接收函数方法与中国及邻区上地幔间断面的研究

The receiver function method applied in researching the discontinuities in upper mantle was systematically studied in this paper. Using the theoretical receiver functions, the characteristics of P410S and P660S phases were analyzed, and the influencing factors for detection of these phases were discussed. The stability of receiver function was studied, and a new computational method of receiver function, RFSSMS (Receiver Function of Stack and Smooth of Multi seismic-records at a Single station), was put forward. We built initial reference velocity model for the media beneath each of 18 seismic stations respectively; then estimated the buried depths of 410-km and 660-km discontinuities(simply marked as '410' and '660') under the stations by using the arrive time differences of P410S and P660S with P. We developed a new receiver function inversion method -PGARFI (Peeling-Genetic Algorithm of Receiver Function Inversion), to obtain the whole crust and upper mantle velocity structure and the depths of discontinuities beneath a station. The major works and results could be summarized as follows: (1) By analysis of the theoretical receiver functions with different velocity models and different ray parameters, we obtain the knowledge: The amplitudes of P410S and P660S phases are decreasing with the increasing of epicentral distance A , and the arrival time differences of these phases with P are shorter as A is longer. The multiple refracted and/or reflected waves yielded on Moho and the discontinuities in the crust interfere the identification of P410S. If existing LVZ under the lithosphere, some multiple waves caused by LVZ will interfere the identification of P410S. The multiple waves produced by discontinuity lied near 120km depth will mix with P410s phase in some range of epicentral distance; and the multiple waves concerned with the discontinuity lied near 210km depth will interfere the identification of P660S. The epicentral distance for P4i0s identification is limited, the upper limit is 80° . The identification of P660S is not restricted by the epicenter distance obviously. The identification of P410S and P6gos in the theoretical receiver functions is interfered weakly from the seismic wave attenuation caused by the media absorption if the Q value in a reasonable range. (2) The stability of receiver function was studied by using synthetic seismograms with different kind of noise. The results show that on the condition of high signal-noise-ratio of seismic records, the high frequency background noise and the low frequency microseism noise do not influence the calculating result of receiver function. But the media "scattering noise" influence the stability of receiver function. When the scattering effect reach some level, the identification of P4iOs and P66os is difficult in single receiver function which is yielded from only one seismic record. We provided a new method to calculate receiver function, that is, with a group of earthquake records, stacking the R and Z components respectively in the frequency domain, and weighted smooth the stacked Z component, then compute the complex spectrum ratio of R to Z. This method can improve the stability of receiver function and protrude the P4i0s and P66os in the receiver function curves. (3) 263 receiver functions were provided from 1364 three component broadband seismograms recorded at 18 stations in China and adjacent areas for the tele-earthquakes. The observed arrival time differences of P410S and P660S with P were obtained in these receiver functions. The initial velocity model for every station was built according to the prior research results. The buried depths of '410' and '660' under a station were acquired by the way of adjusting the depths of these two discontinuities in the initial velocity model until the theoretical arrival time differences of P410S and P660S with P well conformed to the observed. The results show an obvious lateral heterogeneity of buried depths of ' 410' and (660' . The depth of '410' is shallower beneath BJI, XAN, LZH and ENH, but deeper under QIZ and CHTO, and the average is 403km . The average depth of '660' is 663km, deeper under MDJ and MAJO, but shallower under QIZ and HYB. (4) For inversing the whole crust and upper mantle velocity structure, a new inversion method -PGARFI (Peeling-Genetic Algorithm of Receiver Function Inversion) has- been developed here. The media beneath a station is divided into segments, then the velocity structure is inversed from receiver function from surface to deep successively. Using PGARFI, the multi reflection / refraction phases of shallower discontinuities are isolated from the first order refraction transform phase of deep discontinuity. The genetic algorithm with floating-point coding was used hi the inversion of every segment, and arithmetical crossover and non-uniform mutation technologies were employed in the genetic optimization. 10 independent inversions are completed for every segment, and 50 most excellent velocity models are selected according to the priority of fitness from all models produced in the inversion process. The final velocity structure of every segment is obtained from the weighted average of these 50 models. Before inversion, a wide range of velocity variation with depth and depth range of the main discontinuities are given according to priori knowledge. PGARFI was verified with numerical test and applied in the inversion of the velocity structure beneath HIA station down to 700km depth.

大港千米桥地区综合地质地球物理研究

Qianmiqiao buried hill, which is a high-yield burial hill pool, was discovered at Dagang oilfield in 1998. To employ the integrated geological and geophysical research at Qianmiqiao area, it is very valuable and meaningful for the petroleum exploration of Bohai Bay Basin and even the whole country. Based on the previous results, this paper is carried out from the research on Huanghua depression, following the law, i.e. the deep part constrains the shallow, the regional constrains the local, takes the geophysical research in Qianmiqiao oilfield, discusses the formation history of burial hills, burial history, thermal history, the generated and expelling history of hydrocarbon, and migration characteristics, probes into the formation of burial hill pool. This paper uses the gravity and magnetic methods which are based on potential field, with natural sources, configures the inner structure of the earth according to the difference in the density and magnetism of the rock. The geophysical characteristics of Dagang oil field is that it is an area with positive Buge gravity anomal. The upheaval of Moho boundary is in mirror symmetry with the depression of the basin's basement. The positive and negative anomaly distributein axis symmetry, and the orientation is NNE. The thickness of the crust gradually reduces from west to east, from land to sea. The depth gradient strip of Curie surface is similar to Moho boundary, whereas their local buried depth is different. Local fractures imply that the orientation of base rock fractures is NNE-NE, and the base rock is intersected by the fractures of the same/ later term, whose orientation is NW, so the base rock likes rhombic mosaic. The results of tomography show that there exists significant asymmetry in vertical and horizontal direction in the velocity configuration of Huanghua depression. From Dezhou to Tianjin, there exits high-speed block, which extends from south to north. The bottom of this high-speed block is in good agreement with the depth of Moho boundary. Hence we can conclude that the high-speed block is actually the crystal basement. According to seismic data, well data and outcrop data, Huanghua depression can be divided into four structure layers, i.e. Pi,2-T, Ji,2-K, E, N-Q. Qianmiqiao burial hills undergo many tectonic movement, where reverse faults in developed in inner burial hill from Indosinian stage to Yanshanian stage, the normal faults extended in Himalayan stage. Under the influence of tectonic movements, the burial hills show three layers, i.e. the reverse rushing faults in buried hills, paleo-residual hill, and extended horst block. The evolution of burial hills can be divided into four stages: steady raising period from Calenonian to early Hercynian, rushing brake drape period from Indosinian to middle Yanshanian, block tilting period in early Tertiary, and heating depression period from late Tertiary to Quaternary. The basin modeling softwares BasinMod 1-D and Basin 2-D, which are made by PRA corporation, are used in this paper, according to the requirement, corresponding geological model is designed. And we model the burial history, thermal history, hydrocarbon generation and hydrocarbon expelling history of Qianmiqiao area. The results show that present bury depth is the deepest in the geological history, the sedimentary rate of Tertiary is highest and its rising rate of temperature rate is higher. During sedimentary history, there is no large erosion, and in the Tertiary, the deeper sediment was deposited in large space, therefore it is in favor of the conservation and transformation of oil and gas. The thermal research shows that the heat primarily comes from basement of the basin, present geotherm is the highest temperature in the geological history. Major source rock is the strata of ES3, whose organic is abundant, good-typed, maturative and of high-expulsive efficiency. The organic evolution of source rock of O has come to the overmature stage, the evolving time is long and the source rock can be easily destroyed. Therefore it is more difficult for the O formation source rock to form the huge accumulation of oil and gas than Es3 formation. In the research of oil assembling, we first calculated the characteristics of the fluid pressure of single well, then analyzed the distribution of the surplus fluid pressure of each formation and profile, and probe the first hydrocarbon migration situation and the distribution of pressure system of buried hill pool. In every formation, the pressure system of each burial hill has its own characteristics, e.g. high pressure or low pressure. In the research of secondary migration, the fluid potential is calculated while the relative low potential area is figured out. In Qianmiqiao area, the west margin faults have the low potential, and hence is the favorable reconnoiter belt.

利用宽频带台阵资料研究华北地区地壳及上地幔间断面结构

Intense tectonic renovation has occurred in the eastern continent of china since Mesozoic, as evidenced by the high heat flow, widespread magma extrusion and volcanic activities, and development of large sedimentary basins. To explain the cause and mechanism for the tectonic process in this period, some researchers have put forward various models, such as mantle plume, subduction of the Pacific slab, Yangtze Block-North China Block collision, etc. Their seismological evidence, however, is still scarce..During the period from 2000 to 2003, large temporary seismic arrays were established in North China by the Institute of the Geology and Geophysics, Chinese Academy of Sciences. Total 129 portable seismic stations were linearly emplaced across the western and eastern boundaries of the Bohai Bay Basin, and accumulated a large amount of high-quality data. Moreover, abundant data were also collected at the capital digital seismic network established in the ninth five-year period of national economic and social development. These provide an unprecedented opportunity for us to study the deep structure and associated geodynamic mechanism of lithospheric processes in North China using seismological techniques.Seismology is a kind of observation-based science. The development of seismic observations greatly promotes the improvement of seismologic theory and methodology. At the beginning of this thesis, I review the history of seismic observation progress, and present some routine processing techniques used in the array seismology. I also introduce two popular seismic imaging methods (receiver function method and seismic tomography).Receiver function method has been widely used to study the crustal and upper mantle structures, and many relevant research results have been published. In this thesis I elaborate the theory of this method, including the basic concept of receiver functions and the methodology for data pre-processing, stacking and migration. I also address some problems often encountered in practical applications of receiver function imaging.By using the teleseismic data collected at the temporary seismic arrays in North China, in particular, the traveltime information of P-to-S conversion and multiple reverberations of the Moho discontinuity, I obtain the distributions of the crustal thickness and the poisson ratio at the northwest boundary area of the Bohai Bay Basin and discuss the geological implications of the results.Through detailed intestigations on the crustal structural feature around the middle part of the Tanlu fault, considerable disparity in poisson ratios is found in the western and eastern sides of the Tanlu fault. Moreover, an obvious Moho offset is coincidently observed at the same surface location. A reasonable density model for the Tanlu fault area is also derived by simulating the observed gravity variations. Both receiver function study and gravity anomaly modeling suggest that the crustal difference between the western and eastern sides of the Tanlu fault is mainly resulted from their different compositions.With common conversion point imaging of receiver functions, I estimate the depths of the upper and lower boundaries of the mantle transition zone, i.e., the 410 and 660 km discontinuities, beneath most part of the North China continent The thickness of the transition zone (TTZ) in the study area is calculated by subtracting the depth of .410 km discontinuity from that of the 660km discontinuity. The resultant TTZ is 10-15 km larger in the east than in the west of the study area. Phase transitions at the 410 km and the 660 km discontinuities are known to have different Clapeyron slopes. Therefore, the TTZ is sensitive to the temperature changes in the transition zone. Previous studies have shown that the TTZ would be smaller in the mantle plume areas and become larger when the remnants of subducted slabs are present The hypothesis of mantle plume cannot give a reasonable interpretation to the observed TTZ beneath North China, Instead, the receiver function imaging results favor a dynamic model that correlates the thermal structure of the mantle transition zone and associated upper mantle dynamics of North China to the Pacific plate subduction process.

Sistemas alternativos a los fungicidas químicos para el control de Penicillium digitatum (Pers.) Sacc. en limón

Argentina es el principal productor mundial de limones en el mundo y el 90 por ciento de esta producción se sitúa en la provincia de Tucumán. Las pérdidas económicas ocasionadas por las enfermedades de poscosecha representan uno de los principales problemas de la citricultura mundial, siendo el 80 por ciento atribuíbles a infecciones fúngicas. El moho verde causado por Penicillium digitatum (Pers.) Sacc. (PD), es la enfermedad de mayor incidencia y severidad durante la exportación de frutos de limón. Actualmente el control de estas enfermedades se realiza con el uso de fungicidas de síntesis química. Debido a las severas restricciones impuestas a estos productos, por regulaciones ambientales y de la salud, hay una fuerte necesidad de métodos alternativos de control. El objetivo de este trabajo de tesis fue evaluar alternativas de bajo impacto ambiental : bacterias lácticas, extractos vegetales, Serenade® (Bacillus subtilis QST 713) y bicarbonato de sodio; con actividad antifúngica directa o a través de la inducción de mecanismos de defensa, para el control de PD en condiciones in vitro e in vivo (frutos de limón). De un total de 33 cepas de bacterias lácticas evaluadas, se seleccionaron ocho con propiedades antifúngicas frente a PD. Se identificaron los metabolitos antifúngicos como ácidos orgánicos (ácido láctico, ácido acético y ácido fenil láctico) y se determinó la combinación óptima con mayor actividad inhibitoria. Los productos alternativos: extractos vegetales, Serenade® y bicarbonato de sodio, presentaron actividad antifúngica in vitro a PD con porcentajes de inhibición entre 2,1 - 16 por ciento. En los frutos de limón, los tratamientos alternativos no fueron efectivos por sí solos para controlar en forma directa la enfermedad. Estos tratamientos redujeron significativamente la severidad de la enfermedad, excepto el Serenade® cuando fue aplicado simultáneamente con el inóculo. Esta reducción fue más marcada cuando se dejaron transcurrir 18 h entre inoculación y aplicación de los tratamientos. El bicarbonato de sodio al 3 por ciento y en menor medida el Serenade® al 1 por ciento indujeron una respuesta de defensa de los frutos y controlaron la enfermedad en un 96,7 por ciento y 56,7 por ciento, respectivamente. En cromatografía de capa fina y fluorometría se detectó un aumento de la fitoalexina escoparona, sugiriendo que este efecto se produciría como resultado de la inducción de mecanismos de defensa, mientras que la umbeliferona no fue detectada. Estos resultados indican que los productos biológicos actuaron como una barrera al avance de la enfermedad, retrasando la severidad de la misma e induciendo de una respuesta de defensa en los frutos.

Sistemas alternativos a los fungicidas químicos para el control de Penicillium digitatum (Pers.)Sacc. en limón

Argentina es el principal productor mundial de limones en el mundo y el 90 por ciento de esta producción se sitúa en la provincia de Tucumán. Las pérdidas económicas ocasionadas por las enfermedades de poscosecha representan uno de los principales problemas de la citricultura mundial, siendo el 80 por ciento atribuíbles a infecciones fúngicas. El moho verde causado por Penicillium digitatum (Pers.)Sacc. (PD), es la enfermedad de mayor incidencia y severidad durante la exportación de frutos de limón. Actualmente el control de estas enfermedades se realiza con el uso de fungicidas de síntesis química. Debido a las severas restricciones impuestas a estos productos, por regulaciones ambientales y de la salud, hay una fuerte necesidad de métodos alternativos de control. El objetivo de este trabajo de tesis fue evaluar alternativas de bajo impacto ambiental : bacterias lácticas, extractos vegetales, Serenade® (Bacillus subtilis QST 713)y bicarbonato de sodio; con actividad antifúngica directa o a través de la inducción de mecanismos de defensa, para el control de PD en condiciones in vitro e in vivo (frutos de limón). De un total de 33 cepas de bacterias lácticas evaluadas, se seleccionaron ocho con propiedades antifúngicas frente a PD. Se identificaron los metabolitos antifúngicos como ácidos orgánicos (ácido láctico, ácido acético y ácido fenil láctico)y se determinó la combinación óptima con mayor actividad inhibitoria. Los productos alternativos: extractos vegetales, Serenade® y bicarbonato de sodio, presentaron actividad antifúngica in vitro a PD con porcentajes de inhibición entre 2,1 - 16 por ciento. En los frutos de limón, los tratamientos alternativos no fueron efectivos por sí solos para controlar en forma directa la enfermedad. Estos tratamientos redujeron significativamente la severidad de la enfermedad, excepto el Serenade® cuando fue aplicado simultáneamente con el inóculo. Esta reducción fue más marcada cuando se dejaron transcurrir 18 h entre inoculación y aplicación de los tratamientos. El bicarbonato de sodio al 3 por ciento y en menor medida el Serenade® al 1 por ciento indujeron una respuesta de defensa de los frutos y controlaron la enfermedad en un 96,7 por ciento y 56,7 por ciento, respectivamente. En cromatografía de capa fina y fluorometría se detectó un aumento de la fitoalexina escoparona, sugiriendo que este efecto se produciría como resultado de la inducción de mecanismos de defensa, mientras que la umbeliferona no fue detectada. Estos resultados indican que los productos biológicos actuaron como una barrera al avance de la enfermedad, retrasando la severidad de la misma e induciendo de una respuesta de defensa en los frutos.

Gravity Modelling of the Crustal Structure Below Bavali Shear Zone And Adjacent Major Plutons Of Northern Kerala

The primary aim of the present study is to acquire a large amount of gravity data, to prepare gravity maps and interpret the data in terms of crustal structure below the Bavali shear zone and adjacent regions of northern Kerala. The gravity modeling is basically a tool to obtain knowledge of the subsurface extension of the exposed geological units and their structural relationship with the surroundings. The study is expected to throw light on the nature of the shear zone, crustal configuration below the high-grade granulite terrain and the tectonics operating during geological times in the region. The Bavali shear is manifested in the gravity profiles by a steep gravity gradient. The gravity models indicate that the Bavali shear coincides with steep plane that separates two contrasting crustal densities extending beyond a depth of 30 km possibly down to Moho, justifying it to be a Mantle fault. It is difficult to construct a generalized model of crustal evolution in terms of its varied manifestations using only the gravity data. However, the data constrains several aspects of crustal evolution and provides insights into some of the major events.

Collect-o-mania.

En cualquier momento y lugar,se puede recoger cualquier cosa imaginable para coleccionar: insignias, juguetes, huellas dactilares incluso el moho. Aquí hay un montón de ideas de cómo los niños pueden mostrarlas haciendo el propio museo y cómo abrirlo al público.

Una vegetación de ensueño : los mohos.

Describe cómo hacer una observación microscópica de mohos. Para ello indica los pasos a seguir: adquisición del objeto de estudio; material de laboratorio necesario para realizar la prueba; modo de hacer las preparaciones; observación microscópica de dos preparaciones para localizar las hifas, los esporangios, y el moho Penicillum. Continúa con una explicación sobre los hongos, y termina con ejercicios de aplicación de lo observado.

Caracterització de metabòlits produïts per soques de "Pseudomonas fluorescens" efectives en el control biològic de fongs fitopatògens

El principal objectiu d'aquest treball ha estat estudiar la producció de metabòlits amb activitat antibiòtica per soques de l'espècie Pseudomonas fluorescens de la col·lecció EPS, i també avaluar la seva potencialitat com a agents de biocontrol. Es va disposar també de diverses soques de P. fluorescens, cedides per altres investigadors, que van utilitzar-se com a referència perquè algunes són actives en control biològic i produeixen metabòlits secundaris d'interès en el biocontrol de malalties de plantes. La present memòria s'estructura en cinc capítols, que són, introducció al control biològic, descripció de l'etapa de selecció de soques i cerca dels metabòlits produïts, estudi de la producció d'HCN per la soca EPS288, estudi de la producció de l'antibiòtic 2,4-diacetilfloroglucinol (DAPG), i finalment, el darrer capítol, on s'ha estudiat la producció de DAPG sobre material vegetal i la capacitat de colonitzar arrels per diverses soques d'interès. En l'etapa de prospecció, va demostrar-se que un 37% del total de les soques de la col·lecció EPS produïen HCN, totes de l'espècie P. fluorescens, i un 90% d'aquestes provenien de les arrels de plantes. Es va confirmar la producció dels metabòlits secundaris 2,4-diacetilfloroglucinol, àcid fenazina-1-carboxílic, i pirrolnitrina, per diverses soques de la col·lecció EPS seleccionades mitjançant tècniques moleculars. Així, de la col·lecció EPS, les soques EPS317 i EPS808 produeixen DAPG, la EPS263 àcid fenazina-1-carboxílic i pirrolnitrina i, EPS894, EPS895, EPS945 produeixen àcid fenazina-1-carboxílic. La producció d'HCN es va estudiar més exhaustivament en la soca EPS288, seleccionada per la seva activitat antifúngica i candidata a agent de biocontrol contra Stemphylium vesicarium, causant de la estemfiliosi de la perera, i contra Penicillium expansum, causant de la podridura blava en conservació de fruita a postcollita. Per aquest estudi, es va dissenyar i validar un sistema per recollir l'HCN a partir de cultius en medi líquid. S'ha demostrat que la temperatura d'incubació, la concentració cel·lular de sembra i la composició del medi de cultiu afectaven a la producció d'HCN. Els medis complexos i la glicina n'afavorien la síntesi i la font de carboni no afectava. La soca EPS288 va produir més HCN que P. fluorescens CHA0, soca de referència productora d'HCN i descrita com a activa en processos de biocontrol de fongs fitopatògens. En l'estudi de la producció de DAPG, les soques de la col·lecció EPS i de referència, es van comparar en diversos medis de cultiu estudiant l'efecte de la complexitat i consistència del medi, i l'addició de ferro o de glucosa. Va demostrar-se que la producció de DAPG depèn principalment de la soca i de les característiques del medi de cultiu. La glucosa estimula la producció, mentre que el ferro pràcticament no afecta, i en general, el medi sòlid i complex estimula la producció de DAPG. Tanmateix, aquests efectes varien en alguna de les soques assajades donant lloc a comportaments singulars. En el seguiment del creixement amb un sistema automàtic es va comprovar que la velocitat específica de creixement i la concentració cel·lular assolida al final del cultiu, estaven condicionades per la composició del medi de cultiu. En les proves d'antagonisme vers fitopatògens que foren seleccionats com a indicadors, va observar-se que tant l'antagonisme in vitro com la inhibició d'infeccions sobre material vegetal estaven parcialment relacionades amb la producció dels metabòlits secundaris estudiats. La promoció del creixement de portaempelts per aquestes soques depenia de la soca i de l'hoste, però no es pogué establir una relació causa-efecte amb el metabòlits produïts. També es va comprovar que algunes de les soques podien sobreviure en ferides de pomes i de peres, on produïren DAPG. Mutants resistents a rifampicina de diverses soques de la col·lecció EPS i de referència es van inocular en llavors de pomera i de tomatera que es van sembrar i incubar en condicions controlades. Es va fer el seguiment de la població bacteriana total i resistent a rifampicina present a les arrels durant 72 dies. Totes les soques van colonitzar les arrels de les plantes, mantenint una elevada població durant 37 dies, cap d'elles va estimular el creixement ni mostrar efectes fitotòxics, no afectant tampoc signicativament a la població bacteriana espontània de les arrels. La soca EPS808, una de les seleccionades pel treball, va aconseguir uns nivells de producció de DAPG, una velocitat de creixement i una supervivència relativa a les arrels similar a altres soques de referència descrites com a bons agents de biocontrol. En conseqüència, se la considera una candidata a agent de biocontrol que hauria de ser objecte de futurs estudis d'eficàcia.

Deep crustal structure of the Parana Basin from receiver functions and Rayleigh-wave dispersion: Evidence for a fragmented cratonic root

The deep crustal structure of the Parana Basin of southern Brazil is investigated by analyzing P- and PP-wave receiver functions at 17 Brazilian Lithosphere Seismic Project stations within the basin. The study area can be described as a typical Paleozoic intracratonic basin that hosts one of the largest Large Igneous Province of the world and makes a unique setting for investigating models of basin subsidence and their interaction with mantle plumes. Our study consists of (1) an analysis of the Moho interaction phases in the receiver functions to obtain the thickness and bulk Vp/Vs ratio of the basin`s underlying crust and (2) a joint inversion with Rayleigh-wave dispersion velocities from an independent tomographic study to delineate the detailed S-wave velocity variation with depth. The results of our analysis reveal that Moho depths and bulk Vp/Vs ratios (including sediments) vary between 41 and 48 km and between 1.70 and 1.76, respectively, with the largest values roughly coinciding with the basin`s axis, and that S-wave velocities in the lower crust are generally below 3.8 km/s. Select sites within the basin, however, show lower crustal S-wave velocities slightly above 3.9 km/s suggestive of underplated mafic material. We show that these observations are consistent with a fragmented cratonic root under the Parana basin that defined a zone of weakness for the initial Paleozoic subsidence of the basin and which allowed localized mafic underplating of the crust along the suture zones by Cenozoic magmatism.

Estimativa de espessura crustal na Província Borborema (NE/Brasil) através de função do recpetor

Crustal thickness and VP/VS estimates are essential to the studies of subsurface geological structures and also to the understanding of the regional tectonic evolution of a given area. In this dissertation, we use the Langston´s (1979) Receiver Function Method using teleseismic events reaching the seismographic station with angles close to the vertical. In this method, the information of the geologic structures close to the station is isolated so that effects related to the instrument response and source mechanics are not present. The resulting time series obtained after the deconvolution between horizontal components contains the larger amplitude referring to the P arrival, followed by smaller arrival caused by the reverberation and conversion of the P-wave at the base of the crust. We also used the HK-Stacking after Zhu & Kanamori (2000) to obtain crustal thickness and Vp/VS estimates. This method works stacking receiver functions so that the best estimates of crustal thickness and Vp/VS are found when the direct P, the Ps wave and the first multiple are coherently stacked. We used five broadband seismographic stations distributed over the Borborema Province, NE Brazil. Crustal thickness and Vp/VS estimates are consistent with the crust-mantle interface obtained using gravity data. We also identified crutal thickening in the NW portion of the province, close to Sobral/CE. Towards the center-north portion of the province, there is an evident crustal thinning which coincides with a geological feature consisting of an alignment of sedimentary basins known as the Cariris-Potiguar trend. Towards the NE portion of the province, in Solânea/PB and Agrestina/PE regions, occurs a crustal thickening and a systematic increase in the VP/VS values which suggest the presence of mafic rocks in the lower crust also consistent with the hypothesis of underplating in the region

analise da dispersao de ondas de superficie na provincia borborema, Nordeste do Brasil

The Borborema Province, Northeastern Brazil, had its internal structure investigated by different geophysical methods like gravity, magnetics and seismics. Additionally, many geological studies were also carried out to define the structural domains of this province. Despite the plethora of studies, there are still many important open aspects about its evolution. Here, we study the velocity structure of S-wave in the crust using dispersion of surface waves. The dispersion of surface waves allows an estimate of the average thickness of the crust across the region between the stations. The inversion of the velocity structure was carried out using the inter-station dispersion of surface waves of Rayleigh and Love types. The teleseismic events are mainly from the edges of the South and North American plates. The period of data collection occurred between 2007 and 2010 and we selected 7 events with magnitude above 5.0 MW and up to 40 km depth. The difference between the events back-azimuths and the interstation path was not greater than 10. We also know the depth of the Moho, results from Receiver Functions (Novo Barbosa, 2008), and use those as constrains in inversion. Even using different parameterizations of models for the inversion, our results were very similar the mean profiles velocity structure of S-wave. In pairs of stations located in the Cear´a Central Domain Borborema the province, there are ranges of depths for which the velocities of S are very close. Most of the results in the profile near the Moho complicate their interpretation at that depth, coinciding with the geology of the region, where there are many shear zones. In particular, the profile that have the route Potiguar Bacia in inter-station, had low velocities in the crust. We combine these results to the results of gravimetry and magnetometry (Oliveira, 2008) and receptor function (Novo Barbosa, 2008). We finally, the first results on the behavior of the velocity structure of S-wave with depth in the Province Borborema

Feições crustais determinadas pela análize azimutal da função do receptor, na região da estação sismológica de Rio Claro (RCLB)

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Inversão de dados de ondas de superfície Rayleigh

Neste trabalho compilamos informações sobre um grande número de medidas de velocidade de grupo para ondas Rayleigh do modo fundamental, com período até 100 segundos. Tais dados consistiram de informações retiradas da literatura geofísica e cobriram toda a Terra. Parte dos dados foi organizada em trabalhos anteriores e uma segunda parte foi apresentada aqui de forma inédita. Para a América do Sul, selecionamos os principais conjuntos de dados de tais ondas e elaboramos diversos perfis onde a distribuição de velocidade de ondas cisalhantes foi obtida a partir da inversão das curvas de dispersão de velocidade de grupo. Tais perfis serviram para termos uma ideia inicial da estrutura interna da Terra em nosso continente. Com o conjunto global de dados de velocidade de grupo foi possível obtermos os mapas de distribuição lateral de valores de velocidade para cada período referencial entre 20 e 100 segundos. Tais mapas foram produzidos da mesma forma que os mapas de velocidade de fase de ROSA (1986), onde a amostragem for para realizada para blocas medindo 10x10 graus, englobando toda a Terra, em projeção mercator. O valor de velocidade de grupo em cada bloco, para cada período, foi obtido a partir da inversão estocástica dos dados de anomalia de velocidade em relação aos modelos regionalizados de JORDAN (1981) com os valores de velocidade de grupo de ROSA et al. (1992). Os mapas de velocidade de grupo obtidos aqui foram então empregados, na América do Sul, com os valores de velocidade de fase dos mapas obtidos por ROSA (1986). Assim, foi possível determinarmos, em profundidade, os mapas de variação de velocidade de onda cisalhante e os mapas de distribuição de valores de densidade. Com isto, pudemos construir o primeiro mapa de profundidade do Moho (todo do Manto Superior) da América do Sul.

Mapeamento de uma interface separando dois meios homogêneos através da reconstituição gravimétrica compacta: aplicação a dados do LEPLAC-IV

O problema do mapeamento de uma interface separando dois meios homogêneos tem sido tradicionalmente resolvido através da continuação para baixo da anomalia gravimétrica observada. Este procedimento requer a utilização de um filtro passa-baixa ou de um parâmetro de amortecimento, que tendem a diminuir a resolução do relevo estimado da interface. Além disso, o uso da continuação para baixo implica supor (desnecessariamente) que a interface é uma superfície harmônica. Desta forma, a utilização da continuação para baixo é restrita a interfaces que apresentam um relevo suave relativamente à sua profundidade média. As restrições impostas pela continuação para baixo do campo gravimétrico são reduzidas na técnica de inversão proposta para este estudo, cujo objetivo é mapear a interface crosta-manto baseada na incorporação de informações a priori sobre o mínimo momento de inércia da fonte causadora, em relação a um eixo de concentração de massa pré-estabelecido e coincidente com o topo da fonte anômala. Além da introdução de informações sobre o mínimo momento, foi incluída também a possibilidade de haver variação lateral e em profundidade de densidade em setores previamente estabelecidos, o que permite estender a aplicação desta técnica a situações geológicas mais complexas que envolvam a reconstituição de corpos justapostos, que sejam de diferentes naturezas, tais como aqueles presentes em zonas de transição crustal. O método de inversão apresentado foi avaliado em testes usando dados sintéticos e os resultados obtidos mostraram a eficiência desta técnica em recuperar corpos alongados horizontalmente, que apresentem como topo ou base, interfaces arbitrárias a serem mapeadas. Foi também constatada a eficácia do método em reconstituir corpos que comportem variação lateral de densidade que pudessem retratar situações em que se deseja investigar a natureza do embasamento em regiões de transição crustal. Com base nos resultados destes testes, a técnica foi então empregada na inversão gravimétrica de cinco perfis do LEPLAC IV que cruzam a região oceânica adjacente à margem continental sudeste brasileira. Os resultados desta aplicação permitiram inferir a natureza dos corpos que constituem o arcabouço estrutural da região onde encontram-se inseridas a Dorsal de São Paulo e a Zona de Fratura de Porto Alegre, assim como mapear a Moho subjacente.