Dyke or pipe? Contributions of magnetic fabrics to the reconstruction of the geometry of an eroded subvolcanic body (Cadí basin, Pyrenees)

The reconstruction of the geometry of igneous bodies in inverted basins is often a difficult task, because most of their volume can be either below or above the topographic surface. Indirect methods, such as the determination of their internal fabric can give clues to constrain geometrical reconstructions. The Sant Salvador intrusion, located in the Late Carboniferous-Permian Cadí basin (Central-Eastern Pyrenees), is a good example for testing the application of magnetic fabrics to shallow igneous bodies because of (i) its characteristics in terms of crystal composition/orientation, showing a homogeneous petrofabric controlled by plagioclase crystals 0.4 mm in size, (ii) its good, though partial, preservation, (iii) its position in the stratigraphical succession, between volcaniclastic sediments and unconformably overlying red beds, and (iv) the many unknown factors related to the intrusion, including the geometry of the body and its depth and the amount of erosion after intrusion. Furthermore, the Sant Salvador intrusion provides opportunity for checking the correspondence between the petrofabric and the magnetic fabrics when the magnetic carriers of susceptibility (with an average value of 5217·10−6 SI) are mainly ferromagnetic. In this case the main magnetic carriers are magnetite and also hematite, the latter resulting from oxidation processes at the paleosurface. The results of Anisotropy of Magnetic Susceptibility show a bimodality in the K1 disposition after bedding restitution: vertical in the deeper areas of the intrusion and subhorizontal, E-W, in the uppermost stratigraphic positions with an intermediate necking zone in which transition from vertical to horizontal flow is interpreted to occur. Bands deflecting the mineral foliation at the micro scale have also a tectonic or thermal origin but do not seem to interfere with the magnetic ellipsoid axes. Columnar jointing is interpreted to be parallel to the long axis of the intrusion (and therefore to magma flow, and perpendicular to the paleosurface. All these features indicate that the Sant Salvador intrusion can be interpreted as a subvertical pipe feeding a sill that was eroded before the sedimentation of the overlying red beds

Diachronous folding and cleavage in an intraplate setting (Central High Atlas, Morocco) determined through the study of remagnetizations

Remagnetizations are common in intraplate basins. When remagnetizations occur at an intermediate stage between different tectonic processes, they can be used for paleo-geometrical reconstructions and relative dating of different structures. This has a particular interest in geological frameworks where other geological time markers are absent. In order to apply this methodology, it is necessary to calculate the regional remagnetization direction and subsequently to use this reference direction to restore the attitude of the beds at the moment of remagnetization acquisition. In this work, we use this methodology for dating a pervasive cleavage (whose time of formation is controversial) and the associated structures in the Central High Atlas (Morocco). Paleomagnetic directions from 64 sites were used to calculate the remagnetization direction (D = 330.9°, I = 35.1°, A/n = 6.107) which is coincident with the Albian-Cenomanian (ca. 100 M.a.) expected direction for NW Africa. This direction was used to restore the Mesozoic paleo-geometry of beds allowing us to analyze bedding orientation, cleavage and folding relationships between the present day and the Cretaceous geometry. After restoration we conclude that the development of cleavage post-dates remagnetization, being in relation with Cenozoic basin inversion. However, the paleo-geometry shows incipient folds at Cretaceous times, which can be related to an intra-Mesozoic compressional event

Unraveling Multiple Thermotectonic Events Accommodated by Crustal\u2010Scale Faults in Northern Iberia, Spain: Insights From K-Ar Dating of Clay Gouges

Large-scale faults in the continental crust are significant features that control the evolution of sedimentary basins and intraplate mountain chains. Deciphering their evolution is a significant task because faults slip and reactivate in a variety of geological settings. In this work, clay gouges of two major orogen-scale, long-lived faults in northern Iberia, the Río Grío and Vallès-Penedès Faults, were investigated by X-ray diffraction and K-Ar isotopic analysis. Illite polytype determinations of 44 subfractions (from <0.1 to 10 Œºm) allowed us to discriminate between authigenic/synkinematic illite crystals formed during faulting and detrital illite crystals inherited from the host rock. K-Ar dating provided a detailed set of ages corresponding to key stages of the thermotectonic evolution of the Iberian Plate: (a) the Permian to Late Triassic extensional/transtensional activity associated to the emplacement of Late Variscan magmatic bodies and hydrothermal mineralizations, (b) the opening of the Central Atlantic Rift during Late Triassic-Early Jurassic times, (c) the Late Jurassic-Early Cretaceous rifting that led to the development of Mesozoic extensional/transtensional basins in northern Iberia, (d) the final stage of the anticlockwise rotation of the Iberian Plate with respect to Eurasia and the accommodation of the first Pyrenean compressional pulses in Campanian time, and (e) the positive inversion of Mesozoic extensional basins due to far-field stresses associated with the Alpine orogeny during the Paleogene. The results highlight that thermotectonic conditions characterized by high-geothermal gradients strongly favor fault movement and neoformation of clay minerals in fault gouges, regardless of the prevailing tectonic regime

Internal characterization of embankment dams using ground penetrating radar (GPR) and thermographic analysis: A case study of the Medau Zirimilis Dam (Sardinia, Italy)

The stability of embankment dams without an impermeable core depends on the characteristics of the face slab that prevents internal erosion, piping and eventual collapse of the structure. Under a Mediterranean climate, the impermeable asphaltic face slab is subjected to high solar radiation and consequent temperature changes, which can generate the creation of cracks and joints. The Medau Zirimilis Dam, located in the Casteddu River (Sardinia), is an embankment dam that has undergone seepage and continuous repairs in its asphalt face slab. These reparations have been conducted because of the occurrence of cracks and relative movement of different segments of the slab. To evaluate if seepage endangers the integrity of the dam, GPR was used, with different antennas (100, 250 and 500 MHz), along its crest and upstream and downstream faces, and the data were integrated with infrared thermographic images. Although geophysical data do not show structural changes affecting the main dam structure, deformation structures at shallow levels and in particular in the upstream face and along the crest of the dam have been identified. Such deformation affects the road atop the crest, the face slab and underlying levels, resulting in landslides that include material from several meters below the surface. The analysis permitted the identification of the origin of surficial cracks and their effects on the face slab. These sectors, independent of current movement, define the most unstable areas against water level changes that can affect the dam integrity. GPR analysis at the embankments usually has the handicap of high clay content that precludes electromagnetic wave penetration; however, in this case, the obtained resolution and extent of penetration using the different antennas was sufficient, due to the absence of an inner waterproof unit, and permitted the evaluation of the inner structure of the dam and the application of GPR for construction quality surveillance, internal structural characterization and dam monitoring

La presa de Enciso. Certificado de defunción para el valle del Cidacos

El proyecto de presa de Enciso en el valle del Cidacos es ya una realidad: 100 metros de pared de hormigo´n (94 metros desde el cauce, 105 metros sobre cimientos) que se alzan amenazadores sobre Enciso para retener 37 Hm3 (tres cuartas partes del volumen anual del ri´o). Lejos de aportar soluciones para el desarrollo del alto Cidacos, la presa, tal como esta´ disen~ada, constituye un grave riesgo y una hipoteca para el futuro de todas las poblaciones situadas entre Yanguas y Arnedo. En este arti´culo se ex- ponen los riesgos asociados a la construccio´n y llenado de la presa de Enciso, cuyas consecuencias afectara´n a la calidad, estilo de vida y futuro de las gentes que vivan aguas abajo de la misma

Evaluación multidisciplinar 3D de una estructura kárstica asociada a colapso y subsidencia (Cuenca del Ebro)

La propagación de cavidades de disolución localizadas por debajo de series aluviales genera una serie de evidencias cuya representación superficial, en ocasiones, puede no ser indicativa de su extensión real en profundidad. La propagación de cavidades a través de medios heterogéneos, en los que pueden existir niveles cementados, puede producir cambios en la progresión de dichas cavidades y la identificación en superficie de grietas, colapsos, o zonas de subsidencia que pueden involucrar decenas de miles de metros cúbicos de material inestable. Cualquier tipo de evaluación de soluciones mitigadoras en estos contextos debe considerar la amplitud de estos volúmenes y el origen del proceso con independencia de la actividad registrada en superficie. En este trabajo se aborda un estudio integrado con el objetivo de determinar la estructura de un sector con evidencias de actividad kárstica superficial y evaluar su extensión y desarrollo tridimensional integrando el análisis geomorfológico, de inspección de campo, geofísica (GPR) y sondeos. The propagation of solution cavities located below alluvial deposits produce surficial evidences that, in some cases, cannot be representative of their actual extension at depth. Cavity propagation through heterogeneous media, for example with interbedded cemented levels, can produce changes in the propagation of deformation producing the identification of cracks, collapses or subsidence zones at the surface. These processes can involve thousands of cubic meters of unstable materials. Any evaluation of mitigation tasks, in this context, needs to consider: i) the amplitude of the affected volumes and ii) the in depth origin with independence of the surficial recorded activity In this work an integrated analysis is developed to evaluate the size and 3D structure of a sector with surficial evidences of karstic activity integrating geomorphological analysis, field inspection, geophysics (GPR) and boreholes

Basement-Cover Relationships and Their Along-Strike Changes in the Linking Zone (Iberian Range, Spain): A Combined Structural and Gravimetric Study

Contractional deformation in the transition between the Iberian and Catalan Coastal Ranges (Linking Zone) generated both thin-skinned structures detached in low-strength Triassic units and basement-involved structures. To evaluate their extent and relative contribution to the overall structure, we carried out a study combining structural geology and gravimetry. New gravity data (938 stations) and density determinations (827 samples) were acquired and combined with previous existing databases to obtain Bouguer anomaly and residual Bouguer anomaly maps of the study area. Seven serial and balanced cross sections were built, their depth geometries being constrained through the 2.5-D gravity modeling and the 3-D gravity inversion that we accomplished. The residual Bouguer anomaly map shows a good correlation between basement antiforms and gravity highs whereas negative anomalies mostly correspond to (i) Meso-Cenozoic synclines and (ii) Neogene-Quaternary basins. Cross sections depict a southern, thick-skinned domain where extensional, basement faults inherited from Late Jurassic-Early Cretaceous times were inverted during the Cenozoic. To the north, we interpret the existence of both Triassic-detached and basement-involved deformation domains. The two deformation styles are vertically overlapped in the southernmost part of the Catalan Coastal Ranges but relay both across and along strike in the Eastern Iberian Range. These basement and cover relationships and their along-strike variations are analyzed in terms of the interplay between structural inheritance, its obliquity to the shortening direction, and the continuity and effectiveness of Triassic décollements in the study area

El embalse de Mularroya (Zaragoza): problemas geológicos de una obra en avanzado estado de construcción.

El embalse de Mularroya (más de 100 hm3 de capacidad), situado sobre el cauce del río Grío, uno de los afluentes del Jalón (afluente a su vez del Ebro por su margen derecha) es una obra en avanzado estado de construcción. Desde la fase de estudios previos (mediados de los años 90) hasta la actualidad, se han constatado problemas geológicos que ponen en entredicho la oportunidad de la realización de esta obra píblica. En este trabajo se revisan y se aportan nuevos datos sobre los problemas más significativos: (i) más de 1/5 de la superficie del vaso del embalse se asienta sobre unidades carbonatadas permeables del acuífero regional de las unidades del tránsito Triásico-Jurásico (formaciones Imón, Cortes de Tajuña y Cuevas Labradas), que forman una estructura sinclinal con inmersión NNO; (ii) su situación sobre un cauce cuya aportación anual es 20% la capacidad del embalse, lo que requiere el trasvase de agua desde el río Jalón por un tínel de desviación que atraviese estructuras complejas del macizo paleozoico que constituye la Rama Aragonesa de la Cordillera Ibérica; y (iii) los riesgos geológicos que conlleva, fundamentalmente por su localización sobre el sistema de fallas de río Grío, que incluye varios segmentos activos durante el Cuaternario capaces de generar sismos de magnitud entre 6,2 y 6,8. De acuerdo con la simulación realizada mediante el programa IBER, el riesgo de inundación asociado a un posible fallo geotécnico de la presa afectaría significativamente a poblaciones importantes, como Ricla o Calatorao, situadas aguas abajo de la presa. In this work we analyze the geological hazard associated with the Mularroya reservoir (whose total volume is more than 100 hm(3)), located on the Grio river, a tributary of the Jalon river, one of the right-bank main tributaries of the Ebro river. Its construction, about to be finished, is problematic because of (i) the particular geological setting of the reservoir, located on the permeable carbonate units belonging to the Triassic-Jurassic transition (Imon, Cortes de Tajuna and Cuevas Labradas formations), defining a NNW-plunging syncline; (ii) its location on a river whose streamflow per year is 20% of the total reservoir volume, thus needing a gravity fed tunnel from the Jalon river cutting accross complex structures of the Paleozoic massifs of the Aragonian Branch of the Iberian Chain; and (iii) geological risks associated with its particular location, close to the rio Grio fault system, that includes faults that were active during the Quaternary, and are able to generate earthquakes with magnitudes 6.2-6.8. According to our simulations by means of IBER program, flooding risk associated with a possible geotechnical fault of the Mularroya dam would cause severe damage in villages located downstream (Ricla and Calatorao)