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 Host rocks show a unusual, reduced piercement (see Teixell and Barnolas 1995). The diapir is surrounded by a thicker overburden and a significant thickness of syntectonic deposits of the Graus–Tremp Basin. Genetically linked to the Mediano salt-cored anticline (ID #066): pop-up structure evolved from the salt-cored Mediano anticline during Lutetian.

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 54
Name Clamosa
Structure type Evaporite diapir
Deformed/Undeformed Deformed
Buried/Outcropping Outcropping
Geological setting Southern Pyrenees
Geological Regional Setting South Pyrenees Central Unit (Sierras Marginales; Boltaña-Balzes thrust sheet)
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-Marlstone-Gypsum-Halite-Anhydrite
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) Erosional piercement
Classification (Jackson and Talbot, 1986) Salt glacier
Mining activity? N
Mining activity start
Mining activity end
Mining galleries?
Mining products
Mining sub-products
Evaporite flow? Y
Age of evaporite flow Cuisian (Salt inflation), Lutetian (piercement), Oligocene (Crestal Colapse)
Flow or deformation triggering mechanisms Contraction / Sedimentary loading and thrust stacking / anticline crest erosion / strike-parallel local extension of a salt-cored detachment fold
Flow-linked structures? Y
Halokinetic structures Progressive unconformities / Normal faults / Thickness variations
Post-evaporite and pre-kinematic unit/s (overbuden) Jurassic (carbonate breccias, marlstones, limestones) ; Upper Cretaceous (Garumn Facies, calcarenites and limestones) ; Illerdian-Middle Cuisian (limestones, marlstones, calcarenites)
Syn-kinematic unit/s Upper Cuisian(?) (Boltaña Fm., limestones) / Lutetian (Guara Fm., limestones)
Available seismic profiles SP-25 / SP-25 / SP-25 / SP-25(1) / SP-25-1 / SP-25 / SP-25 / SP-15 / SP-17 / SP-84-17 / JAT-98 / SP-25-1 / SP-5 / SP-1 / SP-25 / SP-25 / SP-17 / ND-102 / SP-17 / SP-84-17 / SP-25(1)
Available boreholes PANILLO-EJEP
Additional comments Host rocks show a unusual, reduced piercement (see Teixell and Barnolas 1995). The diapir is surrounded by a thicker overburden and a significant thickness of syntectonic deposits of the Graus–Tremp Basin. Genetically linked to the Mediano salt-cored anticline: pop-up structure evolved from the salt-cored Mediano anticline during Lutetian.

Mining Data

UNIQUE_ID 54
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 54
Outcropping area (km2) 14.97275
Horizontal intersection area (km2) (when buried) Not buried
Depth of intersection area (km2) (when buried) Not buried
Max. Width (Km) 8.35148804
Max. Length (Km) 5.05685705
Max. Evaporites thickness (km) 3
Max. Deformation age (Ma) 49
Min. Deformation age (Ma) 42
Deformation stages 1

Reference Data

UNIQUE_ID 54
Section source Santolaria, P., Casas-Sainz, A. M., Soto, R., Casas, A., 2017. Gravity modelling to assess salt tectonics in the western end of the South Pyrenean Central Unit. Journal of the Geological Society, 174(2), 269-288. [link]
Well / Borehole availability #1 Soto, R., Casas, A. M., Storti, F., & Faccenna, C. (2002). Role of lateral thickness variations on the development of oblique structures at the Western end of the South Pyrenean Central Unit. Tectonophysics, 350(3), 215-235. [link]
Well / Borehole availability #2 Santolaria, P., Casas-Sainz, A. M., Soto, R., Casas, A., 2017. Gravity modelling to assess salt tectonics in the western end of the South Pyrenean Central Unit. Journal of the Geological Society, 174(2), 269-288. [link]
Available data (Stratigraphy) #1 Soto, R., Casas, A. M., Storti, F., & Faccenna, C. (2002). Role of lateral thickness variations on the development of oblique structures at the Western end of the South Pyrenean Central Unit. Tectonophysics, 350(3), 215-235. [link]
Available data (Stratigraphy) #2 Teixell, A., Barnolas, A., 1995. Significado de la discordancia de Mediano en relación con las estructuras adyacentes (Eoceno, Pirineo Central). Geogaceta, 18, 34-37. [link]
Available data (Stratigraphy) #3 Santolaria, P., Casas-Sainz, A. M., Soto, R., Casas, A., 2017. Gravity modelling to assess salt tectonics in the western end of the South Pyrenean Central Unit. Journal of the Geological Society, 174(2), 269-288. [link]
Available data (Stratigraphy) #4 Muñoz, J. A., Beamud, E., Fernández, O., Arbués, P., Dinarès‐Turell, J., Poblet, J., 2013. The Ainsa Fold and thrust oblique zone of the central Pyrenees: Kinematics of a curved contractional system from paleomagnetic and structural data. Tectonics, 32(5), 1142-1175. [link]
Available data (Stratigraphy) #5 Serra-Kiel, J., Canudo, J. I., Dinares, J., Molina, E., Ortiz, N., Pascual, J. O., …, Tosquella, J., 1994. Cronoestratigrafía de los sedimentos marinos del Terciario inferior de la Cuenca de Graus-Tremp (Zona Central Surpirenaica). Revista de la Sociedad Geológica de España, 7(3-4), 273-297. [link]
Available data (Stratigraphy) #6 Poblet, J., Muñoz, J. A., Travé, A., Serra-Kiel, J., 1998. Quantifying the kinematics of detachment folds using three-dimensional geometry: Application to the Mediano anticline (Pyrenees, Spain). Geological Society of America Bulletin, 110(1), 111-125. [link]
Regional Stratigraphy Muñoz, J. A., Beamud, E., Fernández, O., Arbués, P., Dinarès‐Turell, J., Poblet, J., 2013. The Ainsa Fold and thrust oblique zone of the central Pyrenees: Kinematics of a curved contractional system from paleomagnetic and structural data. Tectonics, 32(5), 1142-1175. [link]
Seismic data availability #1 Santolaria, P., Casas-Sainz, A. M., Soto, R., Casas, A., 2017. Gravity modelling to assess salt tectonics in the western end of the South Pyrenean Central Unit. Journal of the Geological Society, 174(2), 269-288. [link]
Seismic data availability #2 Soto, R., Casas, A. M., Storti, F., & Faccenna, C. (2002). Role of lateral thickness variations on the development of oblique structures at the Western end of the South Pyrenean Central Unit. Tectonophysics, 350(3), 215-235. [link]
Seismic data availability #3 Muñoz, J. A., Beamud, E., Fernández, O., Arbués, P., Dinarès‐Turell, J., Poblet, J., 2013. The Ainsa Fold and thrust oblique zone of the central Pyrenees: Kinematics of a curved contractional system from paleomagnetic and structural data. Tectonics, 32(5), 1142-1175. [link]
Available data (Structure) #1 Santolaria, P., Casas-Sainz, A. M., Soto, R., Casas, A., 2017. Gravity modelling to assess salt tectonics in the western end of the South Pyrenean Central Unit. Journal of the Geological Society, 174(2), 269-288. [link]
Available data (Structure) #2 Santolaria, P., Ayala, C., Pueyo, E. L., Rubio, F. M., Soto, R., Calvín, P., …, Casas‐Sainz, A. M., 2020. Structural and geophysical characterization of the western termination of the South Pyrenean triangle zone. Tectonics, 39(8), e2019TC005891. [link]
Available data (Structure) #3 Poblet, J., Muñoz, J. A., Travé, A., Serra-Kiel, J., 1998. Quantifying the kinematics of detachment folds using three-dimensional geometry: Application to the Mediano anticline (Pyrenees, Spain). Geological Society of America Bulletin, 110(1), 111-125. [link]
Available data (Structure) #4 Soto, R., Casas, A. M., Storti, F., & Faccenna, C. (2002). Role of lateral thickness variations on the development of oblique structures at the Western end of the South Pyrenean Central Unit. Tectonophysics, 350(3), 215-235. [link]
Available data (Structure) #5 Muñoz, J. A., Beamud, E., Fernández, O., Arbués, P., Dinarès‐Turell, J., Poblet, J., 2013. The Ainsa Fold and thrust oblique zone of the central Pyrenees: Kinematics of a curved contractional system from paleomagnetic and structural data. Tectonics, 32(5), 1142-1175. [link]
Available data (Structure) #6 Santolaria, P., Mochales, T., Casas Sainz, A., Soto Marín, R., 2015. Análisis de la fracturación en una cuenca de antepaís: el caso de la Fm. Escanilla (Cuenca de Aínsa, Zona Surpirenaica). Geogaceta, 58, 87-90. [link]
Available data (Analogue modelling) #1 Bonini, M., 2003. Detachment folding, fold amplification, and diapirism in thrust wedge experiments. Tectonics, 22(6). [link]
Available data (Analogue modelling) #2 n.a.
Available data (Analogue modelling) #3 n.a.
Available data (Gravimetry – Tomography) #1 Santolaria, P., Ayala, C., Pueyo, E. L., Rubio, F. M., Soto, R., Calvín, P., …, Casas‐Sainz, A. M., 2020. Structural and geophysical characterization of the western termination of the South Pyrenean triangle zone. Tectonics, 39(8), e2019TC005891. [link]
Available data (Gravimetry – Tomography) #2 Santolaria, P., Casas-Sainz, A. M., Soto, R., Casas, A., 2017. Gravity modelling to assess salt tectonics in the western end of the South Pyrenean Central Unit. Journal of the Geological Society, 174(2), 269-288. [link]
Available data (Gravimetry – Tomography) #3 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 (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 Santolaria, P., Casas-Sainz, A. M., Soto, R., Casas, A., 2017. Gravity modelling to assess salt tectonics in the western end of the South Pyrenean Central Unit. Journal of the Geological Society, 174(2), 269-288. [link]
Available data (Petrophysics) #2 n.a.
IGME Geological Map (MAGNA50) Sheet number
Other Maps #1 (source) Muñoz, J. A., Mencos, J., Roca, E., Carrera, N., Gratacós, O., Ferrer, O., Fernández, O., 2018. The structure of the South-Central-Pyrenean fold and thrust belt as constrained by subsurface data. Geologica Acta, 16(4), 439-460. [link]
Other Maps #2 (source) Santolaria, P., Casas-Sainz, A. M., Soto, R., Casas, A., 2017. Gravity modelling to assess salt tectonics in the western end of the South Pyrenean Central Unit. Journal of the Geological Society, 174(2), 269-288. [link]
Other related references #1 Falivene, O., Arbués, P., Ledo, J., Benjumea, B., Muñoz, J. A., Fernández, O., Martínez, S., 2010. Synthetic seismic models from outcrop-derived reservoir-scale three-dimensional facies models: The Eocene Ainsa turbidite system (southern Pyrenees). AAPG bulletin, 94(3), 317-343. [link]
Other related references #2 Lanaja, J. M., R. Querol, A. Navarro, 1987. Contribución de la Exploración Petrolífera al Conocimiento de la Geología de España, pp. 1–465, Instituto Geológico y Minero de España, Madrid. [link]
Other related references #3 Muñoz, J. A., Ferrer, O., Arbués, P., Beamud, E., Roca, E., Fernandez Bellon, O., 2014: Diapir Growth by Longitudinal Extension During the Development of a Thrust Salient in a Deepwater Fold and Thrust Belt: The Ainsa Oblique Zone in the Central Pyrenees. AAPG Annual Convention & Exhibition.
Other related references #4 n.a.