresses related to the onset of the convergence between Africa and Iberia and with the evolution of the Bay of Biscay." @default.
• W2078435752 created "2016-06-24" @default.
• W2078435752 creator A5017769486 @default.
• W2078435752 creator A5037878798 @default.
• W2078435752 creator A5066734518 @default.
• W2078435752 date "2003-11-01" @default.
• W2078435752 modified "2023-10-18" @default.
• W2078435752 title "Integration of subsidence and sequence stratigraphic analyses in the Cretaceous carbonate platforms of the Prebetic (Jumilla–Yecla Region), Spain" @default.
• W2078435752 cites W112890274 @default.
• W2078435752 cites W1484326610 @default.
• W2078435752 cites W1519855472 @default.
• W2078435752 cites W1530377674 @default.
• W2078435752 cites W1532857982 @default.
• W2078435752 cites W1552452377 @default.
• W2078435752 cites W1555588248 @default.
• W2078435752 cites W1558473712 @default.
• W2078435752 cites W1558591015 @default.
• W2078435752 cites W1559200854 @default.
• W2078435752 cites W1562931381 @default.
• W2078435752 cites W1564975307 @default.
• W2078435752 cites W1565054550 @default.
• W2078435752 cites W1590447055 @default.
• W2078435752 cites W1644145629 @default.
• W2078435752 cites W1761232662 @default.
• W2078435752 cites W1893690789 @default.
• W2078435752 cites W191492668 @default.
• W2078435752 cites W1974106972 @default.
• W2078435752 cites W1983330438 @default.
• W2078435752 cites W1984060590 @default.
• W2078435752 cites W1984183896 @default.
• W2078435752 cites W1997252211 @default.
• W2078435752 cites W2001012271 @default.
• W2078435752 cites W2001788443 @default.
• W2078435752 cites W2018804382 @default.
• W2078435752 cites W2019991247 @default.
• W2078435752 cites W2036706368 @default.
• W2078435752 cites W2051819341 @default.
• W2078435752 cites W2052623420 @default.
• W2078435752 cites W2057607406 @default.
• W2078435752 cites W2059131953 @default.
• W2078435752 cites W2059145625 @default.
• W2078435752 cites W2061608310 @default.
• W2078435752 cites W2065020165 @default.
• W2078435752 cites W2065761817 @default.
• W2078435752 cites W2074580673 @default.
• W2078435752 cites W2088033788 @default.
• W2078435752 cites W2088419747 @default.
• W2078435752 cites W2098966379 @default.
• W2078435752 cites W2107760936 @default.
• W2078435752 cites W2107817958 @default.
• W2078435752 cites W2110585121 @default.
• W2078435752 cites W2112338499 @default.
• W2078435752 cites W2112572851 @default.
• W2078435752 cites W2118485173 @default.
• W2078435752 cites W2123117885 @default.
• W2078435752 cites W2125254418 @default.
• W2078435752 cites W2133562679 @default.
• W2078435752 cites W2135886645 @default.
• W2078435752 cites W2141839758 @default.
• W2078435752 cites W2167163594 @default.
• W2078435752 cites W2167557095 @default.
• W2078435752 cites W2230876233 @default.
• W2078435752 cites W2259143260 @default.
• W2078435752 cites W2263460781 @default.
• W2078435752 cites W2291433463 @default.
• W2078435752 cites W2291670795 @default.
• W2078435752 cites W2316940040 @default.
• W2078435752 cites W2742666717 @default.
• W2078435752 cites W2775115782 @default.
• W2078435752 cites W2791509239 @default.
• W2078435752 cites W2889829171 @default.
• W2078435752 cites W2939176893 @default.
• W2078435752 cites W2968647858 @default.
• W2078435752 cites W3014093654 @default.
• W2078435752 cites W30179380 @default.
• W2078435752 cites W3022222581 @default.
• W2078435752 cites W3102749847 @default.
• W2078435752 cites W3112999752 @default.
• W2078435752 cites W3127759058 @default.
• W2078435752 cites W3128198913 @default.
• W2078435752 cites W3131917045 @default.
• W2078435752 cites W3169802802 @default.
• W2078435752 cites W3214980057 @default.
• W2078435752 cites W3216146415 @default.
• W2078435752 cites W55260633 @default.
• W2078435752 cites W630552520 @default.
• W2078435752 cites W635678429 @default.
• W2078435752 cites W646819243 @default.
• W2078435752 cites W840432338 @default.
• W2078435752 cites W981087750 @default.
• W2078435752 cites W2499657496 @default.
• W2078435752 doi "https://doi.org/10.1016/s0031-0182(03)00447-4" @default.
• W2078435752 hasPublicationYear "2003" @default.
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