High-resolution Rayleigh-wave velocity maps of central Europe from a dense ambient-noise data set

We present a new database of surface wave group and phase-velocity dispersion curves derived from seismic ambient noise, cross-correlating continuous seismic recordings from the Swiss Network, the German Regional Seismological Network (GRSN), the Italian national broad-band network operated by the Istituto Nazionale di Geosica e Vulcanologia (INGV). To increase the aperture of the station array, additional measurements from the Mediterranean Very Broad-band Seismographic Network (MedNet), the Austrian Central Institute for Meteorology and Geodynamics (ZAMG), the French, Bulgarian, Hungarian, Romanian and Greek stations obtained through Orfeus are also included. The ambient noise, we are using to assemble our database, was recorded at the above-mentioned stations between 2006 January and 2006 December. Correlating continuous signal recorded at pairs of stations, allows to extract coherent surface wave signal travelling between the two stations. Usually the ambient-noise cross-correlation technique allows to have informations at periods of 30 s or shorter. By expanding the database of noise correlations, we seek to increase the resolution of the central Europe crustal model. We invert the resulting data sets of group and phase velocities associated with 8-35 s Rayleigh waves, to determine 2-D group and phase-velocity maps of the European region. Inversions are conducted by means of a 2-D linearized tomographic inversion algorithm. The generally good agreement of our models with previous studies and good correlation of well-resolved velocity anomalies with geological features, such as sedimentary basins, crustal roots and mountain ranges, documents the effectiveness of our approac

Tomography of the Alpine region from observations of seismic ambient noise

We use correlations of the ambient seismic noise to study the crust in western Europe. Cross correlation of 1 year of noise recorded at 150 three components broadband stations yields more than 3 000 Rayleigh wave group velocity measurements. These measurements are used to construct Rayleigh group velocity maps of the Alpine region and surrounding area in the 5-80 s period band. In the 5-10 s period band, the seismic noise recorded in Europe is dominated by surface waves originating from the Northern Atlantic ocean. This anisotropy of the noise and the uneven station distribution affect the azimuthal distribution of the paths where we obtain reliable group velocity measurements. As a consequence our group velocity models have better resolution in the northeast direction than in the southwest direction. Finally we invert the resulting Rayleigh wave group velocity maps to determine the Moho depth. Our results are in good agreement with the result of the numerous active experiments in the Alps and provide a continuous image of the Alpine structur

Anatomy of the high-frequency ambient seismic wave field at the TCDP borehole.

International audienceThe Taiwan Chelungpu-fault Drilling Project (TCDP) installed a vertical seismic array between 950 and 1270 m depth in an active thrust fault environment. In this paper we analyze continuous noise records of the TCDP array between 1 and 16 Hz. We apply multiple array processing and noise correlation techniques to study the noise source process, properties of the propagation medium, and the ambient seismic wave field. Diurnal amplitude and slowness patterns suggest that noise is generated by cultural activity. The vicinity of the recording site to the excitation region, indicated by a narrow azimuthal distribution of propagation directions, leads to a predominant ballistic propagation regime. This is evident from the compatibility of the data with an incident plane wave model, polarized direct arrivals of noise correlation functions, and the asymmetric arrival shape. Evidence for contributions from scattering comes from equilibrated earthquake coda energy ratios, the frequency dependent randomization of propagation directions, and the existence of correlation coda waves. We conclude that the ballistic and scattered propagation regime coexist, where the first regime dominates the records, but the second is weaker yet not negligible. Consequently, the wave field is not equipartitioned. Correlation signal-to-noise ratios indicate a frequency dependent noise intensity. Iterations of the correlation procedure enhance the signature of the scattered regime. Discrepancies between phase velocities estimated from correlation functions and in-situ measurements are associated with the array geometry and its relative orientation to the predominant energy flux. The stability of correlation functions suggests their applicability in future monitoring efforts

On measuring surface wave phase velocity from station–station cross-correlation of ambient signal

We apply two different algorithms to measure surface wave phase velocity, as a function of frequency, from seismic ambient noise recorded at pairs of stations from a large European network. The two methods are based on consistent theoretical formulations, but differ in the implementation: one method involves the time-domain cross-correlation of signal recorded at different stations; the other is based on frequency-domain cross-correlation, and requires finding the zero-crossings of the real part of the cross-correlation spectrum. Furthermore, the time-domain method, as implemented here and in the literature, practically involves the important approximation that interstation distance be large compared to seismic wavelength. In both cases, cross-correlations are ensemble-averaged over a relatively long period of time (1 yr). We verify that the two algorithms give consistent results, and infer that phase velocity can be successfully measured through ensemble-averaging of seismic ambient noise, further validating earlier studies that had followed either approach. The description of our experiment and its results is accompanied by a detailed though simplifed derivation of ambient-noise theory, writing out explicitly the relationships between the surface wave Green’s function, ambient-noise cross-correlation and phase and group velocities

Toward Forecasting Volcanic Eruptions using Seismic Noise

During inter-eruption periods, magma pressurization yields subtle changes of the elastic properties of volcanic edifices. We use the reproducibility properties of the ambient seismic noise recorded on the Piton de la Fournaise volcano to measure relative seismic velocity variations of less than 0.1 % with a temporal resolution of one day. Our results show that five studied volcanic eruptions were preceded by clearly detectable seismic velocity decreases within the zone of magma injection. These precursors reflect the edifice dilatation induced by magma pressurization and can be useful indicators to improve the forecasting of volcanic eruptions.Comment: Supplementary information: http://www-lgit.obs.ujf-grenoble.fr/~fbrengui/brenguier_SI.pdf Supplementary video: http://www-lgit.obs.ujf-grenoble.fr/~fbrengui/brenguierMovieVolcano.av

Using SVD for improved interferometric Green's function retrieval

Seismic interferometry (SI) is a technique used to estimate the Green's function (GF) between two receiver locations, as if there were a source at one of the receiver locations. However, in many applications, the requirements to recover the exact GF are not satisfied and SI yields a poor estimate of the GF. For these non-ideal cases, we improve the interferometric GFs, by applying singular value decomposition (SVD) to the cross-correlations before stacking. The SVD approach preserves energy that is stationary in the cross-correlations, which is the energy that contributes most to the GF recovery, and attenuates non-stationary energy, which leads to artefacts in the interferometric GF. We apply this method to construct virtual shot gathers (for both synthetic and field data) and demonstrate how using SVD enhances physical arrivals in these gathers. We also find that SVD is robust with respect to weakly correlated random noise, allowing a better recovery of events from noisy data, in some cases recovering energy that would otherwise be completely lost in the noise and that the standard SI technique fails to recover

Understanding fungal functional biodiversity during the mitigation of environmentally dispersed pentachlorophenol in cork oak forest soils

Pentachlorophenol (PCP) is globally dispersed and contamination of soil with this biocide adversely affects its functional biodiversity, particularly of fungi - key colonizers. Their functional role as a community is poorly understood, although a few pathways have been already elucidated in pure cultures. This constitutes here our main challenge - elucidate how fungi influence the pollutant mitigation processes in forest soils. Circumstantial evidence exists that cork oak forests in N. W. Tunisia - economically critical managed forests are likely to be contaminated with PCP, but the scientific evidence has previously been lacking. Our data illustrate significant forest contamination through the detection of undefined active sources of PCP. By solving the taxonomic diversity and the PCP-derived metabolomes of both the cultivable fungi and the fungal community, we demonstrate here that most strains (predominantly penicillia) participate in the pollutant biotic degradation. They form an array of degradation intermediates and by-products, including several hydroquinone, resorcinol and catechol derivatives, either chlorinated or not. The degradation pathway of the fungal community includes uncharacterized derivatives, e.g. tetrachloroguaiacol isomers. Our study highlights fungi key role in the mineralization and short lifetime of PCP in forest soils and provide novel tools to monitor its degradation in other fungi dominated food webs. © 2015 Society for Applied Microbiology and John Wiley & Sons Ltd

L'influence du contexte conjoncturel sur la fonction intégrative de la cour de justice des communautés européennes dans le domaine de la libre circulation des marchandises

Le rôle intégratif que la Cour de justice des Communautés européennes (CJCE) a joué dans la construction européenne est bien connu et très documenté. Ce qui l'est moins ce sont les raisons qui l'ont motivé, et le motivent encore. Si certains se sont déjà penchés sur cette question, un aspect a néanmoins été complètement négligé, celui de l'influence qu'a pu avoir à cet égard le contexte conjoncturel sur la jurisprudence communautaire et plus précisément sur l'orientation que la Cour a choisi de lui donner. Dans ce cadre, les auditoires de la Cour ont un rôle déterminant. Pour s'assurer d'une bonne application de ses décisions, la Cour est en effet amenée à prendre en considération les attentes des États membres, des institutions européennes, de la communauté juridique (tribunaux nationaux, avocats généraux, doctrine et praticiens) et des ressortissants européens (citoyens et opérateurs économiques). Aussi, à la question du pourquoi la CJCE décide (ou non) d'intervenir, dans le domaine de la libre circulation des marchandises, en faveur de l'intégration économique européenne, j'avance l'hypothèse suivante: l'intervention de la Cour dépend d'une variable centrale : les auditoires, dont les attentes (et leur poids respectif) sont elles-mêmes déterminées par le contexte conjoncturel. L'objectif est de faire ressortir l'aspect plus idéologique de la prise de décision de la Cour, largement méconnu par la doctrine, et de démontrer que le caractère fluctuant de la jurisprudence communautaire dans ce domaine, et en particulier dans l'interprétation de l'article 28 du traité CE, s'explique par la prise en compte par la Cour des attentes de ses auditoires, lesquels ont majoritairement adhéré à l'idéologie néolibérale. Afin de mieux saisir le poids - variable - de chaque auditoire de la Cour, j'apprécierai, dans une première partie, le contexte conjoncturel de la construction européenne de 1990 à 2006 et notamment le virage néolibéral que celle-ci a opéré. L'étude des auditoires et de leur impact sur la jurisprudence fera l'objet de la seconde partie de ma thèse. Je montrerai ainsi que la jurisprudence communautaire est une jurisprudence « sous influence », essentiellement au service de la réalisation puis de l'approfondissement du marché intérieur européen.The integrative role played by the Court of Justice of the European Communities (CJEC) in the construction of Europe is well known and documented. However the reasons that have motivated the CJEC in this role are far less known. Although some studies have been conducted on this topic, one aspect has been completely ignored: the influence of the conjunctural context on the European Community case law, and more precisely the orientation that the Court has chosen to give to the latter. Within this scope the Court's audiences play a determining role. To ensure that its decisions are well followed, the CJEC takes into consideration the expectations of the Member States, the European institutions, the judicial community (national tribunals, Advocates General, doctrine and practitioners), and the European citizens and economic operators. In regard to the question as to whether or not the CJEC decides to intervene in the domain of free movement of goods, in favour of the European economic integration, I argue the following hypothesis: the intervention of the Court depends on a central variable, that of the audiences, of which the expectations (and their relative weight) are determined by the conjunctural context. My objective is to point out the ideological aspects of the Court's decision making, mostly unknown to legal scholarship, and to demonstrate that the fluctuating character of case law in this domain, and more precisely in the interpretation of Article 28 of the CE Treaty, is explained by the Court’s taking into consideration the expectations of its audiences, which are mainly committed to the neoliberal ideology. In order to evaluate the varying weight of each audience of the CJEC, the first part of the thesis will delve into the conjunctural context and the European construction from 1990 to 2006 where in particular, we observe a turn towards neoliberalism. The study of the audiences and their impact on EC case law will be the subject of the second part of the thesis. I will show that this case law is "under influence", essentially to the service of the development and the strengthening of the European internal market

Coda-Q in the 2.5s -20s period band from seismic noise - Application to the greater Alpine area

International audienceCoda-Q is used to estimate the attenuation and scattering properties of the Earth (Aki & Chouet 1975). So far focus has been on earthquake data at frequencies above 1 Hz, as the high noise level in the first and second microseismic peak, and possibly lower scattering coefficient, hinder stable measurements at lower frequencies. In this work, we measure and map coda-Q in the period bands 2.5 s-5 s, 5 s-10 s and 10 s-20 s in the greater Alpine region using noise cross-correlations between station pairs, based on data from permanent seismic stations and from the temporary AlpArray experiment. The observed coda-Q for short interstation distances is independent of azimuth so there is no indication of influence of the directivity of the incoming noise field on our measurements. In the 2.5 s-5 s and 5 s-10 s period bands, our measurements are self-consistent, and we observe stable geographic patterns of low and high coda-Q in the period bands 2.5 s-5 s and 5 s-10 s. In the period band 10 s-20 s, the dispersion of our measurements increases and geographic patterns become speculative. The coda-Q maps show that major features are observed with high resolution, with a very good geographical resolution of for example low coda-Q in the Po Plain. There is a sharp contrast between the Po Plain and the Alps and Apennines where coda-Q is high, with the exception a small area in the Swiss Alps which may be contaminated by the low coda-Q of the Po Plain. The coda of the correlations is too short to make independent measurements at different times within the coda, so we cannot distinguish between intrinsic and scattering Q. Measurements on more severely selected datasets and longer timeseries result in identical geographical patterns but lower numerical values. Therefore, high coda-Q values may be overestimated, but the geographic distribution between high and low coda-Q areas is respected. Our results demonstrate that noise correlations are a promising tool for extending coda-Q measurements to frequencies lower than those analysed with earthquake data

Magmatism on rift flanks: insights from ambient noise phase velocity in Afar region

During the breakup of continents in magmatic settings, the extension of the rift valley is commonly assumed to initially occur by border faulting and progressively migrate in space and time toward the spreading axis. Magmatic processes near the rift flanks are commonly ignored. We present phase velocity maps of the crust and uppermost mantle of the conjugate margins of the southern Red Sea (Afar and Yemen) using ambient noise tomography to constrain crustal modification during breakup. Our images show that the low seismic velocities characterize not only the upper crust beneath the axial volcanic systems but also both upper and lower crust beneath the rift flanks where ongoing volcanism and hydrothermal activity occur at the surface. Magmatic modification of the crust beneath rift flanks likely occurs for a protracted period of time during the breakup process and may persist through to early seafloor spreading