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Bicorb-Quesa Diapir

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Journal Article
Published: 01 January 2010
Journal of the Geological Society (2010) 167 (1): 145–153.
... to the BicorbQuesa Diapir. This diapir is composed of evaporitic rocks piercing an overburden of carbonate rocks, providing a wide and contrasting range of electrical resistivity values. In this situation, the MT method may provide a coherent and realistic image of the subsurface. The application of the MT...
FIGURES | View All (7)
Journal Article
Published: 01 April 1996
Journal of the Geological Society (1996) 153 (2): 311–321.
...E. ROCA; P. ANADÓN; R. UTRILLA; A. VÁZQUEZ Abstract The BicorbQuesa diapir belongs to a complex system of evaporite diapirs located in the SE Iberian Peninsula. It was emplaced along the axis of a graben system flanked by two syn-diapir growth basins filled by Miocene sediments. The Miocene...
Journal Article
Journal: AAPG Bulletin
Published: 01 January 2006
AAPG Bulletin (2006) 90 (1): 115–136.
...-related salt welds. In this article, we suggest a new interpretation of these structures as squeezed diapirs based on detailed structural and sedimentological field data of the BicorbQuesa diapir (eastern Prebetics) and offer five analog models, which simulate the polyphase deformation of the eastern...
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Image
(A) Simplified geological map of the Bicorb basin with the location of the BB′ cross section (for map location, see Figure 2). (B-B′) A more detailed cross section through the central part of the Bicorb basin showing the geometric relationships between the Miocene basin fill, the squeezed diapiric stem observed on the northern flank of the Bicorb–Quesa diapir, the later major diapir, and the faults affecting the basin fill and the overburden rocks. No vertical exaggeration. (C) Correlation chart comparing the Miocene tectonic evolution of the Bicorb–Quesa diapir with the main sedimentological and tectonostratigraphic features of the Bicorb basin fill. The synthetic stratigraphic section belongs to the central part of the Bicorb basin. Based on Roca et al. (1996) and Anadón et al. (1998).
Published: 01 January 2006
, the squeezed diapiric stem observed on the northern flank of the BicorbQuesa diapir, the later major diapir, and the faults affecting the basin fill and the overburden rocks. No vertical exaggeration. (C) Correlation chart comparing the Miocene tectonic evolution of the BicorbQuesa diapir with the main
Image
Balanced cross section through the eastern Prebetics showing the main features of the diapiric structures present in this area (for location, see Figure 2). Modified from an unpublished section of M. De Ruig, E. Roca, and M. Sans based on De Ruig (1992), Roca (1992), and Roca et al. (1996) data. The detailed geometry of the squeezed and postcontractional diapirs and primary and secondary welds, as well as of the overlying overburden and basin-fill rocks, are shown in the Bicorb–Quesa diapir and Serra Grossa-Gorda insets. The northern upper part of the Bicorb–Quesa diapir section is a simplification of the cross section BB′ shown in Figure 4.
Published: 01 January 2006
al. (1996) data. The detailed geometry of the squeezed and postcontractional diapirs and primary and secondary welds, as well as of the overlying overburden and basin-fill rocks, are shown in the BicorbQuesa diapir and Serra Grossa-Gorda insets. The northern upper part of the BicorbQuesa diapir
Image
Geological map of Bicorb–Quesa graben system with the piercing Bicorb–Quesa Diapir. B–B', MT modelled cross-section; white dashed box shows location of Figure 4.
Published: 01 January 2010
Fig. 3. Geological map of BicorbQuesa graben system with the piercing BicorbQuesa Diapir. B–B', MT modelled cross-section; white dashed box shows location of Figure 4 .
Image
Simplified geological map of the eastern Prebetics with the location of cross section AA′ shown in Figure 3. Dashed inset in the Bicorb–Quesa diapir area indicates the location of geological map shown in Figure 4. Middle–Upper Triassic diapiric rocks are in black.
Published: 01 January 2006
Figure 2 Simplified geological map of the eastern Prebetics with the location of cross section AA′ shown in Figure 3 . Dashed inset in the BicorbQuesa diapir area indicates the location of geological map shown in Figure 4 . Middle–Upper Triassic diapiric rocks are in black.
Journal Article
Journal: AAPG Bulletin
Published: 15 January 2021
AAPG Bulletin (2021) 105 (1): 53–63.
... , no.  5 , p.  701 – 728 , doi: 10.1306/1D9BC5D9-172D-11D7-8645000102C1865D . Roca , E. , P. Anadón , R. Utrilla , and A. Vázquez , 1996 , Rise, closure and reactivation of the Bicorb-Quesa evaporite diapir, eastern Prebetics, Spain : Journal of the Geological Society , v.  153...
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