Medium change monitoring using ambient seismic noise and coda wave interferometry: examples from intraplate NE Brazil and the Mid-Atlantic Ridge

This thesis presents and discusses the results of ambient seismic noise correlation for two different environments: intraplate and Mid-Atlantic Ridge. The coda wave interferometry method has also been tested for the intraplate data. Ambient noise correlation is a method that allows to retrieve the structural response between two receivers from ambient noise records, as if one of the station was a virtual source. It has been largely used in seismology to image the subsurface and to monitor structural changes associated mostly with volcanic eruptions and large earthquakes. In the intraplate study, we were able to detect localized structural changes related to a small earthquake swarm, which main event is mR 3.7, North-East of Brazil. We also showed that the 1-bit normalization and spectral whitening result on the loss of waveform details and that the phase auto-correlation, which is amplitude unbiased, seems to be more sensitive and robust for our analysis of a small earthquake swarm. The analysis of 6 months of data using cross-correlations detect clear medium changes soon after the main event while the auto-correlations detect changes essentially after 1 month. It could be explained by fluid pressure redistribution which can be initiated by hydromechanical changes and opened path ways to shallower depth levels due to later occurring earthquakes. In the Mid-Atlantic Ridge study, we investigate structural changes associated with a mb 4.9 earthquake in the region of the Saint Paul transform fault. The data have been recorded by a single broadband seismic station located at less than 200 km from the Mid-Atlantic ridge. The results of the phase auto-correlation for a 5-month period, show a strong co-seismic medium change followed by a relatively fast post-seismic recovery. This medium change is likely related to the damages caused by the earthquake’s ground shaking. The healing process (filling of the new cracks) that lasted 60 days can be decomposed in two phases, a fast recovery (70% in ~30 days) in the early post-seismic stage and a relatively slow recovery later (30% in ~30 days). In the coda wave interferometry study, we monitor temporal changes of the subsurface caused by the small intraplate earthquake swarm mentioned previously. The method was first validated with synthetics data. We were able to detect a change of 2.5% in the source position and a 15% decrease of the scatterers’ amount. Then, from the real data, we observed a rapid decorrelation of the seismic coda after the mR 3.7 seismic event. This indicates a rapid change of the subsurface in the fault’s region induced by the earthquake.

Medium change monitoring using ambient seismic noise and coda wave interferometry: examples from intraplate NE Brazil and the Mid-Atlantic Ridge

This thesis presents and discusses the results of ambient seismic noise correlation for two different environments: intraplate and Mid-Atlantic Ridge. The coda wave interferometry method has also been tested for the intraplate data. Ambient noise correlation is a method that allows to retrieve the structural response between two receivers from ambient noise records, as if one of the station was a virtual source. It has been largely used in seismology to image the subsurface and to monitor structural changes associated mostly with volcanic eruptions and large earthquakes. In the intraplate study, we were able to detect localized structural changes related to a small earthquake swarm, which main event is mR 3.7, North-East of Brazil. We also showed that the 1-bit normalization and spectral whitening result on the loss of waveform details and that the phase auto-correlation, which is amplitude unbiased, seems to be more sensitive and robust for our analysis of a small earthquake swarm. The analysis of 6 months of data using cross-correlations detect clear medium changes soon after the main event while the auto-correlations detect changes essentially after 1 month. It could be explained by fluid pressure redistribution which can be initiated by hydromechanical changes and opened path ways to shallower depth levels due to later occurring earthquakes. In the Mid-Atlantic Ridge study, we investigate structural changes associated with a mb 4.9 earthquake in the region of the Saint Paul transform fault. The data have been recorded by a single broadband seismic station located at less than 200 km from the Mid-Atlantic ridge. The results of the phase auto-correlation for a 5-month period, show a strong co-seismic medium change followed by a relatively fast post-seismic recovery. This medium change is likely related to the damages caused by the earthquake’s ground shaking. The healing process (filling of the new cracks) that lasted 60 days can be decomposed in two phases, a fast recovery (70% in ~30 days) in the early post-seismic stage and a relatively slow recovery later (30% in ~30 days). In the coda wave interferometry study, we monitor temporal changes of the subsurface caused by the small intraplate earthquake swarm mentioned previously. The method was first validated with synthetics data. We were able to detect a change of 2.5% in the source position and a 15% decrease of the scatterers’ amount. Then, from the real data, we observed a rapid decorrelation of the seismic coda after the mR 3.7 seismic event. This indicates a rapid change of the subsurface in the fault’s region induced by the earthquake.

TEOLOGIA E TRADIÇÃO NO CONTEXTO DAS RELIGIÕES DE UMBANDA: UMA ANÁLISE DO CONFLITO ENTRE CULTURA ACADÊMICA E POPULAR

A religião de Umbanda ocupa grande espaço na vida e no imaginário religioso brasileiro, e adota as lendas, mitos e folclore da cultura popular brasileira. Desprovida de texto sagrado, a Umbanda rejeita a ideia do entendimento de uma literatura sagrada como pressuposto para uma ligação com o divino, sendo mais preocupada com a experiência religiosa e do sagrado, como ponte entre a dimensão humana e divina. Embora de comum acordo sobre a importância da prática na religião de Umbanda, existe um forte debate teológico na questão do valor principal para as práticas e vida religiosa do filho de santo. De um lado, temos a Doutrina Esotérica que aposta na produção textual e teórica e, de outro, temos a Umbanda de popular, que aposta na experiência pessoal do filho de santo com a tradição oral e as práticas religiosas. De sua fundação até a presente data, a Umbanda Esotérica tem apostado na formação acadêmica como base principal para a instrumentalização do filho de santo para a prática no terreiro, assim como publica��ão de textos, livros, artigos, oferecimento de cursos e a criação da primeira instituição especializada de ensino, a Faculdade de Teologia Umbandista. Se por um lado, para alguns, isso possa parecer uma abertura para a modernização e melhor aceitação das práticas de origem africanas, para outros, representa uma limitação na prática e na experiência do filho de santo devido à racionalidade do espaço acadêmico. Desse modo, pretendo investigar esse conflito no discurso e nas suas especificidades, estudando literatura especializada e orgânica, tendo como eixo de investigação a seguinte questão: O que é mais importante para as práticas religiosas em Umbanda, a formação prática ou a acadêmica?

Imaginer l’Amérique : Québec à travers les vues d’optique des graveurs allemands Habermann et Leizelt

Publiées dans la Collection des prospects durant la guerre d’Indépendance américaine, les vues d’optique Vuë de la Place capitale dans la Ville basse a Quebec, Vuë de la haute ville a Quebeck, Vuë de la basse Ville a Quebec vers le fleuve St-Laurent, Vuë de la rue des recolets de Quebeck et Vuë de Quebeck gravées par les Allemands Franz Xaver Habermann (1721-1796) et Balthasar Frederich Leizelt (1755-1812) entretiennent des liens ténus avec la configuration réelle de la ville de Québec qu’elles représentent. L’escamotage du paradigme documentaire dans ces images est l’enjeu principal de ce mémoire. Il permet de mettre l’accent sur les contraintes formelles découlant du dispositif optique de lecture utilisé ainsi que sur les modèles culturels concernant la perception du territoire urbain américain ayant prévalu lors de la création et de la réception des cinq vues d’optique à l’étude. L’analyse de la vision fictionnelle du paysage donnera également des indices sur les orientations idéologiques et l’imaginaire du lieu, perçu comme un ailleurs lointain, par un ensemble politique qui n’exerce pas de domination directe sur la colonie installée sur le bord du fleuve Saint-Laurent.

La prioridad del Igualitarismo Democrático

Este artículo mostrará que las versiones estrictas del Igualitarismo Democrático y del Igualitarismo de la Suerte son implausibles ya que defienden una visión monista del objeto de la justicia igualitaria. Por el contrario, sus versiones moderadas son aceptables ya que admiten la composición plural del objeto de justicia igualitaria.Esta comprensión plural exige, sin embargo, el establecimiento de prioridades normativas ya que las exigencias de cada valor entran típicamente en conflicto. Aquí, se ofrecerán tres argumentos para defender la prioridad del Igualitarismo Democrático sobre el Igualitarismo de la Suerte: uno instrumental, otro relacionado con el significado expresivo de las políticas públicas estatales y un último que justifica la división del trabajo moral igualitarista.

Imperative, subjunctive, and the desiderative-appellative space in Spanish

After defining the “enunciative scheme” (sentence type) as a communicative unit, the imperative is characterized as a morphologized modality of appellative kind used when the following conditions occur: appellative meaning, 2nd person, future tense and absence of negation. In Spanish, any variation of any of these requirements determines that the subjunctive is used. We reject the idea that the imperative is a variant of subjunctive specialized in appellative function and that both modes share a desiderative morpheme. Working in this way means attributing to a morphological category of the verb a property that actually corresponds to the enunciative schemes (sentence types). We propose to integrate the imperative and subjunctive in the framework of what we call the “desiderative-appellative space”. This “space” brings together various grammatical or grammaticalized means based on the imperative and the subjunctive. Semantically, it is organized around a component of desirability (action appears as desirable) that, by varying several factors, configures a route that goes from a center (the imperative) to a periphery (the expression of desire).

Imaginer l’Amérique : Québec à travers les vues d’optique des graveurs allemands Habermann et Leizelt

Publiées dans la Collection des prospects durant la guerre d’Indépendance américaine, les vues d’optique Vuë de la Place capitale dans la Ville basse a Quebec, Vuë de la haute ville a Quebeck, Vuë de la basse Ville a Quebec vers le fleuve St-Laurent, Vuë de la rue des recolets de Quebeck et Vuë de Quebeck gravées par les Allemands Franz Xaver Habermann (1721-1796) et Balthasar Frederich Leizelt (1755-1812) entretiennent des liens ténus avec la configuration réelle de la ville de Québec qu’elles représentent. L’escamotage du paradigme documentaire dans ces images est l’enjeu principal de ce mémoire. Il permet de mettre l’accent sur les contraintes formelles découlant du dispositif optique de lecture utilisé ainsi que sur les modèles culturels concernant la perception du territoire urbain américain ayant prévalu lors de la création et de la réception des cinq vues d’optique à l’étude. L’analyse de la vision fictionnelle du paysage donnera également des indices sur les orientations idéologiques et l’imaginaire du lieu, perçu comme un ailleurs lointain, par un ensemble politique qui n’exerce pas de domination directe sur la colonie installée sur le bord du fleuve Saint-Laurent.

The Amplifier - v. 17, no. 5

In this issue...Don Heater, Engineering Days, St. Louis Cardinals, Grass Roots, Floyd Bossard, Bill of Rights, Saint Patrick, Optometry, Handball Club, George Carlin

Impact of adenosine nucleotide translocase (ANT) proline isomerization on Ca(2+)-induced cysteine relative mobility/mitochondrial permeability transition pore

Mitochondrial membrane carriers containing proline and cysteine, such as adenine nucleotide translocase (ANT), are potential targets of cyclophilin D (CyP-D) and potential Ca(2+)-induced permeability transition pore (PTP) components or regulators; CyP-D, a mitochondrial peptidyl-prolyl cis-trans isomerase, is the probable target of the PTP inhibitor cyclosporine A (CsA). In the present study, the impact of proline isomerization (from trans to cis) on the mitochondrial membrane carriers containing proline and cysteine was addressed using ANT as model. For this purpose, two different approaches were used: (i) Molecular dynamic (MD) analysis of ANT-Cys(56) relative mobility and (ii) light scattering techniques employing rat liver isolated mitochondria to assess both Ca(2+)-induced ANT conformational change and mitochondrial swelling. ANT-Pro(61) isomerization increased ANT-Cys(56) relative mobility and, moreover, desensitized ANT to the prevention of this effect by ADP. In addition, Ca(2+) induced ANT ""c"" conformation and opened PTP; while the first effect was fully inhibited, the second was only attenuated by CsA or ADP. Atractyloside (ATR), in turn, stabilized Ca(2+)-induced ANT ""c"" conformation, rendering the ANT conformational change and PTP opening less sensitive to the inhibition by CsA or ADP. These results suggest that Ca(2+) induces the ANT ""c"" conformation, apparently associated with PTP opening, but requires the CyP-D peptidyl-prolyl cis-trans isomerase activity for sustaining both effects.

Early Variscan I-type pluton in the pre-Alpine basement of the Western Alps: The ca. 360 Ma Cogne diorite (NW-Italy)

Located at the internal border of the Grand-Saint-Bernard Zone, the diorite and its aureole lie on top of intensively studied Alpine eclogitic units but this pluton, poorly studied yet, has kept locally almost undeformed. The pluton intruded, at similar to 360 Ma, country-rocks mostly composed of dark shales with Na2O > K2O and minor mafic intercalations of tholeiitic basalt affinity. This association is characteristic of the Vanoise (France) basement series, where available age determinations suggest an Early Paleozoic age. Parts of the pluton, and of its hornfels aureole that is evidenced here for the first time, in the Punta Bioula section of Valsavaranche valley (NW-Italy), have been well-preserved from the Alpine deformation. Syn-emplacement hardening, dehydration-induced, probably prevented strain-enhanced Alpine recrystallization. Magmatic rock-types range continuously from subordinate mafic types at SiO2 similar to 48%, of hornblendite with cumulative or appinite affinities, to the main body of quartz diorite to quartz monzonite (SiO2 up to 62%). P-T estimates for the pluton emplacement, based on the abundance of garnet in the hornfelses, using also zircon and apatite saturation thermometry and Al-in-hornblende barometry, suggest T similar to 800-950 degrees C and minimum P in the 0.2-0.5 GPa range, with records of higher pressure conditions (up to 1-2 GPa?) in hornblendite phlogopite-cored amphibole. The high-K, Na > K, calcalkaline geochemistry is in line with a destructive plate-margin setting. Based on major element data and radiogenic isotope signature (epsilon Nd-360 Ma from -1.2 to + 0.9, Sr-87/Sr-86(360 MA) from 0.7054 to 0.7063), the parental magmas are interpreted in terms of deep-seated metabasaltic partial melts with limited contamination from shallower sources, the low radiogenic Nd-content excluding a major contribution from Vanoise tholeiites. There is no other preserved evidence for Variscan magmatism of similar age and composition in the Western Alps, but probable analogs are known in the western and northern parts of French Massif Central. Regarding the Alpine tectonics, not only the age of the pluton and its host-rocks (instead of the Permo-Carboniferous age previously believed), but also its upper mylonitic contact, suggest revisions of the Alpine nappe model. The Cogne diorite allegedly constituted the axial part of the E-verging ``pli en retour [backfold] du Valsavaranche'', a cornerstone of popular Alpine structural models: in fact, the alleged fold limbs, as attested here by field and geochemical data, do not belong to the same unit, and the backfold hypothesis is unfounded. (C) 2012 Elsevier B.V. All rights reserved.

Stable isotope record, Mg/Ca ratios and age model of St. Stephens Quarry, Alabama

In the largest global cooling event of the Cenozoic Era, between 33.8 and 33.5 Myr ago, warm, high-CO2 conditions gave way to the variable 'icehouse' climates that prevail today. Despite intense study, the history of cooling versus ice-sheet growth and sea-level fall reconstructed from oxygen isotope values in marine sediments at the transition has not been resolved. Here, we analyse oxygen isotopes and Mg/Ca ratios of benthic foraminifera, and integrate the results with the stratigraphic record of sea-level change across the Eocene-Oligocene transition from a continental-shelf site at Saint Stephens Quarry, Alabama. Comparisons with deep-sea (Sites 522 (South Atlantic) and 1218 (Pacific)) d18O and Mg/Ca records enable us to reconstruct temperature, ice-volume and sea-level changes across the climate transition. Our records show that the transition occurred in at least three distinct steps, with an increasing influence of ice volume on the oxygen isotope record as the transition progressed. By the early Oligocene, ice sheets were ~25% larger than present. This growth was associated with a relative sea-level decrease of approximately 105 m, which equates to a 67 m eustatic fall.