Structure type | Evaporite Diapir |
Deformed/Undeformed | Deformed |
Geological Setting | Betic system, Pre-Betic cordillera |
Outcropping/buried | Outcropping |
Evaporite unit/s name | Jarafuel, Manuel, Cofrentes, Quesa, Ayora and Imón Fms. |
Evaporite unit/s age | Carnian-Rhaetian (Upper Triassic) |
Evaporite unit/s origin | Marine |
Classif. (Hudec and Jackson, 2009) | Passive piercement |
Classif. (Jackson and Talbot, 1986) | Salt wall |
Age of evaporite flow or deformation (when deformed) | Lower-Middle Pleistocene, Miocene |
Other comments | Bicorp-Quesa, Navarrés and Sellent salt wall segments constitute a continuous kinked salt wall of Middle to Upper Triassic evaporites, that crosses the central part of the Valencian domain. Salt wall development was preceded by a contractional deformation that folded and thrusted the Middle-Upper Triassic successions. Quaternary diapirism in the region (proposed by Gutiérrez et al., 2019) is enhanced by erosional unloading related to fluvial entrenchment |
Unique ID | 50 |
Name | Navarrés |
Structure type | Evaporite diapir |
Deformed/Undeformed | Deformed |
Buried/Outcropping | Outcropping |
Geological setting | Betic System |
Geological Regional Setting | Pre-Betic Cordillera (Valencian domain) |
Evaporite unit/s name | Jarafuel, Manuel, Cofrentes, Quesa, Ayora and Imón Fms. |
Evaporite unit/s age | Carnian-Rhaetian (Upper Triassic) |
Evaporite unit/s era | Mesozoic |
Evaporite unit/s origin | Marine |
Evaporite unit/s composition | Gypsum-Mudstone-Dolostone-Sandstone |
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) | Holocene |
Classification (Hudec and Jackson, 2009) | Passive piercement |
Classification (Jackson and Talbot, 1986) | Salt wall |
Mining activity? | Y |
Mining activity start | – |
Mining activity end | – |
Mining galleries? | – |
Mining products | Limestone (other uses) |
Mining sub-products | – |
Evaporite flow? | Y |
Age of evaporite flow | Miocene (main stage) and Quaternary (late stage?) |
Flow or deformation triggering mechanisms | Late Miocene thin-skinned extensional fault system |
Flow-linked structures? | Y |
Halokinetic structures | Normal high-angle faults / joints / thickness variations / progressive unconformities |
Post-evaporite and pre-kinematic unit/s (overbuden) | Jurassic (anhydrite, calcarenite, dolostones, marly limestones) ; Early Cretaceous (sandstones, dolostones, calcarenites) ; Late Cretaceous (sandstones, dolostones, marly dolostones, limestones) |
Syn-kinematic unit/s | Miocene (red and grey mudstones, sandstones, limestones, conglomerates), Quaternary (fluvial and alluvial deposits) |
Available seismic profiles | |
Available boreholes | ABRULLADOR / BARRANCO BONO / BARRANCO PELOTERO / MONTECARLO / MONTESA-6 (VIÑET) / MONTESA-7 (ALQUERIES) / MONTESA-1 / MONTESA-5 (HONDO EL FIGUERAL) / CALDERON / BANCAL ROJO / CAMINO DEL PINAR / CALDERON-II / CARRASCAL / CARRASCAL (ALGUARIA) / PEDRERA-2 |
Additional comments | Bicorp-Quesa, Navarrés and Sellent salt wall segments constitute a continuous kinked salt wall of Middle to Upper Triassic evaporites, that crosses the central part of the Valencian domain. Salt wall development was preceded by a contractional deformation that folded and thrusted the Middle-Upper Triassic successions. Quaternary diapirism in the region (proposed by Gutiérrez et al., 2019) is enhanced by erosional unloading related to fluvial entrenchment |
UNIQUE_ID | 50 |
Minning exploitations within <2km? | Y |
Historical/Active | Active |
Exploitation name #1 | TOSSAL NEGRE |
Exploitation ID (Spanish National Mining Cadastre) #1 | 855 |
Municipality #1 | Sellent |
Province #1 | VALENCIA |
Company #1 | AGLOMERADOS LOS SERRANOS S.A |
Main minning Products #1 | Limestone (other uses) |
Exploitation name #2 | |
Exploitation ID (Spanish National Mining Cadastre) #2 | |
Municipality #2 | |
Province #2 | |
Company #2 | |
Main minning Products #2 | |
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Exploitation ID (Spanish National Mining Cadastre) #3 | |
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Company #3 | |
Main minning Products #3 |
UNIQUE_ID | 50 |
Outcropping area (km2) | 16.70358 |
Horizontal intersection area (km2) (when buried) | Not buried |
Depth of intersection area (km2) (when buried) | Not buried |
Max. Width (Km) | 5.17317777 |
Max. Length (Km) | 9.52428639 |
Max. Evaporites thickness (km) | 1.1 |
Max. Deformation age (Ma) | 23 |
Min. Deformation age (Ma) | Active? |
Deformation stages | 2 |
UNIQUE_ID | 50 |
Section source | Gutiérrez, F., Sevil, J., Silva, P. G., Roca, E., Escosa, F., 2019. Geomorphic and stratigraphic evidence of Quaternary diapiric activity enhanced by fluvial incision. Navarrés salt wall and graben system, SE Spain. Geomorphology, 342, 176-195. [link] |
Well / Borehole availability #1 | Pérez-López, A., Solé de Porta, N., Ortí, F., 1996. Facies carbonato-evaporiticas del Trías superior y tránsito al Líás en el Levante espanol: nuevas precisiones estratigráficas. Cuadernos de geología ibérica, 20, 245-270. [link] |
Well / Borehole availability #2 | n.a. |
Available data (Stratigraphy) #1 | Roca, E., Beamud, E., Rubinat, M., Soto, R., Ferrer, O., 2013. Paleomagnetic and inner diapiric structural constraints on the kinematic evolution of a salt-wall: The Bicorb-Quesa and northern Navarrés salt-wall segments case (Prebetic Zone, SE Iberia). Journal of Structural Geology, 52, 80-95. [link] |
Available data (Stratigraphy) #2 | Gutiérrez, F., Sevil, J., Silva, P. G., Roca, E., Escosa, F., 2019. Geomorphic and stratigraphic evidence of Quaternary diapiric activity enhanced by fluvial incision. Navarrés salt wall and graben system, SE Spain. Geomorphology, 342, 176-195. [link] |
Available data (Stratigraphy) #3 | Castaño-Fernández, S., Carbó-Gorosabel, A., 1995. Los afloramientos triásicos de la zona de confluencia de las Cordilleras Ibérica y Bética. Aportes de la gravimetría a su interpretación. Cuadernos de geología ibérica, (19), 235-248. [link] |
Available data (Stratigraphy) #4 | Rubinat-Cabanas, M., 2012. Basement fault influence on the Bicorb-Quesa Salt Wall kinematics, insights from Magnetotelluric and Paleomagnetic techniques on Salt Tectonics [Ph.D. thesis]: Universitat de Barcelona, Barcelona, 169pp. [link] |
Available data (Stratigraphy) #5 | Santisteban, C., Ruíz-Sánchez, F., Bello, D., 1989. Los depósitos lacustres del Terciario de Bicorp (Valencia). Acta geológica hispánica, 24(3), 299-307. [link] |
Available data (Stratigraphy) #6 | Ortí, F., Pérez-López, A., Salvany, J. M., 2017. Triassic evaporites of Iberia: Sedimentological and palaeogeographical implications for the western Neotethys evolution during the Middle Triassic–Earliest Jurassic. Palaeogeography, palaeoclimatology, palaeoecology, 471, 157-180. [link] |
Regional Stratigraphy | IGME MAGNA50 SHEET (769-Navarrés). [link] |
Seismic data availability #1 | n.a. |
Seismic data availability #2 | n.a. |
Seismic data availability #3 | n.a. |
Available data (Structure) #1 | Rubinat-Cabanas, M., 2012. Basement fault influence on the Bicorb-Quesa Salt Wall kinematics, insights from Magnetotelluric and Paleomagnetic techniques on Salt Tectonics [Ph.D. thesis]: Universitat de Barcelona, Barcelona, 169pp. [link] |
Available data (Structure) #2 | Roca, E., Beamud, E., Rubinat, M., Soto, R., Ferrer, O., 2013. Paleomagnetic and inner diapiric structural constraints on the kinematic evolution of a salt-wall: The Bicorb-Quesa and northern Navarrés salt-wall segments case (Prebetic Zone, SE Iberia). Journal of Structural Geology, 52, 80-95. [link] |
Available data (Structure) #3 | Gutiérrez, F., Sevil, J., Silva, P. G., Roca, E., Escosa, F., 2019. Geomorphic and stratigraphic evidence of Quaternary diapiric activity enhanced by fluvial incision. Navarrés salt wall and graben system, SE Spain. Geomorphology, 342, 176-195. [link] |
Available data (Structure) #4 | Arche, A., López-Gómez, J., García-Hidalgo, J. F., 2002. Control climático, tectónico y eustático en depósitos del Carniense (Triásico Superior) del SE de la Península Ibérica. Journal of Iberian Geology, 28, 13-30. [link] |
Available data (Structure) #5 | Roca, E., Sans, M., Koyi, H. A., 2006. Polyphase deformation of diapiric areas in models and in the eastern Prebetics (Spain). AAPG bulletin, 90(1), 115-136. [link] |
Available data (Structure) #6 | Soto, R., Beamud, E., Oliva-Urcia, B., Roca, E., Rubinat, M., Villalaín, J. J., 2014. Applicability of magnetic fabrics in rocks associated with the emplacement of salt structures (the Bicorb–Quesa and Navarrés salt walls, Prebetics, SE Spain). Tectonophysics, 629, 319-334. [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 | Castaño-Fernández, S., Carbó-Gorosabel, A., 1995. Los afloramientos triásicos de la zona de confluencia de las Cordilleras Ibérica y Bética. Aportes de la gravimetría a su interpretación. Cuadernos de geología ibérica, (19), 235-248. [link] |
Available data (Gravimetry – Tomography) #2 | Rubinat-Cabanas, M., 2012. Basement fault influence on the Bicorb-Quesa Salt Wall kinematics, insights from Magnetotelluric and Paleomagnetic techniques on Salt Tectonics [Ph.D. thesis]: Universitat de Barcelona, Barcelona, 169pp. [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 | Cuairán, J. B., Inglès, M., Cabo, F. O., 1987. Observaciones sobre mineralogía y geoquímica de lutitas del Keuper de Valencia. Cuadernos de Geología Ibérica, 11, 363-384. [link] |
Available data (Geochemistry) #2 | 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) #3 | n.a. |
Available data (Geochemistry) #4 | n.a. |
Available data (Petrophysics) #1 | Roca, E., Beamud, E., Rubinat, M., Soto, R., Ferrer, O., 2013. Paleomagnetic and inner diapiric structural constraints on the kinematic evolution of a salt-wall: The Bicorb-Quesa and northern Navarrés salt-wall segments case (Prebetic Zone, SE Iberia). Journal of Structural Geology, 52, 80-95. [link] |
Available data (Petrophysics) #2 | Soto, R., Beamud, E., Oliva-Urcia, B., Roca, E., Rubinat, M., Villalaín, J. J., 2014. Applicability of magnetic fabrics in rocks associated with the emplacement of salt structures (the Bicorb–Quesa and Navarrés salt walls, Prebetics, SE Spain). Tectonophysics, 629, 319-334. [link] |
IGME Geological Map (MAGNA50) Sheet number | 769-Navarres. [link] |
Other Maps #1 (source) | Escosa, F. O., Ferrer, O., Roca, E., 2018. Geology of the Eastern Prebetic Zone at the Jumilla region (SE Iberia). Journal of Maps, 14(2), 77-86. [link] |
Other Maps #2 (source) | Rubinat-Cabanas, M., 2012. Basement fault influence on the Bicorb-Quesa Salt Wall kinematics, insights from Magnetotelluric and Paleomagnetic techniques on Salt Tectonics [Ph.D. thesis]: Universitat de Barcelona, Barcelona, 169pp. [link] |
Other related references #1 | Arche, A., López-Gómez, J., García-Hidalgo, J. F., 2002. Control climático, tectónico y eustático en depósitos del Carniense (Triásico Superior) del SE de la Península Ibérica. Journal of Iberian Geology, 28, 13-30. [link] |
Other related references #2 | Santisteban, C., Ruíz-Sánchez, F., Bello, D., 1989. Los depósitos lacustres del Terciario de Bicorp (Valencia). Acta geológica hispánica, 24(3), 299-307. [link] |
Other related references #3 | Ortí-Cabo, F., 1974. El Keuper del Levante español. Estudios Geológicos, 30. [link] |
Other related references #4 | del Olmo, W. M., Motis, K., Martín, D., 2015. El papel del diapirismo de la sal Triásica en la estructuración del Prebético (SE de España). Revista de la Sociedad Geológica de España, 28(1), 3-24. [link] |
UNIQUE_ID | 50 |
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Borehole name #1 | ABRULLADOR |
Company #1 | TRAGSA |
Traget #1 | HYDROGEOLOGY |
Across structure? #1 | N (within 5 km) |
Borehole name #2 | BARRANCO BONO |
Company #2 | TRAGSA |
Traget #2 | HYDROGEOLOGY |
Across structure? #2 | N (within 5 km) |
Borehole name #3 | BARRANCO PELOTERO |
Company #3 | TRAGSA |
Traget #3 | HYDROGEOLOGY |
Across structure? #3 | N (within 5 km) |
Borehole name #4 | MONTECARLO |
Company #4 | TRAGSA |
Traget #4 | HYDROGEOLOGY |
Across structure? #4 | N (within 5 km) |
Borehole name #5 | MONTESA-6 (VIÑET) |
Company #5 | TRAGSA |
Traget #5 | HYDROGEOLOGY |
Across structure? #5 | N (within 5 km) |
Borehole name #6 | MONTESA-7 (ALQUERIES) |
Company #6 | TRAGSA |
Traget #6 | HYDROGEOLOGY |
Across structure? #6 | N (within 5 km) |
Borehole name #7 | MONTESA-1 |
Company #7 | TRAGSA |
Traget #7 | HYDROGEOLOGY |
Across structure? #7 | N (within 5 km) |
Borehole name #8 | MONTESA-5 (HONDO EL FIGUERAL) |
Company #8 | TRAGSA |
Traget #8 | HYDROGEOLOGY |
Across structure? #8 | N (within 5 km) |
Borehole name #9 | CALDERON |
Company #9 | TRAGSA |
Traget #9 | HYDROGEOLOGY |
Across structure? #9 | N (within 5 km) |
Borehole name #10 | BANCAL ROJO |
Company #10 | TRAGSA |
Traget #10 | HYDROGEOLOGY |
Across structure? #10 | N (within 5 km) |
Borehole name #11 | CAMINO DEL PINAR |
Company #11 | TRAGSA |
Traget #11 | HYDROGEOLOGY |
Across structure? #11 | N (within 5 km) |
Borehole name #12 | CALDERON-II |
Company #12 | TRAGSA |
Traget #12 | HYDROGEOLOGY |
Across structure? #12 | N (within 5 km) |
Borehole name #13 | CARRASCAL |
Company #13 | TRAGSA |
Traget #13 | HYDROGEOLOGY |
Across structure? #13 | N (within 5 km) |
Borehole name #14 | CARRASCAL (ALGUARIA) |
Company #14 | TRAGSA |
Traget #14 | HYDROGEOLOGY |
Across structure? #14 | N (within 5 km) |
Borehole name #15 | PEDRERA-2 |
Company #15 | TRAGSA |
Traget #15 | HYDROGEOLOGY |
Across structure? #15 | N (within 5 km) |
UNIQUE_ID | 50 |
X Centroid (Structure shape) | -0.627690 |
Y Centroid (Structure shape) | -0.627690 |
Xmin (Structure shape) | -0.667772 |
Xmax (Structure shape) | -0.585789 |
Ymin (Structure shape) | 38.994168 |
Ymax (Structure shape) | 39.067941 |
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X borehole #1 | -0.676250 |
Y borehole #1 | 39.045541 |
X borehole #2 | -0.589088 |
Y borehole #2 | 39.046924 |
X borehole #3 | -0.707672 |
Y borehole #3 | 39.092113 |
X borehole #4 | -0.617655 |
Y borehole #4 | 39.087307 |
X borehole #5 | -0.622375 |
Y borehole #5 | 38.961745 |
X borehole #6 | -0.640150 |
Y borehole #6 | 38.959583 |
X borehole #7 | -0.639322 |
Y borehole #7 | 38.955332 |
X borehole #8 | -0.617378 |
Y borehole #8 | 38.966238 |
X borehole #9 | -0.678056 |
Y borehole #9 | 39.043324 |
X borehole #10 | -0.713410 |
Y borehole #10 | 39.075557 |
X borehole #11 | -0.560243 |
Y borehole #11 | 39.051468 |
X borehole #12 | -0.676887 |
Y borehole #12 | 39.043752 |
X borehole #13 | -0.637657 |
Y borehole #13 | 38.963407 |
X borehole #14 | -0.639598 |
Y borehole #14 | 38.962636 |
X borehole #15 | -0.578212 |
Y borehole #15 | 39.063592 |