Person:
Martínez Díaz, José Jesús

First Name

José Jesús

Last Name

Martínez Díaz

URI

https://hdl.handle.net/20.500.14352/75270

Affiliation

Universidad Complutense de Madrid

Faculty / Institute

Ciencias Geológicas

Department

Geodinámica, Estratigrafía y Paleontología

Area

Geodinámica Interna

Identifiers

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Now showing 1 - 10 of 137

Identification of latent faults using a radon test
(Geomorphology, 2009) González Díez, A.; Soto, J.; Gómez Arozamena, J.; Bonachea, J.; Martínez Díaz, José Jesús; Cuesta, J. A.; Olague, I.; Remondo, J.; Fernández Maroto, G.; Díaz de Terán, J.R.
This paper discusses the use of 222Rn concentrations in water of natural springs as a geomorphological method to identify latent faults in low-mid term activity areas. The identification of this type of active fault may be crucial in hazard analysis, structural geomorphology and in landscape evolution analysis. The test used to identify these faults is based on the measuring of 222Rn concentrations in water of springs linked to faults, and comparison with those obtained from springs which, although exactly the same lithological context, are not linked with faults (reference values). If the difference between the measured value and the reference value is positive then an anomaly is identified and that measurement indicates a spring linked to a latent fault. The test was applied and validated in springs linked to faults with a latent behaviour in Cantabria, Northern Spain. These faults have shown an intermittent movement over the last 50,000 years, and have contributed towards landslide processes playing a significant role in landscape evolution of the area.
Characterization of historical earthquakes through a study of landslides by lichenometry (Murcia, SE Iberia)
(Natural Hazards, 2023) Crespo Martín, C.; Martínez Díaz, José Jesús; Martín González, Fidel
Earthquakes with magnitudes greater than 4.5–5 induce massive rockfalls close to the fault rupture zone. Driven by seismic shaking, the blocks collapse through the hillslope, which yields a fresh surface that is unbeatable for new lichen colonization. The lichenometric technique involves dating lichens developed on the surfaces of rockfall blocks induced by earthquakes. This study is focused on Cejo de Cano (Lorca, Spain), which is an earthquake-prone landslide scarp, as shown after the 2011 Lorca shaking (Mw 5.2). After this event, the possibility that the rocky volume at the foot of its slope could have a seismic origin started to be considered. In this research, lichenometry is used to date lichens on rock surfaces and test a possible correlation with the cataloged historical earthquakes. This research is important because of the large number of rockfall earthquakes found at this site by applying lichenometry compared to other studies in the literature. This technique allows us to extend the regional seismic catalog because the oldest lichens are older than the documented catalog of historical earthquakes. An oriented rockfall pattern that correlates with the location of epicenters is observed. In addition, the parallel and oblique previous fracturing of Cejo de Cano makes this scarp a suitable place to test whether the fracturing direction of the scarp could control a greater volume of rockfalls. This research opens up a new field of study to evaluate this correlation in larger areas.
Deformation of Copahue volcano: Inversion of InSAR data using a genetic algorithm
(Journal of Volcanology and Geothermal Research, 2011) Velez, Maria Laura; Euillades, Pablo; Caselli, Alberto; Blanco, Mauro; Martínez Díaz, José Jesús
The Copahue volcano is one of the most active volcanoes in Argentina with eruptions having been reported as recently as 1992, 1995 and 2000. A deformation analysis using the Differential Synthetic Aperture Radar technique (DInSAR) was performed on Copahue–Caviahue Volcanic Complex (CCVC) from Envisat radar images between 2002 and 2007. A deformation rate of approximately 2 cm/yr was calculated, located mostly on the north-eastern flank of Copahue volcano, and assumed to be constant during the period of the interferograms. The geometry of the source responsible for the deformation was evaluated from an inversion of the mean velocity deformation measurements using two different models based on pressure sources embedded in an elastic homogeneous half-space. A genetic algorithm was applied as an optimization tool to find the best fit source. Results from inverse modelling indicate that a source located beneath the volcano edifice at a mean depth of 4 km is producing a volume change of approximately 0.0015 km/yr. This source was analysed considering the available studies of the area, and a conceptual model of the volcanic–hydrothermal system was designed. The source of deformation is related to a depressurisation of the system that results from the release of magmatic fluids across the boundary between the brittle and plastic domains. These leakages are considered to be responsible for the weak phreatic eruptions recently registered at the Copahue volcano.
Deterministic seismic hazard analysis from physics-based earthquake simulations in the Eastern Betics (SE Iberia)
(Engineering Geology, 2023) Herrero Barbero, Paula; Álvarez Gómez, José Antonio; Tsige Beyene, Meaza; Martínez Díaz, José Jesús
The low frequency of large destructive earthquakes in the Eastern Betics (SE Iberian Peninsula), not recorded in the instrumental seismic catalog, complicate the estimation of the maximum ground motion that could be reached. Knowing the characteristics and behavior of these large seismic ruptures is crucial for the study of seismic hazard. In this work, we have used a physics-based earthquake simulator to generate a 100 kyr catalog of seismic ruptures associated with seismogenic faults bordering the quaternary Guadalentin and Bajo Segura basins. From these ruptures, we have selected maximum earthquake scenarios, and those associated with certain probabilities of exceeding a severe magnitude from the synthetic catalog. The estimation of maximum peak accelerations (PGA) by means of ground motion prediction equations include a possible site amplification that we have calculated from a detailed geotechnical classification of soils. According to the simulations, the modeled faults have the capacity to generate maximum earthquakes with magnitudes ranging MW 6.7–7.4. Densely populated urban areas located along the Guadalentin valley, such as Lorca, could be subject to site-dependent PGA values close to 0.6 g on the Alhama de Murcia fault trace. Similar ground motion would affect the coastline of SE Alicante province when evaluating the maximum simulated event in the Bajo Segura offshore fault. But already from magnitudes around MW ∼ 6, PGA estimations exceed critical values of 0.5 g at the south side of the Bajo Segura basin and the city of Murcia, highly dependent of ground-motion amplification induced by thick deposits of very soft and saturated soils. Our scenarios reflect that other factors such as fault geometry, kinematics and the capability observed in the simulations to generate multi-fault ruptures also affect the spatial distribution of maximum ground motion in this region. We expect that this evaluation could contribute as an improvement guideline for future strong motion prediction studies prior to the settlement of new urban infrastructures in the Eastern Betics.
Evidence for coseismic events of recurrent prehistoric deformation along the Alhama de Murcia fault, southeastern Spain
(Acta geológica hispánica, 2001) Martínez Díaz, José Jesús; Masana, Eulàlia; Hernández Enrile, José Luis; Santanach, Pere
The Alhama de Murcia fault is a 85 km long oblique-slip fault, and is related to historical and instrumental seismic activity. A paleoseismic analysis of the Lorca-Totana sector of the fault containing MSK I=VIII historical earthquakes was made in order to identify and quantify its seismic potential. We present 1) the results of the neotectonic, structural and geomorphological analyses and, 2) the results of trenching. In the study area, the Alhama de Murcia fault forms a depressed corridor between two strands, the northwestern fault with morphological and structural features of a reverse component of slip, bounding the La Tercia range to the South, and the southeastern fault strand with evidence of sinistral oblique strike-slip movement. The offset along this latter fault trapped the sediments in transit from the La Tercia range towards the Guadalentín depression. The most recent of these sediments are arranged in three generations of alluvial fans and terraces. The first two trenches were dug in the most recent sediments across the southeastern fault strand. The results indicate a coseismic reverse fault deformation that involved the sedimentary sequence up to the intermediate alluvial fan and the Holocene terrace deposits. The sedimentary evolution observed in the trenches suggests an event of temporary damming of the Colmenar creek drainage to the South due to uplifting of the hanging wall during coseismic activation of the fault. Trench, structural and sedimentological features provide evidence of at least three coseismic events, which occurred after 125,000 yr. The minimum vertical slip rate along the fault is 0.06 mm/yr and the average recurrence period should not exceed 40,000 yr in accordance with the results obtained by fan topographic profiling. Further absolute dating is ongoing to constrain these estimates
Informe del sismo de Lorca del 11 de mayo de 2011
(2011) Cabañas Rodríguez, Luis; Carreño Herrero, Emilio; Izquierdo Álvarez, Arancha; Martínez Solares, José Manuel; Capote Del Villar, Ramón; Martínez Díaz, José Jesús; Benito Oterino, Belén; Gaspar Escribano, Jorge; Rivas Medina, Alicia; García Mayordomo, Julián; Perez López, Raúl; Rodríguez Pascua, Miguel A.; Corella, Patrick Murphy
An approach for identification of areas with higher expected damage and definition of priority levels for prevention plans in Murcia Province (SE Spain)
(Bollettino di geofisica teorica ed applicata, 2008) Benito, B.; Gaspar Escribano, Jorge M.; Martínez Díaz, José Jesús; García Rodríguez, M.J.; Jiménez Peña, M.E.; Canora, C.; Álvarez Gómez, José Antonio
The Murcia Region is one of the most active zones in Spain, where three earthquakes took place in 1999, 2002 and 2005. In spite of their low magnitudes (Mw 4.8), these earthquakes caused important damage, the last one reaching an EMS-98 intensity of VII. After that event, the RISMUR project started, aimed at providing a general picture of the seismic risk, which allows us to identify zones requiring a more detailed analysis of where prevention plans should be prioritized. A multi disciplinary study, starting with the seismic hazard assessment, which follows the Probabilistic Seismic Hazard Assessment methodology has been carried out at a regional scale. The expected ground motion (rock sites), for a return period of 475 years, has been characterized in terms of PGA and spectral ordinates and the corresponding maps have been drawn. In addition, a regional geotechnical study has been done and a classification of eight types of soils has been proposed, with the corresponding amplification factors. The combination of previous maps and factors, gives a new hazard map which already includes local effects. In parallel, a vulnerability assessment of the Murcian building stock is carried out, based fundamentally on the age of construction and following the EMS-98 criteria. Taking into account the expected ground motions and building vulnerabilities, the distribution of expected damage is estimated by the application of probability damage matrixes. A suite of maps representing seismic risk in terms of damage parameters for the entire region and from which we can identify the locations with higher expected damage have been obtained. We use the Coulomb stress transfer map of the region as additional criteria for defining priority areas where detailed studies should be performed. This gives information about the zones with stress load due to the previous seismicity and where new events could be triggered. The superposition of this map with the active faults of the region and the locations with higher expected damage allows us to establish a four-level priority ranking where future local-scale analyses should be made.
Seismogenic potential and tsunami threat of the strike-slip Carboneras fault in the western Mediterranean from physics-based earthquake simulations
(Natural Hazards and Earth System Sciences, 2023) Álvarez Gómez, José Antonio; Herrero Barbero, Paula; Martínez Díaz, José Jesús
Strike-slip fault ruptures have a limited capacity to generate vertical deformation, and for this reason they are usually dismissed as potential destructive tsunami sources. At the western tip of the western Mediterranean, in the Alboran Sea, tectonics is characterized by the presence of large transcurrent fault systems and minor reverse and normal faults in a zone of diffuse deformation. The strike-slip Carboneras fault is one of the largest sources in the Alboran Sea and therefore with the greatest seismogenic capacity. It is also one of the active structures with higher slip rates in the eastern Betic fault zone and has been proposed as the source of the damaging 1522 (M 6.5; Int. VIII–IX) Almeria earthquake. The dimensions and location of the Carboneras fault imply a high seismic and tsunami threat. In this paper we present tsunami simulations from seismic sources generated with physics-based earthquake simulators. We have generated a 1 Myr synthetic seismic catalogue consistent on 773 893 events, with magnitudes ranging between Mw 3.3 and 7.6. From these events we have selected those sources producing a potential energy capable of generating a noticeable tsunami, those sources being earthquakes with magnitudes ranging from 6.71 to 7.62. The Carboneras fault has the capacity to generate locally damaging tsunamis; however, on a regional scale its tsunami threat is limited. The frequency–magnitude distribution of the generated seismic catalogue reflects the variability of magnitudes associated with the rupture of the entire fault, departing the upper limit from the classical Gutenberg–Richter potential relation. The inter-event time for the maximum earthquake magnitudes is usually between 2000 and 6000 years. The use of physics-based earthquake simulations for tsunamigenic sources allows an in-depth characterization of the scenarios, allowing a qualitative leap in their parametrization.
Evaluación de la peligrosidad sísmica en España para aplicaciones relacionadas con la seguridad nuclear. Resultados preliminares.
(2011) Benito, B.; Gaspar-Escribano, J. M.; Rivas-Medina, A.; Martínez Díaz, José Jesús; Rodríguez, O.; Ramírez, M. S.
En este trabajo se presentan los avances realizados en el marco del proyecto “Evaluación de la Peligrosidad Sísmica en España para aplicaciones relacionadas con la seguridad nuclear” financiado por el Consejo de Seguridad Nuclear. La finalidad última del proyecto es ahondar en el conocimiento de la peligrosidad sísmica y de su incertidumbre en los emplazamientos de instalaciones críticas como instalaciones nucleares y almacenamientos de residuos radiactivos en nuestro país. Con ese propósito, una primera fase del proyecto está destinada a recopilar y estructurar toda la información generada en proyectos previos financiados por el CSN (DAÑOS, SIGMA, PRIOR, EXPEL y DATACIÓN) concerniente a estudio de fallas activas, análisis de paleosismicidad, catálogos sísmicos y de movimiento fuerte del suelo, etc.. Esta información está siendo integrada y unificada en una Base de Datos y en un Sistema de Información Geográfica. Paralelamente, el código informático desarrollado en el proyecto EXPEL está siendo actualizado para desarrollar cálculos de peligrosidad sísmica siguiendo la metodología PSHA de una forma eficiente, incluyendo formulación de un árbol lógico, cuantificación de incertidumbres epistémicas y aleatorias, análisis de sensibilidad de diferentes opciones en los resultados y desagregación. Los resultados preliminares del proyecto son presentados en esta comunicación, dando una orientación hacia futuros desarrollos y toma de decisiones relacionados con la seguridad nuclear.
Mineralogía espacial: de la materia primigenia a la exploración de Marte
(Macla, 2004) Martínez Díaz, José Jesús; Rull, Fernando; Lunar Hernández, María Del Rosario