General Information

Structure type
Deformed/Undeformed
Geological Setting ,
Outcropping/buried
Evaporite unit/s name
Evaporite unit/s age
Evaporite unit/s origin
Classif. (Hudec and Jackson, 2009)
Classif. (Jackson and Talbot, 1986)
Age of evaporite flow or deformation (when deformed) ,
Other comments Recent paleoseismological studies of Quaternary (alluvial and colluvial detrital deposits) affected by the Concud Fault have recognized eleven events between ca. 74 ka BP and the present day (see Ezquerro et al., 2016).

Location

Location

Map (detail)

Location
Location

Geological map

Location

Cross section

Location

Structure type (Hudec and Jackson, 2009)

Location

Regional Stratigraphy

Location

Other maps 1

Location

Other maps 2

Generic Data

Unique ID 84
Name Concud
Structure type Evaporite-detached thrust
Deformed/Undeformed Deformed
Buried/Outcropping Outcropping
Geological setting Iberian Range
Geological Regional Setting Teruel-Jiloca Graben
Evaporite unit/s name Keuper facies
Evaporite unit/s age Carnian-Rhaetian (Upper Triassic)
Evaporite unit/s era Mesozoic
Evaporite unit/s origin Marine
Evaporite unit/s composition Shale-Gypsum-Anhydrite-Ophites
Post-kinematic unit/s (or post-evaporite units when evaporites are undeformed)  Quaternary (alluvial and colluvial detrital deposits)
Post-kinematic unit/s age (or post-evaporite units when evaporites are undeformed) Pleistocene-Holocene
Classification (Hudec and Jackson, 2009) Thrust piercement
Classification (Jackson and Talbot, 1986) Salt wall
Mining activity? N
Mining activity start
Mining activity end
Mining galleries?
Mining products
Mining sub-products
Evaporite flow? Y
Age of evaporite flow Late Miocene-Active now
Flow or deformation triggering mechanisms Active extensional system in the Iberian range
Flow-linked structures? Y
Halokinetic structures Low-angle unconformities / joints
Post-evaporite and pre-kinematic unit/s (overbuden) Jurassic (limestones, dolostones, marlstones, bioclastic limestones marly limestones)
Syn-kinematic unit/s Miocene (shales, claystones, conglomerates, brecchias) ; Pliocene (conglomerates, alluvial deposits) ; Pleistocene-Holocene (alluvial and colluvial deposits)
Available seismic profiles ILIHA C-F
Available boreholes VENTA GUARINA (CAUDE-1) / CAUDE-2 / CELADAS
Additional comments Recent paleo seismological studies of Quaternary (alluvial and colluvial detrital deposits) affected by the Concud Fault have recognized eleven events between ca. 74 ka BP and the present day (see Ezquerro et al., 2016)

Mining Data

UNIQUE_ID 84
Minning exploitations within <2km? N
Historical/Active
Exploitation name #1
Exploitation ID (Spanish National Mining Cadastre) #1
Municipality #1
Province #1
Company #1
Main minning Products #1
Exploitation name #2
Exploitation ID (Spanish National Mining Cadastre) #2
Municipality #2
Province #2
Company #2
Main minning Products #2
Exploitation name #3
Exploitation ID (Spanish National Mining Cadastre) #3
Municipality #3
Province #3
Company #3
Main minning Products #3

Quantitative Data

UNIQUE_ID 84
Outcropping area (km2) 1.65245
Horizontal intersection area (km2) (when buried) Not buried
Depth of intersection area (km2) (when buried) Not buried
Max. Width (Km) 1.51447414
Max. Length (Km) 7.19064132
Max. Evaporites thickness (km) 0.4
Max. Deformation age (Ma) 10
Min. Deformation age (Ma) Active
Deformation stages 1

Reference Data

UNIQUE_ID 84
Section source Lafuente, P., Arlegui, L. E., Liesa, C. L., Pueyo, Ó., Simón, J. L., 2014. Spatial and temporal variation of palaeoseismic activity at an intraplate, historically quiescent structure: The Concud fault (Iberian Chain, Spain). Tectonophysics, 632, 167-187. [link]
Well / Borehole availability #1 n.a.
Well / Borehole availability #2 n.a.
Available data (Stratigraphy) #1 Ezquerro, L., Moretti, M., Liesa, C. L., Luzón, A., Pueyo, E. L., Simón, J. L., 2016. Controls on space–time distribution of soft-sediment deformation structures: applying palaeomagnetic dating to approach the apparent recurrence period of paleoseisms at the Concud Fault (eastern Spain). Sedimentary Geology, 344, 91-111. [link]
Available data (Stratigraphy) #2 Lafuente, P., Arlegui, L. E., Liesa, C. L., Pueyo, Ó., Simón, J. L., 2014. Spatial and temporal variation of palaeoseismic activity at an intraplate, historically quiescent structure: The Concud fault (Iberian Chain, Spain). Tectonophysics, 632, 167-187. [link]
Available data (Stratigraphy) #3 Arche, A., López-Gómez, J., Herranz, P., Márquez-Aliaga, A., Sole de Porta, N., 1995. The Permian and Triassic sediments of the Teruel area, SE Iberian Ranges, Spain/Les sédiments permiens et triasiques de la région de Teruel, Chaîne Ibérique, Espagne. Sciences Géologiques, bulletins et mémoires, 48(1), 101-117. [link]
Available data (Stratigraphy) #4 Alonso-Zarza, A. M., Meléndez, A., Martín-García, R., Herrero, M. J., Martín-Pérez, A., 2012. Discriminating between tectonism and climate signatures in palustrine deposits: lessons from the Miocene of the Teruel Graben, NE Spain. Earth-Science Reviews, 113(3-4), 141-160. [link]
Available data (Stratigraphy) #5 Ezquerro, L., Simón, J. L., Luzón, A., Liesa, C. L., 2020. Segmentation and increasing activity in the Neogene-Quaternary Teruel Basin rift (Spain) revealed by morphotectonic approach. Journal of Structural Geology, 104043. [link]
Available data (Stratigraphy) #6 Arche, A., Gómez, J. L., Marzo, M., Hernández, H. M. V., 2004. The siliciclastic Permian-Triassic deposits in Central and northeastern Iberian Peninsula (Iberian, Ebro and Catalan basins): a proposal for correlation. Geologica Acta, 4, 305-320. [link]
Regional Stratigraphy Ezquerro, L., Lafuente, P., Pesquero, M. D., Alcalá, L., Arlegui, L., Liesa, C., Luque, L., Rodriguez-Pascua, M., Simón, J.L., 2012. Una cubeta endorreica residual Plio-Pleistocena en la zona de relevo entre las fallas de Concud y Teruel: implicaciones paleogeográficas. Revista de la Sociedad Geológica de España, 25, 157-175. [link]
Seismic data availability #1 Diaz, J., Gallart Muset, J., Córdoba, D., Senos, L., Matias, L., Suriñach, E., …, Maguire, P., 2020. The ILIHA deep seismic sounding experiment (Iberian LIthosphere Heterogeneity and Anisotropy). DigitalCSIC – SEISDARE data repository. [link]
Seismic data availability #2 n.a.
Seismic data availability #3 n.a.
Available data (Structure) #1 Ezquerro, L., Simón, J. L., Luzón, A., Liesa, C. L., 2020. Segmentation and increasing activity in the Neogene-Quaternary Teruel Basin rift (Spain) revealed by morphotectonic approach. Journal of Structural Geology, 104043. [link]
Available data (Structure) #2 Lafuente, P., Arlegui, L. E., Casado, I., Ezquerro, L., Liesa, C. L., Pueyo, Ó., Simón, J. L., 2011. Geometría y cinemática de la zona de relevo entre las fallas neógeno-cuaternarias de Concud y Teruel (Cordillera Ibérica). Revista de la Sociedad Geológica de España, 24(1–2), 117-133. [link]
Available data (Structure) #3 Ezquerro, L., Moretti, M., Liesa, C. L., Luzón, A., Pueyo, E. L., Simón, J. L., 2016. Controls on space–time distribution of soft-sediment deformation structures: applying palaeomagnetic dating to approach the apparent recurrence period of paleoseisms at the Concud Fault (eastern Spain). Sedimentary Geology, 344, 91-111. [link]
Available data (Structure) #4 Lafuente, P., Arlegui, L. E., Liesa, C. L., Pueyo, Ó., Simón, J. L., 2014. Spatial and temporal variation of palaeoseismic activity at an intraplate, historically quiescent structure: The Concud fault (Iberian Chain, Spain). Tectonophysics, 632, 167-187. [link]
Available data (Structure) #5 Gracia, A. C., Sainz, A. C., 2000. ¿Tiene el sistema de fosas de Teruel origen extensional?. Revista de la Sociedad Geológica de España, 13(3–4), 445-470. [link]
Available data (Structure) #6 Peiro, A., Simón, J. L., Román-Berdiel, T., 2020. Fault relay zones evolving through distributed longitudinal fractures: The case of the Teruel graben system (Iberian Chain, Spain). Journal of Structural Geology, 131, 103942. [link]
Available data (Analogue modelling) #1 n.a.
Available data (Analogue modelling) #2 n.a.
Available data (Analogue modelling) #3 n.a.
Available data (Gravimetry – Tomography) #1 Ayala, C., Bohoyo, F., Maestro, A., Reguera, M. I., Torne, M., Rubio, F., Fernández, M., García-Lobón, J. L., 2016. Updated Bouguer anomalies of the Iberian Peninsula: a new perspective to interpret the regional geology. Journal of Maps, 12(5), 1089-1092. [link]
Available data (Gravimetry – Tomography) #2 n.a.
Available data (Gravimetry – Tomography) #3 n.a.
Available data (Geochemistry) #1 Ortí, F., García-Veigas, J., Rossell, L., Jurado, M. J., Utrilla, R., 1996. Formaciones salinas de las cuencas triásicas en la Península Ibérica: Caracterización Petrológica y Geoquímica. Cuadernos de Geología Ibérica, 20, 13-35. [link]
Available data (Geochemistry) #2 n.a.
Available data (Geochemistry) #3 n.a.
Available data (Geochemistry) #4 n.a.
Available data (Petrophysics) #1 Ezquerro, L., Moretti, M., Liesa, C. L., Luzón, A., Pueyo, E. L., Simón, J. L., 2016. Controls on space–time distribution of soft-sediment deformation structures: applying palaeomagnetic dating to approach the apparent recurrence period of paleoseisms at the Concud Fault (eastern Spain). Sedimentary Geology, 344, 91-111. [link]
Available data (Petrophysics) #2 n.a.
IGME Geological Map (MAGNA50) Sheet number 567-Teruel. [link]
Other Maps #1 (source) Ezquerro, L., Luzón, A., Simón, J. L., Liesa, C. L., 2019. Alluvial sedimentation and tectono-stratigraphic evolution in a narrow extensional zigzag basin margin (northern Teruel Basin, Spain). Journal of Palaeogeography, 8(1), 1-25. [link]
Other Maps #2 (source) Gracia, A. C., Sainz, A. C., 2000. ¿ Tiene el sistema de fosas de Teruel origen extensional?. Revista de la Sociedad Geológica de España, 13(3–4), 445-470. [link]
Other related references #1 Lago, M., Dumitrescu, R., Bastida, J., Arranz, E., Gil-Imaz, A., Pocovi, A., …, Vaquer, R., 1996. Características de los magmatismos alcalino y subalcalino, pre-Hettangiense, del borde SE de la Cordillera Ibérica. Cuadernos de Geología Ibérica, 20, 159-181. [link]
Other related references #2 Rodríguez-López, J. P., Melendez, N., De Boer, P. L., Soria, A. R., 2012. Controls on marine–erg margin cycle variability: aeolian–marine interaction in the mid‐Cretaceous Iberian Desert System, Spain. Sedimentology, 59(2), 466-501. [link]
Other related references #3 Guitérrez, F., Ortí, F., Gutiérrez, M., Pérez-González, A., Benito, G., Gracia, F. J., Durán, J. J., 2002. Paleosubsidence and active subsidence due to evaporite dissolution in Spain. Carbonates and Evaporites, 17(2), 121. [link]
Other related references #4 n.a.