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Artículos de revistas sobre el tema "Basque-Cantabrian Basin"

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Publicado: 10 de marzo de 2023
Última modificación: 11 de marzo de 2023

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1

Calvo-Rathert, M., J. Cuevas, J. M. Tubía, M. F. Bógalo y A. Gogichaishvili. "A paleomagnetic study of the Basque Arc (Basque-Cantabrian Basin, Western Pyrenees)". International Journal of Earth Sciences 96, n.º 6 (19 de enero de 2007): 1163–78. http://dx.doi.org/10.1007/s00531-006-0149-8.

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2

Beroiz, C. y A. Permanyer. "HYDROCARBON HABITAT OF THE SEDANO TROUGH, BASQUE-CANTABRIAN BASIN, SPAIN". Journal of Petroleum Geology 34, n.º 4 (20 de septiembre de 2011): 387–409. http://dx.doi.org/10.1111/j.1747-5457.2011.00511.x.

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3

Lescoutre, Rodolphe y Gianreto Manatschal. "Role of rift-inheritance and segmentation for orogenic evolution: example from the Pyrenean-Cantabrian system". BSGF - Earth Sciences Bulletin 191 (2020): 18. http://dx.doi.org/10.1051/bsgf/2020021.

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The Basque-Cantabrian junction corresponds to an inverted rift accommodation zone at the limit between the former hyperextended Pyrenean and Cantabrian rift segments. The recognition of an inherited rift segment boundary allows to investigate the reactivation associated with large-scale rift segmentation in an orogenic system. We use criteria from published field observations and seismic data to propose a new map of rift domains for the Basque-Cantabrian junction. We also provide balanced cross-sections that allow to define the along-strike architecture associated with segmentation during rifting and subsequent Alpine reactivation. Based on these results, this study aims to characterize and identify reactivated and newly formed structures during inversion of two rift segments and its intermitted segment boundary. It also aims to describe the timing of thin-skinned and thick-skinned deformation associated with the inversion of segmented rift systems. During convergence, two phases have been recognized within the rift segment (eastern Mauléon basin). The Late Cretaceous to Paleocene underthrusting/subduction phase was mostly governed by thin-skinned deformation that reactivated the former hyperextended domains and the supra-salt sedimentary cover. The Eocene to Miocene collisional phase, controlled by thick-skinned deformation that took place once necking domains collided and formed an orogenic wedge. At the rift segment boundary, the underthrusting/subduction phase was already controlled by thick-skinned deformation due to the formation of shortcutting thrust faults at the termination of overlapping V-shaped rift segments. This led to the formation of a proto-wedge composed of the Basque massifs. We suggest that this proto-wedge is responsible for the preservation of pre-Alpine structures in the Basque massifs and for the emplacement of subcontinental mantle rocks at a crustal level beneath the western Mauléon basin. These results argue for a first order cylindrical orogenic architecture from the Central Pyrenean segment to the Cantabrian segment (up to the Santander transfer zone) despite rift segmentation. They also highlight the control of 3D rift-inheritance for the initial phase of orogenic evolution and for the local architecture of mountain belts.
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4

Gómez, Manuel, Jaume Vergés y Carlos Riaza. "Inversion tectonics of the northern margin of the Basque Cantabrian Basin". Bulletin de la Société Géologique de France 173, n.º 5 (1 de septiembre de 2002): 449–59. http://dx.doi.org/10.2113/173.5.449.

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Abstract The northern margin of the Basque-Cantabrian Basin was analysed combining stratigraphic and structural data from both surface and subsurface together with reflectance of vitrinite data from oil wells. The use of cross-section balancing techniques in addition to thermal modelling enabled us to reconstruct the tectonic, burial and thermal evolutions of the basin margin as well as those of the Landes High to the N in two different periods. The section restoration at the end of the Cretaceous shows a northern basin margin structure influenced by evaporites related to south-dipping normal faults. The reconstruction in middle Eocene times yielded up to 1 800 m of Paleocene-middle Eocene deposits on top of the basin margin. Subsequent tectonic inversion related to the Pyrenean compression led to the north-directed thrusting of basement units and to the formation of thrust slices or inverted folds in the cover along the northern margin of the basin. Tectonic subsidence analysis together with maturity data provided evidence that oil was generated in the basin during the late syn-rift and post-rift stages in the Late Cretaceous and became overmature during the period of incipient inversion after 55 Ma. In the autochthonous Landes High, the oil was generated after the tectonic inversion period 37 Ma.
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5

Cámara, Pedro. "Inverted turtle salt anticlines in the Eastern Basque-Cantabrian basin, Spain". Marine and Petroleum Geology 117 (julio de 2020): 104358. http://dx.doi.org/10.1016/j.marpetgeo.2020.104358.

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6

García-Mondéjar, J., L. M. Agirrezabala, A. Aranburu, P. A. Fernández-Mendiola, I. Gómez-Pérez, M. López-Horgue y I. Rosales. "Aptian— Albian tectonic pattern of the Basque— Cantabrian Basin (Northern Spain)". Geological Journal 31, n.º 1 (marzo de 1996): 13–45. http://dx.doi.org/10.1002/(sici)1099-1034(199603)31:1<13::aid-gj689>3.0.co;2-y.

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7

Morales, Tomás, Gorka Uribe-Etxebarria, Jesús A. Uriarte y Iñigo Fernández de Valderrama. "Geomechanical characterisation of rock masses in Alpine regions: the Basque Arc (Basque-Cantabrian basin, Northern Spain)". Engineering Geology 71, n.º 3-4 (febrero de 2004): 343–62. http://dx.doi.org/10.1016/s0013-7952(03)00160-1.

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8

Ábalos, B. "Geologic map of the Basque-Cantabrian Basin and a new tectonic interpretation of the Basque Arc". International Journal of Earth Sciences 105, n.º 8 (25 de enero de 2016): 2327–54. http://dx.doi.org/10.1007/s00531-016-1291-6.

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9

Miró, Jordi, Josep A. Muñoz, Gianreto Manatschal y Eduard Roca. "The Basque – Cantabrian Pyrenees: report of data analysis". BSGF - Earth Sciences Bulletin 191 (2020): 22. http://dx.doi.org/10.1051/bsgf/2020024.

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This contribution presents the analysis of a data set that was put together in the PhD thesis of Jordi Miró which is part of the OROGEN Project. The Basque – Cantabrian Pyrenees, that are the focus of this report, have been extensively studied over the last years. Several open debates in the Earth Science community aroused from this realm regarding the formation and reactivation of rift domains and formation of fold and thrust belts. This report summarizes the main tectonic models proposed to explain both the extension and reactivation history over this area and compile a series of data to consider for further discussions and interpretations. This report includes a thematic map of the Basque – Cantabrian Pyrenees showing an analysis of the tectono-stratigraphic evolution of the area. The map covers an area of more than 33 000 km2 and is a graphic representation of the geology of the region based on a large geodatabase including previous published maps and field observations. A composite reflection seismic line crossing the entire Basque – Cantabrian Pyrenees from the Ebro foreland basin to the offshore Landes High is also presented. This section enables to present a continuous dataset along the entire area with the projection of few drill holes, which are presented with the stratigraphic logs following the same tectono-stratigraphic legend obtained from the previous analysis. The main goal of this data report is to provide a coherent and complete dataset to the community, which enables to propose, discuss and test some of the new concepts related to the formation and reactivation of rifted margins. This data report is complementary to the contributions of Lescoutre and Manatschal (2020) and Cadenas et al. (in prep) that are part of the same special volume.
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10

Salazar Ramírez, Roselis W. y Concha Herrero. "LOWER TOARCIAN FORAMINIFERA OF THE SAN ANDRÉS SECTION (BASQUE-CANTABRIAN BASIN, SPAIN)". Journal of Foraminiferal Research 45, n.º 4 (octubre de 2015): 321–43. http://dx.doi.org/10.2113/gsjfr.45.4.321.

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11

Fernandez-Mendiola, P. A. y J. García-Mondejar. "Mid-cretaceous palaeogeographical evolution of the central Basque-Cantabrian basin (northern Spain)". Palaeogeography, Palaeoclimatology, Palaeoecology 81, n.º 1-2 (diciembre de 1990): 115–26. http://dx.doi.org/10.1016/0031-0182(90)90043-7.

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12

Aróstegui, J., M. C. Zuluaga, F. Velasco, M. Ortega-Huertas y F. Nieto. "Diagenesis of the Central Basque-Cantabrian Basin (Iberian Peninsula) based on illite-smectite distribution". Clay Minerals 26, n.º 4 (diciembre de 1991): 535–48. http://dx.doi.org/10.1180/claymin.1991.026.4.08.

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AbstractX-ray diffraction was used to analyse the distribution of clay minerals in the <2 µm fraction of the lutitic and marly facies from the centre of the Basque-Cantabrian Basin (Basque Arc), where the sedimentary section is 2000 to 10,000 m thick. Most of the deposits were laid down during the Cretaceous and Paleogene and were related to the opening and closing of the Bay of Biscay. The most noteworthy variations are in kaolinite, smectite and mixed-layered (R = 0, R = 1 and R ≥ 3) illite-smectite, which can be ascribed both to provenance and to diagenesis. A general diminution in expandability is related to the gradual transformation of smectite to illite from south to north, and with depth. Temperature, residence time and chemical activity during diagenesis are the factors that had greatest influence on the changes in the original mineral assemblages inherited from the source area. On the basis of the clay minerals and the Kübler index, a general scheme is proposed for the diagenetic evolution of the area from the initial stages to anchimetamorphism.
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13

Ducoux, Maxime, Laurent Jolivet, Emmanuel Masini, Romain Augier, Abdeltif Lahfid, Matthias Bernet y Sylvain Calassou. "Distribution and intensity of High-Temperature Low-Pressure metamorphism across the Pyrenean-Cantabrian belt: constraints on the thermal record of the pre-orogenic hyperextension rifting". BSGF - Earth Sciences Bulletin 192 (2021): 43. http://dx.doi.org/10.1051/bsgf/2021029.

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Whereas a straightforward link between crustal thinning and geothermal gradients during rifting is now well established, the thermal structure of sedimentary basins within hyperextended domains remains poorly documented. For this purpose, we investigate the spatial distribution of rift-related High-Temperature Low-Pressure (HT/LP) metamorphism recorded in the preserved hyperextended rift basins inverted and integrated in the Pyrenean-Cantabrian belt. Based on Vitrinite Reflectance (Ro) data measured in 169 boreholes and more than 200 peak-metamorphic temperatures (Tmax) data obtained by Raman Spectroscopy of Carbonaceous Material (RSCM) added to ∼425 previously published Tmax data, we propose a new map depicting the spatial distribution of the HT/LP metamorphism of the Pyrenean-Cantabrian belt. We also provide three regional-scale geological cross-sections associated with Ro and Tmax data to constrain the distribution of paleo-isograds at depth. Based on these results, we show that the impact of rift-related metamorphism is restricted to the pre- and syn-rift sequence suggested by the depth profiles of Ro values measured in different tectonostratigraphic intervals (pre-, syn- and post-rift and syn-convergence sediments). However, a small strip of early orogenic sediments (Santonian in age) appears also affected by high temperatures along the North Pyrenean Frontal Thrust and above the Grand Rieu ridge, which we attribute to the percolation of hot hydrothermal fluids sourced from the dehydration of underthrust basement and/or sedimentary rocks at depth during the early orogenic stage. The map shows that the HT/LP metamorphism (reaching ∼500 °C) is recorded with similar intensity along the Pyrenean-Cantabrian belt from the west in the Basque-Cantabrian Basin to the east in the Boucheville and Bas-Agly basins, for similar burial and rift-related structural settings. This thermal peak is also recorded underneath the northern border of the Mauléon Basin (calibrated by wells). It suggests that the high temperatures were recorded at the basement-sediment interface underneath the most distal part of the hyperextended domain. At basin-scale, we observe in the Basque-Cantabrian, Mauléon-Arzacq and Tarascon rift segments an asymmetry of the thermal structure revealed by different horizontal thermal gradients, supporting an asymmetry of the former hyperextended rift system. Using our results, we compare the Pyrénées to the Alps that also recorded hyperextension but no HT/LP metamorphic event and suggest that the high-temperature record within the basins depends on high sedimentation rate promoting a thermal blanketing effect and circulation of hydrothermal fluids.
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14

Gomez-Perez, I., P. A. Fernandez-Mendiola y J. Garcia-Mondejar. "A mixed carbonate-siliciclastic ramp model (Upper Aptian, Basque-Cantabrian Basin, Northern Iberia)". Géologie Méditerranéenne 21, n.º 3 (1994): 77–80. http://dx.doi.org/10.3406/geolm.1994.1531.

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15

AGIRREZABALA, LUIS MIGUEL y JAUME DINARÈS-TURELL. "Albian syndepositional block rotation and its geological consequences, Basque–Cantabrian Basin (western Pyrenees)". Geological Magazine 150, n.º 6 (2 de mayo de 2013): 986–1001. http://dx.doi.org/10.1017/s0016756813000149.

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AbstractStratigraphic, structural, palaeocurrent and palaeomagnetic analyses of Upper Albian deep-water deposits in and around the Deba block (Northern Iberia) are presented. Results indicate an anticlockwise vertical-axis rotation of this block by 35° during a maximum time span of c. 1 Ma (Late Albian intra-C. auritus ammonite Subzone). This Albian syndepositional block rotation is interpreted to be the consequence of the coeval activity of conjugate major sinistral strike-slip faults and minor (antithetic) dextral strike-slip faults, which border the Deba block. On the base of conservative estimations, a minimum block-rotation rate of 35° Ma−1 and a sinistral strike-slip rate of 1.2 km Ma−1 are calculated. As a consequence of the interaction of the rotated Deba block with adjacent non-rotated blocks, its corners experienced coeval transpressive (NW and SE corners) and transtensional deformations (SW and, possibly, NE corners). At the transtensional SW corner, two domal high-reflective seismic structures have been recorded and interpreted as high-level magmatic laccoliths. These magmatic intrusions triggered the development of a mineralizing hydrothermal system, which vented to the Late Albian seafloor warm to hot hydrocarbon-rich fluids. Vented hydrocarbon was generated from Albian organic-rich sediments by contact alteration with hydrothermal fluids.
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16

Bermúdez-Rochas, David Didier. "New hybodont shark assemblage from the Early Cretaceous of the Basque-Cantabrian Basin". Geobios 42, n.º 6 (noviembre de 2009): 675–86. http://dx.doi.org/10.1016/j.geobios.2009.06.004.

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17

Pérez-García, Adán, Iratxe Boneta, Alfonso Alday y Xabier Murelaga. "The oldest Quaternary turtle remains from the Basque-Cantabrian Basin (Atxoste, Álava, Spain)". Comptes Rendus Palevol 14, n.º 6-7 (septiembre de 2015): 605–11. http://dx.doi.org/10.1016/j.crpv.2014.12.002.

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18

López-Horgue, Mikel A. y Arantxa Bodego. "Mesozoic and Cenozoic decapod crustaceans from the Basque-Cantabrian basin (Western Pyrenees): new occurrences and faunal turnovers in the context of basin evolution". Bulletin de la Société géologique de France 188, n.º 3 (2017): 14. http://dx.doi.org/10.1051/bsgf/2017180.

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Twenty-nine new identifications of fossil decapod crustacean remains in the Basque-Cantabrian Basin (Western Pyrenees) spanning from the Jurassic to the Miocene and coming from twenty-four new and five yet known localities are described here for the first time. These remains represent a substantial advance in the knowledge of these faunas and their diversity in this basin, giving an accurate image of the decapod faunal succession. The study includes a taxonomical description and discussion with reference to the known occurrences. Their accurate dating and the environmental ascription have been possible after the analysis of the stratigraphic occurrence in the context of a well-known basinal stratigraphy. This has ultimately permitted a brief analysis of the decapod palaeoecology and faunal turnovers in the context of basin evolution.
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19

Velasco, F., J. M. Herrero, I. Yusta, J. A. Alonso, I. Seebold y D. Leach. "Geology and Geochemistry of the Reocin Zinc-Lead Deposit, Basque-Cantabrian Basin, Northern Spain". Economic Geology 98, n.º 7 (1 de noviembre de 2003): 1371–96. http://dx.doi.org/10.2113/gsecongeo.98.7.1371.

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20

SWENNEN, RUDY, JULIE DEWIT, ELS FIERENS, PHILIPPE MUCHEZ, MUMTAZ SHAH, FADI NADER y DAVID HUNT. "Multiple dolomitization events along the Pozalagua Fault (Pozalagua Quarry, Basque-Cantabrian Basin, Northern Spain)". Sedimentology 59, n.º 4 (31 de enero de 2012): 1345–74. http://dx.doi.org/10.1111/j.1365-3091.2011.01309.x.

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21

Bodego, Arantxa, Eneko Iriarte, Luis Miguel Agirrezabala, Joaquín García-Mondéjar y Mikel A. López-Horgue. "Synextensional mid-Cretaceous stratigraphic architecture of the eastern Basque–Cantabrian basin margin (western Pyrenees)". Cretaceous Research 55 (julio de 2015): 229–61. http://dx.doi.org/10.1016/j.cretres.2015.01.006.

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22

Ossó, Àlex y Josep Anton Moreno-Bedmar. "A new species of Etyus Leach in MANTELL, 1822 (Decapoda, Brachyura, Etyidae) from the lower Aptian (Lower Cretaceous) of Cantabria, Spain". Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 296, n.º 1 (1 de mayo de 2020): 175–83. http://dx.doi.org/10.1127/njgpa/2020/0892.

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A new species of etyid crab, Etyus tresgalloi, is recorded from outcrops of Aptian sedimentary rocks at Cuchía (Cantabria, northern Spain). The dorsal carapace of the sole specimen recovered possesses sufficient diagnostic characters such as general carapace outline and, in particular, configuration of branchial grooves, to allow it to be assigned to the Etyidae, despite the fact that it does not retain any ventral elements or appendages. This new record brings the number of brachyurans recorded from the Aptian of the Basque-Cantabrian Basin to three. Based on ammonite evidence, Etyus tresgalloi n. sp. is dated as early Aptian (Deshayesites forbesi ammonite Zone).
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23

Morales, Tomás, Jon Ander Clemente, Laura Damas Mollá, Eñaut Izagirre y Jesus A. Uriarte. "Analysis of instabilities in the Basque Coast Geopark coastal cliffs for its environmentally friendly management (Basque-Cantabrian basin, northern Spain)". Engineering Geology 283 (marzo de 2021): 106023. http://dx.doi.org/10.1016/j.enggeo.2021.106023.

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24

Martín, Adriana, Miguel Sevilla y Joaquín Zurutuza. "Western Pyrenees geodetic deformation study using the Guipuzcoa GNSS network". Journal of Applied Geodesy 12, n.º 3 (26 de julio de 2018): 229–38. http://dx.doi.org/10.1515/jag-2017-0041.

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Abstract The Basque Country in the north of Spain is located inside the Basque-Cantabrian basin of the western Pyrenees which remarkable seismic-tectonic implications justify the need of geodetic control in the area. In order to perform a crustal deformation study we have analysed all daily observations from the GNSS permanent network of Guipuzcoa and external IGS stations, from January 2007 to November 2011. We have carried out the data processing applying double differences methodology in the automatic processing module BPE (Bernese Processing Engine) from Bernese GNSS software version 5.0. Solution was aligned to geodetic reference framework ITRF2008, by using the IGS08 solution and updated satellite and terrestrial antennas calibration. This five years network study results: Coordinate time series, velocities and baseline lengths variations show internal stability among inner stations and from them with respect to outer IGS stations, concluding that no deformations have been observed.
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25

Alonso, Jesus, Antonio Arillo, Eduardo Barrón, J. Carmelo Corral, Joan Grimalt, Jordi F. López, Rafael López et al. "A new fossil resin with biological inclusions in Lower Cretaceous deposits from Álava (northern Spain, Basque-Cantabrian Basin)". Journal of Paleontology 74, n.º 1 (enero de 2000): 158–78. http://dx.doi.org/10.1017/s0022336000031334.

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The occurrence of amber in Sierra de Cantabria (álava, Basque Country) has been known for more than two decades but biological inclusions have only recently been found. The existence of crustaceans (amphipods and isopods), chelicerates (acari and arachnids), 12 orders of insects, and several bird feathers are reported in this preliminary study. In addition, there are leaf remains, molluscs, and a fair number of inorganic inclusions.Pollen analysis of the clastic series indicates an age between upper Aptian—middle Albian, which allows an assignment of this stratigraphic unit to the Nograro Formation. Chemical analysis indicates that the amber has high maturity, which reflects its Cretaceous age. Chemical composition analysis also indicates an araucariacean origin, which is corroborated by pollen found within the amber deposit.This new fossil site provides information for the reconstruction of paleocommunities of arthropods and sedimentary environments in the extreme south of the Basque-Cantabrian Basin during the Lower Cretaceous, characterized by coniferous forests with an understory of vascular cryptograms. Some of the identified arthropods add to the fossil record for various groups that are poorly known or unknown for this time period. This Lagerstätte constitutes one of the most important deposits of Mesozoic amber in the world.
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26

García-Mondéjar, Joaquín, Pedro A. Fernández-Mendiola y Hugh G. Owen. "The OAE1a in Cuchía (Early Aptian, Spain): C and O geochemistry and global correlation". Acta Geologica Polonica 65, n.º 4 (1 de diciembre de 2015): 525–43. http://dx.doi.org/10.1515/agp-2015-0023.

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Abstract C-isotopes, TOC and O geochemical data from the lower Aptian Cuchía section in the western Basque-Cantabrian basin (BCB) allow an accurate delimitation of the OAE1a-equivalent and its geochemical Menegatti´s segments, a detailed δ13Ccarb correlation with regional and interregional sections, and a high-resolution construction of TOC and bulk-rock δ18Ocarb curves and their interpretation. The δ13Ccarb values range from -2‰ and +4‰ (VPDB). They agree with previous data from the eastern BCB sections (Aralar) confirming the ammonite age of the OAE1a in the Basque-Cantabrian basin: Deshayesites forbesi, Deshayesites deshayesi, and Deshayesites deshayesi-Dufrenoyia furcata transition Zones. Interregional δ13Ccarb correlation with pelagic (Cismon, Italy, and Mid-Pacific Mountains, DSDP Site 463) and neritic (Roquefort-La Bédoule, France) core sections, reveals a common profile of a wide negative excursion characteristic of the OAE1a. It consists of a double trough separated by a flat relative maximum, with two negative spikes in the upper trough of neritic sections. TOC absolute values range from 0.12% to 1.37%. Segments of the TOC curve with persistent low values closely correspond with descending segments of the δ13Ccarb curve, and are attributed to lesser organic productivity in the BCB. Detailed bulk-rock δ18Ocarb data (-5.71‰ to -1.05 ‰ PDB) and variation curve show two main positive O-isotope shifts and three minor positive inflections, within a general negative trend characteristic of the OAE1a. The two major positive shifts correspond to both shallowing upwards sequences and the lowermost can be related to a eustatic sea level fall. Independent interregional correlation of the O-isotope shifts with C-isotopes supports their interpretation as punctuating colder events within a general warming trend.
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27

Márquez-Aliaga, Ana, Susana Damborenea, Juan José Gómez y Antonio Goy. "Bivalves from the Triassic-Jurassic transition in Northern Spain (Asturias and Western Basque-Cantabrian Basin)". Ameghiniana 47, n.º 2 (junio de 2010): 185–205. http://dx.doi.org/10.5710/amgh.v47i2.3.

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28

Alcalde, J., D. Martí, C. Juhlin, A. Malehmir, D. Sopher, E. Saura, I. Marzán et al. "3-D reflection seismic imaging of the Hontomín structure in the Basque-Cantabrian Basin (Spain)". Solid Earth Discussions 5, n.º 2 (13 de septiembre de 2013): 1575–614. http://dx.doi.org/10.5194/sed-5-1575-2013.

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Abstract. The Basque-Cantabrian Basin of the Northern Iberia peninsula constitutes a unique example of a major deformation system, featuring a dome structure developed by extensional tectonics followed by compressional reactivation. The occurrence of natural resources in the area and the possibility of establishing a geological storage site for carbon dioxide motivated the acquisition of a 3-D seismic reflection survey in 2010, centered on the Jurassic Hontomín dome. The objectives of this survey were to obtain a geological model of the overall structure and to establish a baseline model for a possible geological CO2 storage site. The 36 km2 survey included approximately 5000 mixed (Vibroseis and explosives) source points recorded with a 25 m inline source and receiver spacing. The target reservoir is a saline aquifer, at approximately 1450 m depth, encased and sealed by carbonate formations. Acquisition and processing parameters were influenced by the rough topography and relatively complex geology. A strong near surface velocity inversion is evident in the data, affecting the quality of the data. The resulting 3-D image provides constraints on the key features of the geologic model. The Hontomín structure is interpreted to consist of an approximately 107 m2 large elongated dome with two major W–E and NW–SE striking faults bounding it.
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29

Alcalde, J., D. Martí, C. Juhlin, A. Malehmir, D. Sopher, E. Saura, I. Marzán et al. "3-D reflection seismic imaging of the Hontomín structure in the Basque–Cantabrian Basin (Spain)". Solid Earth 4, n.º 2 (9 de diciembre de 2013): 481–96. http://dx.doi.org/10.5194/se-4-481-2013.

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Abstract. The Basque–Cantabrian Basin of the northern Iberia Peninsula constitutes a unique example of a major deformation system, featuring a dome structure developed by extensional tectonics followed by compressional reactivation. The occurrence of natural resources in the area and the possibility of establishing a geological storage site for carbon dioxide motivated the acquisition of a 3-D seismic reflection survey in 2010, centered on the Jurassic Hontomín dome. The objectives of this survey were to obtain a geological model of the overall structure and to establish a baseline model for a possible geological CO2 storage site. The 36 km2 survey included approximately 5000 mixed (Vibroseis and explosives) source points recorded with a 25 m inline source and receiver spacing. The target reservoir is a saline aquifer, at approximately 1450 m depth, encased and sealed by carbonate formations. Acquisition and processing parameters were influenced by the rough topography and relatively complex geology. A strong near-surface velocity inversion is evident in the data, affecting the quality of the data. The resulting 3-D image provides constraints on the key features of the geologic model. The Hontomín structure is interpreted to consist of an approximately 107 m2 large elongated dome with two major (W–E and NW–SE) striking faults bounding it. Preliminary capacity estimates indicate that about 1.2 Gt of CO2 can be stored in the target reservoir.
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30

Soto, Ruth, Antonio M. Casas-Sainz, Juan J. Villalaín y Belén Oliva-Urcia. "Mesozoic extension in the Basque–Cantabrian basin (N Spain): Contributions from AMS and brittle mesostructures". Tectonophysics 445, n.º 3-4 (diciembre de 2007): 373–94. http://dx.doi.org/10.1016/j.tecto.2007.09.007.

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31

Frankovic, Allen, Luis Eguiluz y Luis M. Martínez-Torres. "Geodynamic evolution of the Salinas de Añana diapir in the Basque-Cantabrian Basin, Western Pyrenees". Journal of Structural Geology 83 (febrero de 2016): 13–27. http://dx.doi.org/10.1016/j.jsg.2015.12.001.

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32

Tavani, Stefano y Josep Anton Muñoz. "Mesozoic rifting in the Basque-Cantabrian Basin (Spain): Inherited faults, transversal structures and stress perturbation". Terra Nova 24, n.º 1 (1 de diciembre de 2011): 70–76. http://dx.doi.org/10.1111/j.1365-3121.2011.01040.x.

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33

Berrezueta, Edgar, Timea Kovacs y Linda Luquot. "Qualitative and Quantitative Changes of Carbonate Rocks Exposed to SC CO2 (Basque-Cantabrian Basin, Northern Spain)". Applied Sciences 7, n.º 11 (1 de noviembre de 2017): 1124. http://dx.doi.org/10.3390/app7111124.

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34

Cuevas, J. y J. M. Tubia. "The discovery of scapolite marbles in the Biscay Synclinorium (Basque-Cantabrian basin, Western Pyrenees): geodynamic implications". Terra Nova 11, n.º 6 (10 de diciembre de 1999): 259–65. http://dx.doi.org/10.1046/j.1365-3121.1999.00255.x.

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35

Santamaria, Robert y Martinez Ricardo. "Preliminary report on Middle Coniacian-Lower Santonian Ammonite distribution from the Basque-Cantabrian Basin (Northern Spain)". Geobios 26 (enero de 1993): 341–45. http://dx.doi.org/10.1016/s0016-6995(06)80388-8.

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36

López-Horgue, M. A., E. Iriarte, S. Schröder, P. A. Fernández-Mendiola, B. Caline, H. Corneyllie, J. Frémont, M. Sudrie y S. Zerti. "Structurally controlled hydrothermal dolomites in Albian carbonates of the Asón valley, Basque Cantabrian Basin, Northern Spain". Marine and Petroleum Geology 27, n.º 5 (mayo de 2010): 1069–92. http://dx.doi.org/10.1016/j.marpetgeo.2009.10.015.

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37

Ábalos, B., A. Alkorta y V. Iríbar. "Geological and isotopic constraints on the structure of the Bilbao anticlinorium (Basque–Cantabrian basin, North Spain)". Journal of Structural Geology 30, n.º 11 (noviembre de 2008): 1354–67. http://dx.doi.org/10.1016/j.jsg.2008.07.008.

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38

Perilli, Nicola, Ángela Fraguas y María José Comas-Rengifo. "Reproducibility and reliability of the Pliensbachian calcareous nannofossil biohorizons from the Basque-Cantabrian Basin (Northern Spain)". Geobios 43, n.º 1 (enero de 2010): 77–85. http://dx.doi.org/10.1016/j.geobios.2009.06.009.

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39

Agirrezabala, L. M., F. Sarrionandia y M. Carracedo-Sánchez. "Diatreme-forming volcanism in a deep-water faulted basin margin: Lower Cretaceous outcrops from the Basque-Cantabrian Basin, western Pyrenees". Journal of Volcanology and Geothermal Research 337 (mayo de 2017): 124–39. http://dx.doi.org/10.1016/j.jvolgeores.2017.03.019.

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40

Ducoux, M., L. Jolivet, J. ‐P Callot, C. Aubourg, E. Masini, A. Lahfid, E. Homonnay, F. Cagnard, C. Gumiaux y T. Baudin. "The Nappe des Marbres Unit of the Basque‐Cantabrian Basin: The Tectono‐thermal Evolution of a Fossil Hyperextended Rift Basin". Tectonics 38, n.º 11 (noviembre de 2019): 3881–915. http://dx.doi.org/10.1029/2018tc005348.

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41

Fernández-Mendiola, Pedro A., J. García-Mondéjar y H. G. Owen. "Comments on “New insight on the age of the Aparein black shales in the Basque-Cantabrian Basin, northern Spain” Frau, Camille." Newsletters on Stratigraphy 54, n.º 4 (2 de septiembre de 2021): 497–99. http://dx.doi.org/10.1127/nos/2021/0668.

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42

Elorza, Javier, Juan José Gómez-Alday y Álvaro Jiménez Berrocoso. "Syndepositional processes in the pigmentation of oceanic red beds: evidence from the Basque–Cantabrian Basin (northern Spain)". Geological Magazine 158, n.º 9 (13 de abril de 2021): 1683–703. http://dx.doi.org/10.1017/s0016756821000248.

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AbstractOceanic red beds (ORBs) are present in Upper Cretaceous and Danian deep-marine deposits in the Basque–Cantabrian Basin of northern Spain. The presence and regularity of the succession of marl–limestone couplets is exceptional based on the macroscopic, microscopic and geochemical evidence collected. Five types of marl–limestone couplets are identified based on the colour, and a high maximum sedimentation rate (3.6 cm ka–1 ) is noted. The oxidizing activity of deep, cold-water masses is indicated by the oxygen isotope signal in the lower–upper Maastrichtian and Danian sections and the presence of the boreal inoceramid Spyridoceramus tegulatus. In theory, the variation in colour from grey to greenish-yellow, purple and pink up to red tones correlates with the Fe2+/(Fe2++Fe3+) ratio. It is interpreted as the possible palaeoenvironmental transit of particles that sediment out slowly in oxic environments when they circulate through cooler, oxidizing water masses. The colour is considered to be a depositional feature, and hematite, detected by X-ray diffraction, is the main staining agent, without discarding the possible redistribution of previous oxyhydroxides passing to hematite as a final product. The cell filling of the foraminifer shells does not incorporate appreciable amounts of Fe and Mg during diagenesis. Bacterial activity is detected using scanning electron microscopy images, both in the coccolith debris and in the detrital micas, although there is uncertainty as to its importance in the staining process.
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43

Iriarte, E., M. A. López-Horgue, S. Schroeder y B. Caline. "Interplay between fracturing and hydrothermal fluid flow in the Asón Valley hydrothermal dolomites (Basque–Cantabrian Basin, Spain)". Geological Society, London, Special Publications 370, n.º 1 (2012): 207–27. http://dx.doi.org/10.1144/sp370.10.

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44

Nieto, F. "Evolution of Illite/Smectite from Early Diagenesis through Incipient Metamorphism in Sediments of the Basque-Cantabrian Basin". Clays and Clay Minerals 44, n.º 3 (1996): 304–23. http://dx.doi.org/10.1346/ccmn.1996.0440302.

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45

Bodego, A., E. Iriarte, M. A. López-Horgue y I. Álvarez. "Rift-margin extensional forced folds and salt tectonics in the eastern Basque-Cantabrian rift basin (western Pyrenees)". Marine and Petroleum Geology 91 (marzo de 2018): 667–82. http://dx.doi.org/10.1016/j.marpetgeo.2018.02.007.

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46

Radmacher, Wiesława, Karolina Kobos, Jarosław Tyszka, Agata Jarzynka y José Antonio Arz. "Palynological indicators of palaeoenvironmental perturbations in the Basque-Cantabrian Basin during the latest Cretaceous (Zumaia, northern Spain)". Marine and Petroleum Geology 112 (febrero de 2020): 104107. http://dx.doi.org/10.1016/j.marpetgeo.2019.104107.

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47

Agirrezabala, Luis M., Carmen Dorronsoro y Albert Permanyer. "Geochemical correlation of pyrobitumen fills with host mid-Cretaceous Black Flysch Group (Basque-Cantabrian Basin, western Pyrenees)". Organic Geochemistry 39, n.º 8 (agosto de 2008): 1185–88. http://dx.doi.org/10.1016/j.orggeochem.2008.03.012.

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48

Salazar-Ramírez, Roselis W., Concha Herrero y Antonio Goy. "Lower Toarcian ammonite and foraminifera assemblages in the San Miguel de Aguayo Section (Basque-Cantabrian Basin, Spain)". Journal of Iberian Geology 46, n.º 1 (10 de diciembre de 2019): 39–60. http://dx.doi.org/10.1007/s41513-019-00118-8.

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49

Benito-Calvo, Alfonso, Antonio Tarriño, Pedro José Lobo, Iosu Junguitu y David Larreina. "Geomorphology and prehistoric flint mining evidence in the Sierra de Araico (Basque-Cantabrian Basin), Burgos-Álava, Spain". Journal of Maps 6, n.º 1 (enero de 2010): 584–90. http://dx.doi.org/10.4113/jom.2010.1147.

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50

Fraaije, René H. B., Mikel A. López-Horgue, Niel L. Bruce, Barry W. M. van Bakel, Pedro Artal, John W. M. Jagt y Adiël A. Klompmaker. "New isopod and achelatan crustaceans from mid–Cretaceous reefal limestones in the Basque-Cantabrian Basin, northern Spain". Cretaceous Research 101 (septiembre de 2019): 61–69. http://dx.doi.org/10.1016/j.cretres.2019.04.012.

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