Structure type | Evaporite body |
Deformed/Undeformed | Undeformed |
Geological Setting | Ebro foreland basin, Southeastern Domain |
Outcropping/buried | Outcropping |
Evaporite unit/s name | Talavera Fm., Valldeperes, Pira, Rauric and Santa Coloma Fms. |
Evaporite unit/s age | Bartonian (Paleogene), Stampian (Paleogene) |
Evaporite unit/s origin | Continental |
Classif. (Hudec and Jackson, 2009) | No diapirism |
Classif. (Jackson and Talbot, 1986) | No diapirism |
Age of evaporite flow or deformation (when deformed) | Undeformed |
Other comments | Not evaporite flow occurred but the sedimentation was coeval to Paleogene compression and development of NNW-verging folds and thrusts. Diagenetic cycle consisting of deposition of primary gypsum; transformation of this gypsum into anhydrite during burial; and anhydrite hydration into secondary gypsum during final exhumation defined by Ortí et al. (2007). Gypsiferous lithofacies are currently preserved as secondary gypsum. |
Unique ID | 119 |
Name | Montblanc-Vimbodí |
Structure type | Evaporite body |
Deformed/Undeformed | Undeformed |
Buried/Outcropping | Outcropping |
Geological setting | Ebro Basin |
Geological Regional Setting | Barberà Sector |
Evaporite unit/s name | Valledeperes Fm. (Vilaverd gypsum and Lilla gypsum) / Pira Fm. (La Guàrdia gypsum, Pira Gypsum, Els Prats Gypsum and Sarral Gypsum) / Rauric Fm. (Rocafort Gypsum) / Santa Coloma Fm. (Aguiló Gypsum) / Talavera Fm. (Talavera Gypsum) |
Evaporite unit/s age | Bartonian-Stampian (Paleogene) |
Evaporite unit/s era | Cenozoic |
Evaporite unit/s origin | Continental (lacustrine) |
Evaporite unit/s composition | Gypsum / Claystonestone / Marlstone / Gypsarenites / Anhydrite / Sandstone |
Post-kinematic unit/s (or post-evaporite units when evaporites are undeformed) | Upper Miocene (conglomerates and red claystones) ; Quaternary (alluvial and colluvial detrital deposits) |
Post-kinematic unit/s age (or post-evaporite units when evaporites are undeformed) | Upper Miocene-Holocene |
Classification (Hudec and Jackson, 2009) | No diapirism |
Classification (Jackson and Talbot, 1986) | No diapirism |
Mining activity? | N |
Mining activity start | |
Mining activity end | |
Mining galleries? | |
Mining products | |
Mining sub-products | |
Evaporite flow? | N |
Age of evaporite flow | – |
Flow or deformation triggering mechanisms | – |
Flow-linked structures? | – |
Halokinetic structures | – |
Post-evaporite and pre-kinematic unit/s (overbuden) | – |
Syn-kinematic unit/s | – |
Available seismic profiles | |
Available boreholes | HOMBRIO DE LA MARCA-1 / MOMBRIO DE LA MARCA-1 / MONTBLANC-1 |
Additional comments | Not evaporite flow occurred but the sedimentation was coeval to Paleogene compression and development of NNW-verging folds and thrusts. Diagenetic cycle consisting of deposition of primary gypsum; transformation of this gypsum into anhydrite during burial; and anhydrite hydration into secondary gypsum during final exhumation defined by Ortí et al. (2007). Gypsiferous lithofacies are currently preserved as secondary gypsum. |
UNIQUE_ID | 119 |
Minning exploitations within <2km? | N |
Historical/Active | |
Exploitation name #1 | |
Exploitation ID (Spanish National Mining Cadastre) #1 | |
Municipality #1 | |
Province #1 | |
Company #1 | |
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Main minning Products #3 |
UNIQUE_ID | 119 |
Outcropping area (km2) | 43.83918 |
Horizontal intersection area (km2) (when buried) | Not buried |
Depth of intersection area (km2) (when buried) | Not buried |
Max. Width (Km) | 25.3666462 |
Max. Length (Km) | 5.61570157 |
Max. Evaporites thickness (km) | 0.6 |
Max. Deformation age (Ma) | – |
Min. Deformation age (Ma) | – |
Deformation stages | 0 |
UNIQUE_ID | 119 |
Section source | IGME MAGNA 50. SHEET 418 (MONTBLANCH) |
Well / Borehole availability #1 | n.a. |
Well / Borehole availability #2 | n.a. |
Available data (Stratigraphy) #1 | Ortí, F., Rosell, L., Ingles, M., Playa, E., 2007. Depositional models of lacustrine evaporites in the SE margin of the Ebro Basin (Paleogene, NE Spain). Geologica Acta: an international earth science journal, 5(1), 19-34. [link] |
Available data (Stratigraphy) #2 | Sanjuan, J., Martín-Closas, C., Costa, E., Barberà, X., Garcés, M., 2014. Calibration of Eocene-Oligocene charophyte biozones in the Eastern Ebro Basin (Catalonia, Spain). Stratigraphy, 11(1), 61-81. [link] |
Available data (Stratigraphy) #3 | Colldeforns, B., Anadón, P., Cabrera, L., 1994. Nuevos datos sobre la litoestratigrafía del Eoceno-Oligoceno inferior de la zona suroriental de la Cuenca del Ebro (sector de Pontils-Montblanc, provincias de Tarragona y Barcelona). Geogaceta, 16, 98-101. [link] |
Available data (Stratigraphy) #4 | Colldeforns, B., Anadón, P., Cabrera, L., 1994. Litoestratigrafía del Eoceno superior-Oligoceno inferior de la zona oriental de la cuenca del Ebro. Sector de Igualada-Santa Coloma de Queralt. Geogaceta, 15, 55-58. [link] |
Available data (Stratigraphy) #5 | Colombo, F., 1986. Estratigrafía y Sedimentología del borde meridional occidental de los Catalánides (prov. de Tarragona, España). Cuadernos de geología ibérica, 10, 55-116. [link] |
Available data (Stratigraphy) #6 | Costa, E., Garces, M., López‐Blanco, M., Beamud, E., Gómez‐Paccard, M., Larrasoaña, J. C., 2010. Closing and continentalization of the South Pyrenean foreland basin (NE Spain): magnetochronological constraints. Basin Research, 22(6), 904-917. [link] |
Regional Stratigraphy | Ortí, F., Rosell, L., Ingles, M., Playa, E., 2007. Depositional models of lacustrine evaporites in the SE margin of the Ebro Basin (Paleogene, NE Spain). Geologica Acta: an international earth science journal, 5(1), 19-34. [link] |
Seismic data availability #1 | n.a. |
Seismic data availability #2 | n.a. |
Seismic data availability #3 | n.a. |
Available data (Structure) #1 | Vergés, J., Marzo, M., Santaeulària, T., Serra-Kiel, J., Burbank, D. W., Muñoz, J. A., Giménez-Montsant, J., 1998. Quantified vertical motions and tectonic evolution of the SE Pyrenean foreland basin. Geological Society, London, Special Publications, 134(1), 107-134. [link] |
Available data (Structure) #2 | Anadón, P., Cabrera, L., GuimerÀ, J. and Santanach, P., 1985. Paleogene strike-slip deformation and sedimentation along the southeastern margin of the Ebro basin. In: K. T. Biddle and N. Christie-Blick (Editors), Strike-Slip Deformation, Basin Formation and Sedimentation. Soc. Econ. Palaeontol. Mineral. Spec. Publ., 37: 303-318. [link] |
Available data (Structure) #3 | Anadón, P., Cabrera, L., Colombo, F., Marzo, M. y Riba, O., 1986. Syntectonic intradeforrnational unconformities in alluvial fan deposits, Eastern Ebro Basin margins (NE Spain). In Ph. Allen and P. Hornewood (eds.): Foreland basins. Spec. Publ. I.A.S., 8: 33-45. [link] |
Available data (Structure) #4 | n.a. |
Available data (Structure) #5 | n.a. |
Available data (Structure) #6 | n.a. |
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 | Guinea, A., Playà, E., Rivero, L., Himi, M., 2010. Electrical resistivity tomography and induced polarization techniques applied to the identification of gypsum rocks. Near Surface Geophysics, 8(3), 249-257. [link] |
Available data (Gravimetry – Tomography) #2 | 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) #3 | n.a. |
Available data (Geochemistry) #1 | n.a. |
Available data (Geochemistry) #2 | n.a. |
Available data (Geochemistry) #3 | n.a. |
Available data (Geochemistry) #4 | n.a. |
Available data (Petrophysics) #1 | Costa, E., 2011. Paleogene Chronostratigraphy of the SE Margin of the Ebro Basin: Biochronological and Tectonosedimentary Evolution Implications [Ph.D. thesis]: Universitat de Barcelona, 271p. [link] |
Available data (Petrophysics) #2 | Costa, E., Garces, M., López‐Blanco, M., Beamud, E., Gómez‐Paccard, M., Larrasoaña, J. C., 2010. Closing and continentalization of the South Pyrenean foreland basin (NE Spain): magnetochronological constraints. Basin Research, 22(6), 904-917. [link] |
IGME Geological Map (MAGNA50) Sheet number | 418-Montclanch. [link] |
Other Maps #1 (source) | Guimerà, J. J., 2018. Structure of an intraplate fold-and-thrust belt: The Iberian Chain. A synthesis. Geologica Acta, 16(4), 427-438. [link] |
Other Maps #2 (source) | Ortí, F., Rosell, L., Ingles, M., Playa, E., 2007. Depositional models of lacustrine evaporites in the SE margin of the Ebro Basin (Paleogene, NE Spain). Geologica Acta, 5(1), 19-34. [link] |
Other related references #1 | Barberà, X., 1990. Magnetostratigrafia de l’oligocé del sector sud-orietnal de la conca de l’ebre implicacions magnetobiocronólogiques i següencials [Ph.D. thesis]: Universitat de Barcelona, 247p. [link] |
Other related references #2 | Colombo, F., 1980. Estratigrafía y sedimentología del Terciario Inferior continental de los Catalánides [Ph.D. thesis]: Universitat de Barcelona, 116p. [link] |
Other related references #3 | Costa, E., 2011. Paleogene Chronostratigraphy of the SE Margin of the Ebro Basin: Biochronological and Tectonosedimentary Evolution Implications [Ph.D. thesis]: Universitat de Barcelona, 271p. [link] |
Other related references #4 | n.a. |
UNIQUE_ID | 119 |
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Borehole name #1 | HOMBRIO DE LA MARCA-1 |
Company #1 | TRAGSA |
Traget #1 | HYDROGEOLOGY |
Across structure? #1 | N (within 5 km) |
Borehole name #2 | MOMBRIO DE LA MARCA-1 |
Company #2 | TRAGSA |
Traget #2 | HYDROGEOLOGY |
Across structure? #2 | N (within 5 km) |
Borehole name #3 | MONTBLANC-1 |
Company #3 | TRAGSA |
Traget #3 | HYDROGEOLOGY |
Across structure? #3 | N (within 5 km) |
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UNIQUE_ID | 119 |
X Centroid (Structure shape) | 1.196125 |
Y Centroid (Structure shape) | 1.196125 |
Xmin (Structure shape) | 1.063899 |
Xmax (Structure shape) | 1.329697 |
Ymin (Structure shape) | 41.384749 |
Ymax (Structure shape) | 41.503498 |
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X borehole #1 | 1.299676 |
Y borehole #1 | 41.447086 |
X borehole #2 | 1.299676 |
Y borehole #2 | 41.447086 |
X borehole #3 | 1.177457 |
Y borehole #3 | 41.370196 |
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