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Journal articles on the topic 'Basque-Cantabrian Basin'

Author: Grafiati

Published: 10 March 2023

Last updated: 31 July 2025

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1

Boneta Jiménez, Iratxe, Corina Liesau Von Lettow-Vorbeck, and Adán Pérez-García. "European Pond Turtle (Emys orbicularis) remains in Iron Age contexts of the Spanish Northem Iberian Peninsula." Archaeofauna 31 (October 11, 2023): 97–108. http://dx.doi.org/10.15366/archaeofauna2022.31.004.

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The aim of this paper is to present some new data concerning the systematic identifications of several terrapin findings documented in three Iberian Iron Age sites from the Northern Meseta and Basque-Cantabrian Basin: El Soto de Medinilla (Valladolid), La Mota (Valladolid) and La Hoya (Álava). New interpretations concerning the first-hand study of these remains are presented. With the aim of comprehending the interaction of humans with these reptiles, we consider that they were mainly captured as a food resource. The previous identification of Emys orbicularis (i.e., the European Pond Turtle)

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Calvo-Rathert, M., J. Cuevas, J. M. Tubía, M. F. Bógalo, and A. Gogichaishvili. "A paleomagnetic study of the Basque Arc (Basque-Cantabrian Basin, Western Pyrenees)." International Journal of Earth Sciences 96, no. 6 (2007): 1163–78. http://dx.doi.org/10.1007/s00531-006-0149-8.

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3

Lescoutre, Rodolphe, and 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 rift

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4

Beroiz, C., and A. Permanyer. "HYDROCARBON HABITAT OF THE SEDANO TROUGH, BASQUE-CANTABRIAN BASIN, SPAIN." Journal of Petroleum Geology 34, no. 4 (2011): 387–409. http://dx.doi.org/10.1111/j.1747-5457.2011.00511.x.

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Gómez, Manuel, Jaume Vergés, and Carlos Riaza. "Inversion tectonics of the northern margin of the Basque Cantabrian Basin." Bulletin de la Société Géologique de France 173, no. 5 (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

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6

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

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7

García-Mondéjar, J., L. M. Agirrezabala, A. Aranburu, et al. "Aptian— Albian tectonic pattern of the Basque— Cantabrian Basin (Northern Spain)." Geological Journal 31, no. 1 (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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8

Morales, Tomás, Gorka Uribe-Etxebarria, Jesús A. Uriarte, and Iñigo Fernández de Valderrama. "Geomechanical characterisation of rock masses in Alpine regions: the Basque Arc (Basque-Cantabrian basin, Northern Spain)." Engineering Geology 71, no. 3-4 (2004): 343–62. http://dx.doi.org/10.1016/s0013-7952(03)00160-1.

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9

Ábalos, B. "Geologic map of the Basque-Cantabrian Basin and a new tectonic interpretation of the Basque Arc." International Journal of Earth Sciences 105, no. 8 (2016): 2327–54. http://dx.doi.org/10.1007/s00531-016-1291-6.

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10

Miró, Jordi, Josep A. Muñoz, Gianreto Manatschal, and 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 con

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Salazar Ramírez, Roselis W., and Concha Herrero. "LOWER TOARCIAN FORAMINIFERA OF THE SAN ANDRÉS SECTION (BASQUE-CANTABRIAN BASIN, SPAIN)." Journal of Foraminiferal Research 45, no. 4 (2015): 321–43. http://dx.doi.org/10.2113/gsjfr.45.4.321.

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12

Fernandez-Mendiola, P. A., and J. García-Mondejar. "Mid-cretaceous palaeogeographical evolution of the central Basque-Cantabrian basin (northern Spain)." Palaeogeography, Palaeoclimatology, Palaeoecology 81, no. 1-2 (1990): 115–26. http://dx.doi.org/10.1016/0031-0182(90)90043-7.

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13

B. I., Odoh,, Ahaneku, C. V., Nwafuluibeya, S. C., et al. "Comprehensive Basin Analysis and Petroleum Potential Evaluation of Ayoluengo Oil Field, Basque-Cantabrian Basin, Spain." Journal of Geography, Environment and Earth Science International 28, no. 10 (2024): 125–42. http://dx.doi.org/10.9734/jgeesi/2024/v28i10830.

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This study presents a comprehensive basin analysis and petroleum potential evaluation of the Ayoluengo oil field in the Basque-Cantabrian Basin, Spain. Using an integrated approach combining geological, geophysical, and geochemical data, we analyzed the basin's evolution and petroleum system elements. The dataset included 2D and 3D seismic data, well logs, formation tops, and geophysical maps. Our analysis revealed a complex structural framework characterized by salt diapirism and halokinetic structures. Well log interpretation and sequence stratigraphic analysis identified two genetic sequenc

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14

Ducoux, Maxime, Laurent Jolivet, Emmanuel Masini, et al. "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

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15

Aróstegui, J., M. C. Zuluaga, F. Velasco, M. Ortega-Huertas, and F. Nieto. "Diagenesis of the Central Basque-Cantabrian Basin (Iberian Peninsula) based on illite-smectite distribution." Clay Minerals 26, no. 4 (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 expan

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Gomez-Perez, I., P. A. Fernandez-Mendiola, and J. Garcia-Mondejar. "A mixed carbonate-siliciclastic ramp model (Upper Aptian, Basque-Cantabrian Basin, Northern Iberia)." Géologie Méditerranéenne 21, no. 3 (1994): 77–80. http://dx.doi.org/10.3406/geolm.1994.1531.

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17

AGIRREZABALA, LUIS MIGUEL, and JAUME DINARÈS-TURELL. "Albian syndepositional block rotation and its geological consequences, Basque–Cantabrian Basin (western Pyrenees)." Geological Magazine 150, no. 6 (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 e

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18

Bermúdez-Rochas, David Didier. "New hybodont shark assemblage from the Early Cretaceous of the Basque-Cantabrian Basin." Geobios 42, no. 6 (2009): 675–86. http://dx.doi.org/10.1016/j.geobios.2009.06.004.

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19

Pérez-García, Adán, Iratxe Boneta, Alfonso Alday, and Xabier Murelaga. "The oldest Quaternary turtle remains from the Basque-Cantabrian Basin (Atxoste, Álava, Spain)." Comptes Rendus Palevol 14, no. 6-7 (2015): 605–11. http://dx.doi.org/10.1016/j.crpv.2014.12.002.

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20

López-Horgue, Mikel A., and 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, no. 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

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21

Ladron de Guevara Aguirreche, Martin, Arantxa Bodego, Eneko Iriarte, Luis Troya, Laura Damas-Mollá, and Arantza Aranburu. "Evidence of a Cenomanian shallow-marine carbonate platform in the northwestern margin of the Bortziriak-Cinco Villas massif, eastern Basque-Cantabrian Basin." Geogaceta 74 (December 18, 2023): 19–22. http://dx.doi.org/10.55407/geogaceta98191.

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Basin margin evolution of rift basins is not always well constrained. In the northeastern margin of the Basque-Cantabrian Basin, a revision of a carbonate succession permits deciphering the transition from synto post-rift phases in the poorly studied northwestern margin of the Bortziriak-Cinco Villas massif. The sedimentological analysis shows three main lithofacies, attributed to a shallow-marine, non-rimmed carbonate platform. On the other hand, biostratigraphic analysis based on the presence of Caprina adversa rudist indicates a Cenomanian age for the succession. Thus, this study illustrate

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22

Ossó, Àlex, and 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, no. 1 (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 tresgall

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23

Velasco, F., J. M. Herrero, I. Yusta, J. A. Alonso, I. Seebold, and D. Leach. "Geology and Geochemistry of the Reocin Zinc-Lead Deposit, Basque-Cantabrian Basin, Northern Spain." Economic Geology 98, no. 7 (2003): 1371–96. http://dx.doi.org/10.2113/gsecongeo.98.7.1371.

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24

SWENNEN, RUDY, JULIE DEWIT, ELS FIERENS, et al. "Multiple dolomitization events along the Pozalagua Fault (Pozalagua Quarry, Basque-Cantabrian Basin, Northern Spain)." Sedimentology 59, no. 4 (2012): 1345–74. http://dx.doi.org/10.1111/j.1365-3091.2011.01309.x.

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25

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

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26

Martín, Adriana, Miguel Sevilla, and Joaquín Zurutuza. "Western Pyrenees geodetic deformation study using the Guipuzcoa GNSS network." Journal of Applied Geodesy 12, no. 3 (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.

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García-Mondéjar, Joaquín, Pedro A. Fernández-Mendiola, and Hugh G. Owen. "The OAE1a in Cuchía (Early Aptian, Spain): C and O geochemistry and global correlation." Acta Geologica Polonica 65, no. 4 (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: Deshayes

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Alonso, Jesus, Antonio Arillo, Eduardo Barrón, et al. "A new fossil resin with biological inclusions in Lower Cretaceous deposits from Álava (northern Spain, Basque-Cantabrian Basin)." Journal of Paleontology 74, no. 1 (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 Form

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Morales, Tomás, Jon Ander Clemente, Laura Damas Mollá, Eñaut Izagirre, and 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 (March 2021): 106023. http://dx.doi.org/10.1016/j.enggeo.2021.106023.

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30

Márquez-Aliaga, Ana, Susana Damborenea, Juan José Gómez, and Antonio Goy. "Bivalves from the Triassic-Jurassic transition in Northern Spain (Asturias and Western Basque-Cantabrian Basin)." Ameghiniana 47, no. 2 (2010): 185–205. http://dx.doi.org/10.5710/amgh.v47i2.3.

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31

Alcalde, J., D. Martí, C. Juhlin, et al. "3-D reflection seismic imaging of the Hontomín structure in the Basque-Cantabrian Basin (Spain)." Solid Earth Discussions 5, no. 2 (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

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Alcalde, J., D. Martí, C. Juhlin, et al. "3-D reflection seismic imaging of the Hontomín structure in the Basque–Cantabrian Basin (Spain)." Solid Earth 4, no. 2 (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

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33

Soto, Ruth, Antonio M. Casas-Sainz, Juan J. Villalaín, and Belén Oliva-Urcia. "Mesozoic extension in the Basque–Cantabrian basin (N Spain): Contributions from AMS and brittle mesostructures." Tectonophysics 445, no. 3-4 (2007): 373–94. http://dx.doi.org/10.1016/j.tecto.2007.09.007.

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

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35

Tavani, Stefano, and Josep Anton Muñoz. "Mesozoic rifting in the Basque-Cantabrian Basin (Spain): Inherited faults, transversal structures and stress perturbation." Terra Nova 24, no. 1 (2011): 70–76. http://dx.doi.org/10.1111/j.1365-3121.2011.01040.x.

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36

Berrezueta, Edgar, Timea Kovacs, and Linda Luquot. "Qualitative and Quantitative Changes of Carbonate Rocks Exposed to SC CO2 (Basque-Cantabrian Basin, Northern Spain)." Applied Sciences 7, no. 11 (2017): 1124. http://dx.doi.org/10.3390/app7111124.

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Cuevas, J., and J. M. Tubia. "The discovery of scapolite marbles in the Biscay Synclinorium (Basque-Cantabrian basin, Western Pyrenees): geodynamic implications." Terra Nova 11, no. 6 (1999): 259–65. http://dx.doi.org/10.1046/j.1365-3121.1999.00255.x.

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

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López-Horgue, M. A., E. Iriarte, S. Schröder, et al. "Structurally controlled hydrothermal dolomites in Albian carbonates of the Asón valley, Basque Cantabrian Basin, Northern Spain." Marine and Petroleum Geology 27, no. 5 (2010): 1069–92. http://dx.doi.org/10.1016/j.marpetgeo.2009.10.015.

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Ábalos, B., A. Alkorta, and V. Iríbar. "Geological and isotopic constraints on the structure of the Bilbao anticlinorium (Basque–Cantabrian basin, North Spain)." Journal of Structural Geology 30, no. 11 (2008): 1354–67. http://dx.doi.org/10.1016/j.jsg.2008.07.008.

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41

Perilli, Nicola, Ángela Fraguas, and María José Comas-Rengifo. "Reproducibility and reliability of the Pliensbachian calcareous nannofossil biohorizons from the Basque-Cantabrian Basin (Northern Spain)." Geobios 43, no. 1 (2010): 77–85. http://dx.doi.org/10.1016/j.geobios.2009.06.009.

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42

Ladron de Guevara Aguirreche, Martin, Arantxa Bodego, and Eneko Iriarte. "Albitization evidences of Mesozoic carbonates: petrological study of authigenic albites in the northwest of the Bortziriak Cinco Villas Massif, eastern Basque-Cantabrian Basin." Geogaceta 74 (December 18, 2023): 31–34. http://dx.doi.org/10.55407/geogaceta98190.

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The presence of authigenic Na-feldspars in sedimentary carbonate rocks is unusual and its origin is controversial in terms of genesis and timing. The use of optical microscopy, cathodoluminescence and in situ semi-quantitative EDX analysis techniques, has allowed the identification and characterization of authigenic albite crystals in the Mesozoic pre- and syn-rift carbonates of the northwestern margin of the Bortziriak-Cinco Villas Massif, in the northeastern Basque-Cantabrian Basin (western Pyrenees). The euhedral habit, crystal size, spatial distribution and crosscutting relationships, toge

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Agirrezabala, L. M., F. Sarrionandia, and 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 (May 2017): 124–39. http://dx.doi.org/10.1016/j.jvolgeores.2017.03.019.

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44

Ducoux, M., L. Jolivet, J. ‐P Callot, et al. "The Nappe des Marbres Unit of the Basque‐Cantabrian Basin: The Tectono‐thermal Evolution of a Fossil Hyperextended Rift Basin." Tectonics 38, no. 11 (2019): 3881–915. http://dx.doi.org/10.1029/2018tc005348.

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45

Elorza, Javier, Juan José Gómez-Alday, and Álvaro Jiménez Berrocoso. "Syndepositional processes in the pigmentation of oceanic red beds: evidence from the Basque–Cantabrian Basin (northern Spain)." Geological Magazine 158, no. 9 (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 pr

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Iriarte, E., M. A. López-Horgue, S. Schroeder, and 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, no. 1 (2012): 207–27. http://dx.doi.org/10.1144/sp370.10.

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Nieto, F. "Evolution of Illite/Smectite from Early Diagenesis through Incipient Metamorphism in Sediments of the Basque-Cantabrian Basin." Clays and Clay Minerals 44, no. 3 (1996): 304–23. http://dx.doi.org/10.1346/ccmn.1996.0440302.

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

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Radmacher, Wiesława, Karolina Kobos, Jarosław Tyszka, Agata Jarzynka, and 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 (February 2020): 104107. http://dx.doi.org/10.1016/j.marpetgeo.2019.104107.

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Agirrezabala, Luis M., Carmen Dorronsoro, and Albert Permanyer. "Geochemical correlation of pyrobitumen fills with host mid-Cretaceous Black Flysch Group (Basque-Cantabrian Basin, western Pyrenees)." Organic Geochemistry 39, no. 8 (2008): 1185–88. http://dx.doi.org/10.1016/j.orggeochem.2008.03.012.

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