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Thèses sur le sujet « Seismology »

Auteur : Grafiati

Publié le 4 juin 2021

Mis à jour le 25 juillet 2025

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1

Suryanto, Wiwit. "Rotational Motions in Seismology." Diss., lmu, 2006. http://nbn-resolving.de/urn:nbn:de:bvb:19-78505.

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2

Herrmann, Felix J. "Seismology meets compressive sampling." Institute for Pure & Applied Mathematics. University of California, Los Angeles, 2007. http://hdl.handle.net/2429/603.

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3

Krüger, Frank, Matthias Ohrnberger, and Dirk Rößler. "Rupture imaging of large earthquakes with a poststack isochrone migration method." Universität Potsdam, 2008. http://opus.kobv.de/ubp/volltexte/2008/1839/.

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Rapid and robust characterization of large earthquakes in terms of their spatial extent and temporal duration is of high importance for disaster mitigation and early warning applications. Backtracking of seismic P-waves was successfully used by several authors to image the rupture process of the great Sumatra earthquake (26.12.2004) using short period and broadband arrays. We follow here an approach of Walker et al. to backtrack and stack broadband waveforms from global network stations using traveltimes for a global Earth model to obtain the overall spatio-temporal development of the energy r

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4

Valle, G. Raul del. "Model parameterization in refraction seismology." Thesis, McGill University, 1986. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=66057.

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5

Suzuki, Osamu 1968. "Reflection seismology for nondestructive evaluation." Thesis, Massachusetts Institute of Technology, 2002. http://hdl.handle.net/1721.1/84812.

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6

Mosher, Stephen Glenn. "Neural Network Applications in Seismology." Thesis, Université d'Ottawa / University of Ottawa, 2021. http://hdl.handle.net/10393/42329.

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Neural networks are extremely versatile tools, as evidenced by their widespread adoption into many ﬁelds in the sciences and beyond, including the geosciences. In seismology neural networks have been primarily used to automatically detect and discriminate seismic signals within time-series data, as well as provide location estimates for their sources. However, as neural network research has signiﬁcantly progressed over the past three decades, so too have its applications in seismology. Such applications now include earthquake early warning systems based on smartphone data collected from large

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7

Monteiro, Mario Joao Pires Fernandes Garcia. "Seismology of the solar convection zone." Thesis, Queen Mary, University of London, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.362457.

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8

Caiado, Camila Carneiro Da S. "Bayesian methods applied to reflection seismology." Thesis, Durham University, 2012. http://etheses.dur.ac.uk/3388/.

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Quantifying uncertainty in models derived from observed seismic data is an important issue in exploration geophysics. In this research we examine the geological structure of the subsurface of the Earth using controlled source seismology which consists of data recorded in time and the distance between acoustic sources and receivers. There are a number of inversion tools to map data into depth models, but a full exploration of the uncertainty of such models is rarely done because of the lack of robust strategies available for the analysis of large non-linear complex systems. In reflection seismo

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9

Entwistle, Elizabeth. "Retrospective seismology by source-receiver interferometry." Thesis, University of Edinburgh, 2015. http://hdl.handle.net/1842/10457.

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Seismology is the study of earthquakes and the Earth’s internal structure using seismic waves. Traditional seismology is constrained by the timing and location of seismic sources, and by the location of seismometers with which energy from the sources are recorded. Improvements in the global seismometer networks have reduced the latter constraint. Furthermore, recent advances into Seismic Interferometry (SI) have enabled detailed information about the Earth’s interior to be obtained using ambient seismic noise, hence even in areas with low natural seismicity. The most common approach to SI is t

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10

Pham, Nguyen-Dinh. "Rotational motions in seismology : theory, observation, modeling." kostenfrei, 2009. http://edoc.ub.uni-muenchen.de/10801/.

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11

Pham, Nguyen Dinh. "Rotational Motions in Seismology: Theory, Observation, Modeling." Diss., lmu, 2009. http://nbn-resolving.de/urn:nbn:de:bvb:19-108013.

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12

Deuss, A. F. "Theoretical and observational studies in global seismology." Thesis, University of Oxford, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.270362.

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13

Al-Attar, David. "Theoretical problems in global seismology and geodynamics." Thesis, University of Oxford, 2011. http://ora.ox.ac.uk/objects/uuid:e700e8df-49d0-47e0-8929-cd254c5416c1.

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In Chapter 2, we consider the hydrostatic equilibrium figure of a rotating earth model with arbitrary radial density profile. We derive an exact non-linear partial differential equation describing the equilibrium figure. Perturbation theory is used to obtain approximate forms of this equation, and we show that the first-order theory is equivalent to Clairaut's equation. In Chapter 3, a method for parametrizing the possible equilibrium stress fields of a laterally heterogeneous earth model is described. In this method a solution of the equilibrium equations is first found that satisfies some de

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14

Craig, Timothy James. "Constraints on lithosphere rheology from earthquake seismology." Thesis, University of Cambridge, 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.648303.

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15

Krüger, Christian. "Seismology of adolescent general relativistic neutron stars." Thesis, University of Southampton, 2015. https://eprints.soton.ac.uk/384187/.

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16

Wagner, Lara Suzanne. "Investigations of Upper Mantle Structure using Broadband Seismology." Diss., Tucson, Arizona : University of Arizona, 2005. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu%5Fetd%5F1204%5F1%5Fm.pdf&type=application/pdf.

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17

Alberts, Ernst Patrick. "Horizon mapping in exploration seismology using artficial intelligence." Thesis, Imperial College London, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.272160.

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18

Williamson, P. R. "Tomographic inversion of traveltime data in reflection seismology." Thesis, University of Cambridge, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.383956.

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19

Willemsen, Lucas Abraham. "Problems with a localized nature in exploration seismology." Thesis, Massachusetts Institute of Technology, 2017. http://hdl.handle.net/1721.1/108840.

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Thesis: Ph. D. in Geophysics, Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2017.<br>This electronic version was submitted by the student author. The certified thesis is available in the Institute Archives and Special Collections.<br>Cataloged from student-submitted PDF version of thesis.<br>Includes bibliographical references (pages 267-274).<br>A wide range of problems in seismology have a localized nature. Examples include inversion for time-lapse change, salt boundary position and Amplitude or Phase Versus Angle (AVA/PVA). With increasing

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20

Callor, Nickolas Brenten. "Coordinated Persistent Homology and an Application to Seismology." BYU ScholarsArchive, 2019. https://scholarsarchive.byu.edu/etd/9115.

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The theory of persistent homology (PH), introduced by Edelsbrunner, Letscher, and Zomorodian in [1], provides a framework for extracting topological information from experimental data. This framework was then expanded by Carlsson and Zomorodian in [2] to allow for multiple parameters of analysis with the theory of multidimensional persistent homology (MPH). This particular generalization is considerably more difficult to compute and to apply than its predecessor. We introduce an intermediate theory, coordinated persistent homology (CPH), that allows for multiple parameters while still preservi

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21

Ross, Christopher P. "AVO limitations near salt structures." Diss., Georgia Institute of Technology, 1992. http://hdl.handle.net/1853/31010.

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22

Jones, Ian Frederick. "Applications of the Karhunen-Loève transform in reflection seismology." Thesis, University of British Columbia, 1985. http://hdl.handle.net/2429/25831.

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The Karhunen-Loève transform, which optimally extracts coherent information from multichannel data, has been applied to several problems in reflection seismic data processing. The transform is derived by a least-squares construction of an orthogonal set of principal components and eigenvectors, with corresponding eigenvalues. Data are reconstructed as a linear combination of the principal components. The mathematical properties of the Karhunen-Loève transform which render it applicable to problems in seismic data processing are reviewed, and a number of new algorithms developed. Most algorith

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23

Douglas, John. "A critical reappraisal of some problems in engineering seismology." Thesis, Imperial College London, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.404768.

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24

Dymova, Maria V. "Coronal seismology : novel approach of exploring the solar atmosphere." Thesis, University of Sheffield, 2006. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.434541.

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25

Quinn, Rory. "Marine high-resolution reflection seismology : acquisition, processing and applications." Thesis, University of Southampton, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.243092.

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26

Cinella, Jacqueline Rose. "A Cellular Seismology Investigation of the Caribbean Plate Region." Thesis, Boston College, 2014. http://hdl.handle.net/2345/3817.

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Thesis advisor: Alan L. Kafka<br>A CELLULAR SEISMOLOGY INVESTIGATION OF THE CARIBBEAN PLATE REGION Jacqueline Rose Cinella Dr. Alan Kafka, thesis advisor The Caribbean Plate region (CPR) provides a natural laboratory for a Cellular Seismology (CS) investigation due to its diversity of plate boundaries and the associated seismotectonic environments. Study of the CPR is of interest due, in part, to the occurrence of devastating earthquakes, such as the 2010 earthquake in Haiti. Using data from this region, this study addresses fundamental questions about CS forecasts: to what extent do the time

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27

Ely, Gregory Tsiang. "Applications of a fast helmholtz solver in exploration seismology." Thesis, Massachusetts Institute of Technology, 2019. https://hdl.handle.net/1721.1/121757.

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Thesis: Ph. D., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2019<br>Cataloged from PDF version of thesis.<br>Includes bibliographical references (pages 141-150).<br>Seismic imaging techniques rely on a velocity model inverted from noisy data via a non-linear inverse problem. This inferred velocity model may be inaccurate and lead to incorrect interpretations of the subsurface. In this thesis, I combine a fast Helmholtz solver, the field expansion method, with a reduced velocity model parameterization to address the impact of an uncertain or

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28

Hanson, Jeffrey Acton. "Seismic and hydroacoustic investigations near Ascension Island /." Diss., Connect to a 24 p. preview or request complete full text in PDF format. Access restricted to UC campuses, 1998. http://wwwlib.umi.com/cr/ucsd/fullcit?p9823701.

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29

Fisher, Steven Wolf. "Effects of magnitude, depth, and time on Cellular Seismology Forecasts." Thesis, Boston College, 2013. http://hdl.handle.net/2345/3031.

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Thesis advisor: Alan L. Kafka<br>This study finds that, in most cases analyzed to date, past seismicity tends to delineate zones where future earthquakes are likely to occur. Network seismicity catalogs for the New Madrid Seismic Zone (NMSZ), Australia (AUS), California (CA), and Alaska (AK) are analyzed using modified versions of the Cellular Seismology (CS) method of Kafka (2002, 2007). The percentage of later occurring earthquakes located near earlier occurring earthquakes typically exceeds the expected percentage for randomly distributed later occurring earthquakes, and the specific percen

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30

Lenham, Joseph. "High resolution seismology, archaeology and submerged landscapes : an interdisciplinary study." Thesis, University of Southampton, 2000. https://eprints.soton.ac.uk/42130/.

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Archaeological investigation of the shallow coastal environment has traditionally been conducted through exclusively marine or terrestrial methods, creating artificial division between sites located in the intertidal and subtidal zones. This thesis demonstrates a successful seamless inter-disciplinary survey methodology, utilising side scan sonar, sub-bottom profilers, aerial photography and archaeological field inspection to establish the correct spatial and contextual relationships of submerged archaeological structures. To facilitate survey of the shallow intertidal zone, a novel catamaran-

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31

Brodsky, Emily Elizabeth Gurnis Michael. "Studies in fluid dynamics as applied to seismology and volcanology /." Diss., Pasadena, Calif. : California Institute of Technology, 2001. http://resolver.caltech.edu/CaltechETD:etd-08152001-152200.

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32

Rößler, Dirk, Frank Krüger, and Matthias Ohrnberger. "Automatic near real-time characterisation of large earthquakes." Universität Potsdam, 2008. http://opus.kobv.de/ubp/volltexte/2008/1838/.

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We use seismic array methods (semblance analysis) to image areas of seismic energy release in the Sunda Arc region and world-wide. Broadband seismograms at teleseismic distances (30° ≤ Δ ≤ 100°) are compared at several subarrays. Semblance maps of different subarrays are multiplied. High semblance tracked over long time (10s of second to minutes) and long distances indicate locations of earthquakes. The method allows resolution of rupture characteristics important for tsunami early warning: start and duration, velocity and direction, length and area. The method has been successfully applied to

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33

Scott, James B. "Seismic noise in the shallow subsurface methods for using it in earthquake hazard assessment /." abstract and full text PDF (free order & download UNR users only), 2007. http://0-gateway.proquest.com.innopac.library.unr.edu/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:3258847.

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34

Assimaki, Dominic 1975. "Topography effects in the 1999 Athens earthquake : engineering issues in seismology." Thesis, Massachusetts Institute of Technology, 2004. http://hdl.handle.net/1721.1/30048.

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Thesis (Sc. D.)--Massachusetts Institute of Technology, Dept. of Civil and Environmental Engineering, 2004.<br>Includes bibliographical references.<br>It is well known that irregular topography can substantially affect the amplitude and frequency characteristics of seismic motion. Macroseismic observations of destructive earthquakes often show higher damage intensity at the tops of hills, ridges and canyons than at lower elevations and on flat areas. Systematic seismic motion amplification over convex topographies has been confirmed by instrumental studies and also predicted by theoretical and

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35

Sharrock, David Stuart. "Structure and heterogeneity of the Earth's mantle from broadband earthquake seismology." Thesis, University of Edinburgh, 1995. http://hdl.handle.net/1842/12920.

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Attenuation of seismic energy is often seen as an unavoidable 'problem' in earthquake seismology. Observation of earthquakes at teleseismic distances is severely limited by the signal-to-noise ratio of the recording seismograph. However, the underlying mechanisms behind seismic attenuation are very different to those underlying other parameters and seismic attenuation can yield information on the structure of the Earth different to that obtained from, for example, seismic wave speed studies. In this study, 59 globally-distributed earthquakes and explosions, recorded at the four UK-type arrays

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36

Tinker, Mark Andrew 1968. "Broadband seismology and the detection and verification of underground nuclear explosions." Diss., The University of Arizona, 1997. http://hdl.handle.net/10150/282322.

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On September 24, 1996, President Clinton signed the Comprehensive Test Ban Treaty (CTBT), which bans the testing of all nuclear weapons thereby limiting their future development. Seismology is the primary tool used for the detection and identification of underground explosions and thus, will play a key role in monitoring a CTBT. The detection and identification of low yield explosions requires seismic stations at regional distances (1500 km). However, because the regional wavefield propagates within the extremely heterogeneous crustal waveguide, the seismic waveforms are also very complicated.

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37

Cambiotti, G. "MODELLING THE EARTH: COMPRESSIBLE VISCOELASTODYNAMICS, GRAVITATIONAL SEISMOLOGY AND TRUE POLAR WANDER." Doctoral thesis, Università degli Studi di Milano, 2012. http://hdl.handle.net/2434/169994.

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This thesis reviews and sheds new light on compressible Earth models and theories for the modelling of megathrust earthquakes and rotational instabilities caused by glacial isostatic adjustments and mantle convection. The basic theory is outlined in the first chapter, where we discuss the response of a self-gravitating Earth to external forces and loads seated at its surface or interior and we focus on elastic static perturbations and the transition between the elastic and fluid behaviours of the Earth that occurs on thousand and million years time scales. In the first part of this the

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38

Nichols, Andrew M. "Lessons learned from dynamic analyses of Mexico City and applied to Richmond B.C." Thesis, University of British Columbia, 1987. http://hdl.handle.net/2429/42004.

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The implications of the acceleration data recorded during the September 19, 1985 Mexican earthquake for seismic design in Canada are investigated by determining if the deep deposits of the Fraser Delta could cause large amplification of earthquake motions. The conditions for amplification of low level incoming ground motions at deep sites are identified; in particular, the critical role of variation in shear modulus with shear strain. The current procedure for determining site specific ground motions is evaluated and major sources of uncertainty in the results identified. Criteria for

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39

Buckner, Jesse Conard. "Crustal Structure in a Mesozoic Extensional Terrane: The South Georgia Rift and the Epicentral Area of the 1886 Charleston, South Carolina, Earthquake." Thesis, Virginia Tech, 2011. http://hdl.handle.net/10919/31210.

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On August 31, 1886 a large scale earthquake occurred in Summerville, S.C. causing severe damage in the coastal city of Charleston. Although intensive geological and geophysical studies have been conducted in the area, uncertainty remains about the details of the event. Recently evidence from seismic reflection profiles have shed light on the tectonic environment of the area. The epicentral area of the 1886 event lies within the South Georgia Rift, a Mesozoic rift terrane. Previous studies have revealed clues to the geologic structure and evolution of this feature. SEISDATA4 is the largest sei

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40

Davison, Frederick C. "Stress tensor estimates derived from focal mechanism solutions of sparse data sets: applications to seismic zones in Virginia and eastern Tennessee." Diss., Virginia Polytechnic Institute and State University, 1988. http://hdl.handle.net/10919/53686.

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A technique has been developed to estimate the directions of principal stresses from focal mechanism solutions, under the assumption that the stress is homogeneous throughout the seismic zone. That method is called the Multiple Solution per Earthquake Technique (MSET), and utilizes each member of multiple focal mechanism solution set as a possible solution. The MSET is useful when applied to small data sets, and differs from existing techniques in that (1) the use of multiple focal mechanisms for individual earthquakes allows for a range in the possible orientation of the fault geometry, while

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41

Lee, Cho-min. "The tectonic framework of Hong Kong and vicinity and its relationship to regional seismicity /." [Hong Kong] : University of Hong Kong, 1990. http://sunzi.lib.hku.hk/hkuto/record.jsp?B13122368.

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42

Liu, Enru. "Shear-wave splitting in cross-hole seismology and channel waves in anisotropic waveguides." Thesis, University of Edinburgh, 1989. http://hdl.handle.net/1842/12439.

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43

Mercier, Jean-Philippe. "Improved teleseismic Green's functions and western Canada mantle structure and evolution." Thesis, University of British Columbia, 2008. http://hdl.handle.net/2429/2779.

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The present thesis is divided into three distinct parts and focuses both on the improvement of deconvolution technique in a teleseismic context for crustal and upper-mantle studies and on the understanding of western Canada structure and evolution through seismic imaging. The first part presents estimates of the P-component of the teleseismic-P Green's functions for three stations of the Canadian National Seismic Network (CNSN) obtained using a new deconvolution technique. Our results show evidence of the principal, first-order scattered Moho phases and, in particular, the Pp_Mp. The second pa

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44

Billington, Edward Davis. "Spatial and temporal seismicity variations in the South Sandwich and Northwestern South American subduction." Thesis, Georgia Institute of Technology, 1986. http://hdl.handle.net/1853/25950.

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45

Zheng, York Yao. "Time-lapse seismic imaging using elastic full waveform inversion of ocean-bottom cable data." Thesis, University of Cambridge, 2014. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.648657.

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46

Blazek, Kirk. "The one-dimensional inverse problem of reflection seismology on a viscoacoustic medium /." Thesis, Connect to this title online; UW restricted, 2006. http://hdl.handle.net/1773/5725.

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47

Gorman, Andrew Robert. "Deep Probe, investigating the lithosphere of western North America with refraction seismology." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2001. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/NQ61096.pdf.

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48

Black, Jennifer Anne. "Structure of the deep Earth using array seismology and core seismic phases." Thesis, University of Liverpool, 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.440753.

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49

Petrescu, Laura. "Precambrian lithospheric structure and evolution : evidence from broadband seismology in Eastern Canada." Thesis, Imperial College London, 2017. http://hdl.handle.net/10044/1/52450.

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The thick and seismically fast Precambrian continental remnants (cratons) provide fundamental clues about the tectonic processes that operated on the early Earth. Eastern Canada is a natural laboratory to study such processes: its geological record spans more than 3 Ga of Earth history, including the assembly of the largest Archean craton in the world, the Superior craton, which is surrounded by global scale Proterozoic and Phanerozoic orogenic belts. To investigate the crustal and lithospheric structure of eastern Canada, earthquake data recorded at a new broadband seismic network were analys

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50

Scott, Patricia Frances. "Applications of the Kirchhoff-Helmholtz Integral to Problems in Body Wave Seismology." Diss., Pasadena, Calif. : California Institute of Technology, 1985. http://resolver.caltech.edu/CaltechETD:etd-06062005-132701.

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