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Dissertations / Theses on the topic 'Teleseism'

Author: Grafiati

Published: 10 March 2023

Last updated: 19 July 2025

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1

Pucciarelli, Giuseppe. "Seismic tomography of Italy (with special regard to Southern Tyrrhenian)." Doctoral thesis, Universita degli studi di Salerno, 2017. http://hdl.handle.net/10556/2569.

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2015 - 2016<br>The topic of my PhD thesis is a seismic tomography which has as object of investigation Italy, particularly Southern Italy and Southern Tyrrhenian. This tomography has been obtained by means of inversion of teleseismic data. Seismic tomography is a method of investigation which is considerably stabilized in the field of Geophysics. Its goal is the achievement of a tridimensional velocity model of a subsoil of a determined area. For reaching this aim, it is necessary to gather arrival times of seismic events registered by seismic stations that are distributed in an opportu

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2

Burdick, Scott A. (Scott Anthony). "Teleseismic transmission and reflection tomography." Thesis, Massachusetts Institute of Technology, 2014. http://hdl.handle.net/1721.1/87516.

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Thesis: Ph. D. in Geophysics, Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2014.<br>Cataloged from PDF version of thesis.<br>Includes bibliographical references.<br>The aim of seismic tomography is to determine a model of Earth properties that best explain observed seismic data. In practice, the limitations placed on our observations and computational capabilities force us to make a number of decisions about the scales and parameterizations of models, the nature of the data considered, and the approximations to wave propagation that connect t

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3

Henry, Chris. "Teleseismic studies of large submarine earthquakes." Thesis, University of Oxford, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.249590.

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4

Foley, John Edward. "Crustal structure from teleseismic bodywave data." Thesis, Massachusetts Institute of Technology, 1990. http://hdl.handle.net/1721.1/52914.

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Thesis (Sc.D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 1990.<br>Includes bibliographical references (leaves 245-255).<br>by John Edward Foley.<br>Sc.D.

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5

Snowden, Conor B. "The complexity of teleseismic P-waves." Thesis, University of Edinburgh, 2003. http://hdl.handle.net/1842/11422.

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Complex short-period teleseismic P-waveforms (consisting of the direct P wave and surface reflections pP and sP) are observed from many earthquake sources. It is often not possible to easily interpret these waveforms in terms of those three phases. This is necessary to obtain accurate earthquake depths and P and S wave radiation patterns. This thesis examines the contribution made by various factors to P-wave seismogram complexity using both synthetic and real data. First, using a number of synthetic waveforms it is confirmed that long duration sources can contribute significantly to the compl

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6

Sargeant, Susanne. "Modelling shallow earthquakes with teleseismic broadband data." Thesis, University of East Anglia, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.251561.

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7

Ihmle, Pierre Frédéric. "Teleseismic study of rupture processes with long duration." Thesis, Massachusetts Institute of Technology, 1994. http://hdl.handle.net/1721.1/54395.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 1994.<br>Includes bibliographical references (p. 229-238).<br>by Pierre Frédéric Ihmle.<br>Ph.D.

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8

Eken, Tuna. "Isotropic and Anisotropic P and S Velocities of the Baltic Shield Mantle : Results from Analyses of Teleseismic Body Waves." Doctoral thesis, Uppsala universitet, Geofysik, 2009. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-102501.

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The upper mantle structure of Swedish part of Baltic Shield with its isotropic and anisotropic seismic velocity characteristics is investigated using telesesismic body waves (i.e. P waves and shear waves) recorded by the Swedish National Seismological Network (SNSN). Nonlinear high-resolution P and SV and SH wave isotropic tomographic inversions reveal velocity perturbations of ± 3 % down to at least 470 km below the network. Separate SV and SV models indicate several consistent major features, many of which are also consistent with P-wave results. A direct cell by cell comparison of SH and SV

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9

Letort, Jean. "Méthodes télésismiques d'estimation de la profondeur des séismes : développements et applications." Thesis, Grenoble, 2014. http://www.theses.fr/2014GRENU016/document.

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Cette thèse traite de l'étude de la profondeur des séismes modérés (4 < M < 5.5), à travers l'utilisation de données telesismiques, c'est à dire à partir d'enregistrements de sismographes situes a des distances de 3000 jusqu'à 9000 km de la source. L'estimation de la profondeur d'un séisme s'obtient en comparant les temps d'arrivée de l'onde directe (P) générée par ce séisme, avec ceux des ondes réfléchies sur la surface de la Terre, au-dessus du foyer du séisme (les phases de profondeur pP, sP). Nous utilisons le réseau du CTBTO (Comprehensive Test-Ban-Treaty-Organization, composé de mi

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10

Jiang, Wei Ping. "Determination of crustal velocity structures from teleseismic p waves." Thesis, Georgia Institute of Technology, 1989. http://hdl.handle.net/1853/25773.

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11

Morice, Stephen Patrick. "A receiver function study in the Peloponnese, Greece." Thesis, University of Cambridge, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.264508.

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12

Lipke, Katrin, Max Zitzmann, Manuel Amberger, et al. "Traveltime residuals at regional and teleseismic distances for SE-Asia." Universität Potsdam, 2007. http://opus.kobv.de/ubp/volltexte/2007/1411/.

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Traveltime residuals for worldwide seismic stations are calculated. We use P and S waves from earthquakes in SE-Asia at teleseismic and regional distances. The obtained station residuals help to enhance earthquake localisation. Furthermore we calculated regional source dependent station residuals. They show a systematic dependence of the locality of the source. These source dependent residuals reflect heterogenities along the path and can be used for a refinement of earthquake localisation.<br>Laufzeitresiduen für weltweite seismische Stationen werden berechnet. Wir nutzen P - und S-Wellen vo

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13

Baker, Benjamin Ian. "2.5d teleseismic waveform tomography with application to the tien shan." Thesis, Rensselaer Polytechnic Institute, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=3613267.

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<p> The analysis of passive source seismic data recorded by quasi-linear deployments of broadband stations at teleseismic distances has proven to be an effective means of probing the subsurface of the Earth. However, current methodologies are far from being able to exploit all the interpretable signal in these data sets. In this thesis, I describe a 2.5D, frequency domain, visco-elastic waveform tomography algorithm for imaging with this type of data. To compute synthetic seismograms (the forward problem), the general equations of motion are discretized with p-adaptive finite elements. This ap

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14

Yu, Chunquan Ph D. Massachusetts Institute of Technology. "Imaging of crust and mantle structures with teleseismic reflected waves." Thesis, Massachusetts Institute of Technology, 2016. http://hdl.handle.net/1721.1/104597.

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Thesis: Ph. D., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2016.<br>Cataloged from PDF version of thesis.<br>Includes bibliographical references.<br>In this thesis, we developed and applied seismic imaging methods based on teleseismic reflected waves to study discontinuities in the crust and mantle. Specifically, we further developed virtual deep seismic sounding (VDSS) to probe the Moho and we used SS precursors to study mantle transition zone discontinuities. To extend the applicability of VDSS, we developed a source deconvolution scheme

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15

Scire, Alissa. "Imaging Variations in the Central Andean Mantle and the Subducting Nazca Slab with Teleseismic Tomography." Diss., The University of Arizona, 2015. http://hdl.handle.net/10150/556487.

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The Nazca-South America convergent margin is marked by the presence of the Andean mountain belt, which stretches along the 8000-km long western margin of the South American plate. The subduction zone is characterized by significant along-strike changes in both upper plate structure and slab geometry that make it an ideal region to study the relationship between the subducting slab, the surrounding mantle, and the overriding plate. This dissertation summarizes the results of three finite frequency teleseismic tomography studies of the central Nazca-South America subduction zone which improve ou

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16

Fan, Chengliang. "Extracting P-primary transmission and reflection impulse responses from teleseismic data." [Bloomington, Ind.] : Indiana University, 2005. http://gateway.proquest.com/openurl?url_ver=Z39.88-2004&res_dat=xri:pqdiss&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&rft_dat=xri:pqdiss:3199414.

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Thesis (Ph.D.)--Indiana University, Dept. of Geological Sciences, 2005.<br>Source: Dissertation Abstracts International, Volume: 66-11, Section: B, page: 5867. Adviser: Gary L. Pavlis. Title from dissertation home page (viewed Oct. 11, 2006).

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17

Condori, Cristobal, George S. França, Hernando J. Tavera, Diogo F. Albuquerque, Brandon T. Bishop, and Susan L. Beck. "Crustal structure of north Peru from analysis of teleseismic receiver functions." PERGAMON-ELSEVIER SCIENCE LTD, 2017. http://hdl.handle.net/10150/625974.

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In this study, we present results from teleseismic receiver functions, in order to investigate the crustal thickness and Vp/Vs ratio beneath northern Peru. A total number of 981 receiver functions were analyzed, from data recorded by 28 broadband seismic stations from the Peruvian permanent seismic network, the regional temporary SisNort network and one CTBTO station. The Moho depth and average crustal Vp/Vs ratio were determined at each station using the H-k stacking technique to identify the arrival times of primary P to S conversion and crustal reverberations (PpPms, PpSs + PsPms). The resu

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18

Ashoori, Pareshkoohi Azadeh. "Lithospheric Structure Across the Northern Canadian Cordillera from Teleseismic Receiver Functions." Thesis, Université d'Ottawa / University of Ottawa, 2016. http://hdl.handle.net/10393/35535.

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A major change in seismic velocities between Earth’s crust and mantle is known as the Mohorovicic discontinuity (Moho). The depth of the Moho plays an important role in characterizing the overall structure of the crust and can be related to the tectonic setting of a region. Teleseismic P-wave receiver function techniques can provide estimates of the depth of the Moho and therefore crustal thickness under a broadband station. In this research we are interested in the structure of the crust and mantle across the northern Canadian cordillera, described by various tectonic settings. The teleseismi

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19

Rondenay, Stéphane. "Teleseismic imaging of the southeastern Canadian Shield and Cascadia subduction zone." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2001. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/NQ61166.pdf.

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20

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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21

Marson-Pidgeon, Katrina Ann, and katrina marson-pidgeon@anu edu au. "Seismogram synthesis for teleseismic events with application to source and structural studies." The Australian National University. Research School of Earth Sciences, 2001. http://thesis.anu.edu.au./public/adt-ANU20010925.152548.

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The aim of this thesis is to develop procedures for the modelling and inversion of teleseismic P and S waveforms which are as flexible as possible. This flexibility is necessary in order to obtain accurate source depth and mechanism estimates for small to moderate size events, such as those that are relevant in the context of monitoring the Comprehensive Nuclear-Test-Ban Treaty (CTBT). ¶ The main challenge for extending source depth and mechanism inversion methods to smaller events is to ensure that sufficiently accurate synthetic seismograms are available for comparison with observed records.

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22

Shomali, Z. Hossein. "Dynamic Source Models of Icelandic Earthquakes and Teleseismic Tomograhy along the TOR array." Doctoral thesis, Uppsala University, Department of Earth Sciences, 2001. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-1451.

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<p>This thesis describes new inversion-oriented methodological developments and their seismological applications. In the first study presented the dynamic source parameters of some local Icelandic earthquakes are studied by employing a time domain moment tensor inversion method. A windowing method for direct P and S phases was used and the inversion was performed for frequencies lower than the associated corner frequency under the double-couple constraint. The inversion algorithm could determine the dynamic source parameters correctly, even under conditions of poor azimuthal coverage. The seco

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23

Shomali, Z. Hossein. "Dynamic source models of Icelandic earthquakes and teleseismic tomography along the TOR array /." Uppsala : Acta Universitatis Upsaliensis : Univ.-bibl. [distributör], 2001. http://publications.uu.se/theses/91-554-5098-9/.

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24

Tomlinson, James Peter. "A teleseismic receiver function study of the crustal structure of the British Isles." Thesis, University of Leicester, 2003. http://hdl.handle.net/2381/30454.

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The onshore crustal and upper mantle velocity structure of the British Isles has been investigated by teleseismic receiver function analysis. The results of the study augment the dense offshore and sparse onshore models of the structure beneath the area. In total almost 1500 receiver functions have been analysed, which have been calculated using teleseismic data from 34 broadband and short-period, three-component seismic recording instruments. The crustal structure has primarily been investigated using 1D grid search and forward modelling techniques, returning crustal thicknesses, bulk crystal

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25

Corradini, Marina. "Reconstruction of the earthquake rupture process through coherent teleseismic imaging and statistical modeling." Thesis, Université de Paris (2019-....), 2019. https://theses.md.univ-paris-diderot.fr/CORRADINI_Marina_va1.pdf.

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De nombreuses études ont tenté d’éclairer la complexité de la rupture sismique de grands séismes en utilisant des techniques d’imagerie cohérente telles que la back- projection (BP). Dans une étude récente, Fukahata et al. (2013) ont suggéré que, d’un point de vue théorique, l’image BP de la rupture sismique est liée au glissement ou à la vitesse de glissement sur la faille. Cependant, la relation quantitative entre les images BP et les propriétés physiques du processus de rupture reste encore peu connue. Cette thèse vise à clarifier comment les images BP du champ d’ondes rayonné peuvent être

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26

Adams, David C. 1952. "Effects of noise on teleseismic T* estimation and attenuation tomography of the Yellowstone region." Thesis, University of Oregon, 2009. http://hdl.handle.net/1794/10368.

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xv, 108 p. : ill. (some col.) A print copy of this thesis is available through the UO Libraries. Search the library catalog for the location and call number.<br>Studies on seismic attenuation are an important complement to those on seismic velocity, especially when interpreting results in terms of temperature. But estimation of attenuation (t*) is more computationally involved and prone to contamination by noise, especially signal-generated noise. We have examined the effects of various forms of synthetic noise on t* estimation using time and frequency domain methods with varying window lengt

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27

Arlitt, Robert. "Teleseismic body wave tomography across the Trans-European suture zone between Sweden and Denmark /." [S.l.] : [s.n.], 1999. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=13501.

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28

Cassidy, John Francis. "Teleseismic receiver function analysis of the crust and upper mantle of southwestern British Columbia." Thesis, University of British Columbia, 1991. http://hdl.handle.net/2429/30966.

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The northern Cascadia subduction zone has been the site of numerous geophysical studies during the past two decades. However, little is known of the deep structure (> 40 km) or S-velocities throughout this region. In this study, locally generated P-to-S conversions (Ps) contained in ~100 teleseismic P-wave coda have been analysed to determine the S-velocity structure to upper mantle depths. Prior to the analysis, the applications and limitations of this technique as applied to a dipping layer environment have been examined. It is concluded that strict stacking bounds (≤ 10° in ∆ and BAZ) shou

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29

Chen, Chin-Wu Ph D. Massachusetts Institute of Technology. "Teleseismic imaging of the Slave craton and implications for the assembly of cratonic lithosphere." Thesis, Massachusetts Institute of Technology, 2010. http://hdl.handle.net/1721.1/58394.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2010.<br>Cataloged from PDF version of thesis.<br>Includes bibliographical references (p. 123-132).<br>In this dissertation, I investigate the assembly and evolution of the Archean cratonic lithosphere by using two complementary seismological methods to image the lithospheric structure of the Slave craton in Canada. First, I perform surface wave tomographic inversions to constrain the depth dependence of Rayleigh wave phase velocity, shear wave velocity, and azimuthal anisotropy of the

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30

Schneider, Felix Michael [Verfasser]. "Imaging an Intra-continental Subduction in Central Asia with Teleseismic Receiver Functions / Felix Michael Schneider." Berlin : Freie Universität Berlin, 2014. http://d-nb.info/1054341443/34.

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31

VanDecar, John Callaway. "Upper-mantle structure of the Cascadia subduction zone from non-linear teleseismic travel-time inversion /." Thesis, Connect to this title online; UW restricted, 1991. http://hdl.handle.net/1773/6804.

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32

Hammond, William Charles. "Dynamics, flow and melt content of the Southern East Pacific Rise upper mantle from teleseismic tomography /." view abstract or download file of text, 2000. http://wwwlib.umi.com/cr/uoregon/fullcit?p9998033.

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Thesis (Ph. D.)--University of Oregon, 2000.<br>Typescript. Includes vita and abstract. Includes bibliographical references (leaves 139-151). Also available for download via the World Wide Web; free to University of Oregon users.

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33

Frassetto, Andrew Michael. "TELESEISMIC STUDIES OF THE NORTH AMERICAN CORDILLERA: EVALUATING THE CHANGING STRUCTURE, COMPOSITION, AND FABRIC AFTER SUBDUCTION." Diss., The University of Arizona, 2009. http://hdl.handle.net/10150/195821.

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The cessation of wide-scale subduction and orogenic compression during the early to mid-Cenozoic radically altered the North American Cordillera. This dissertation summarizes the results of three seismic studies, conducted in different regions of western North America, aimed at understanding how the structure and character of the crust and upper mantle relate to regions of post-subduction magmatism and persisting high elevations. Across the southern Basin and Range and Colorado Plateau teleseismic receiver functions show that only the Colorado Plateau contains thick crust commensurate with its

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34

Hosseini, Kasra [Verfasser], and Heiner [Akademischer Betreuer] Igel. "Global multiple-frequency seismic tomography using teleseismic and core-diffracted body waves / Kasra Hosseini. Betreuer: Heiner Igel." München : Universitätsbibliothek der Ludwig-Maximilians-Universität, 2016. http://d-nb.info/1106854594/34.

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35

Heuer, Barbara. "Lithospheric and upper mantle structure beneath the western Bohemian Massif obtained from teleseismic P and S receiver functions." Potsdam : Geoforschungszentrum [u.a.], 2006. http://www.diss.fu-berlin.de/2006/401/index.html.

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36

El-Haddadeh, B. R. H. "Seismological investigation of the crust and upper mantle structure of the British Isles using teleseismic travel time data." Thesis, University of Leeds, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.372598.

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37

Schneider, Felix Michael [Verfasser]. "Imaging an intra-continental subduction in Central Asia with teleseismic receiver functions / Felix Michael Schneider. Deutsches GeoForschungsZentrum GFZ." Potsdam : Deutsches GeoForschungsZentrum GFZ, 2014. http://nbn-resolving.de/urn:nbn:de:kobv:b103-14063.

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38

Dewberry, Shawn Robert. "Crustal and upper mantle structure for the Pacific Northwest from an analysis of short-period teleseismic network data /." Thesis, Connect to this title online; UW restricted, 1996. http://hdl.handle.net/1773/6795.

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39

THAPA, HARI RAM. "Crustal structure and discontinuities beneath the Nepal Himalaya using seismic ambient noise and teleseismic P wave coda autocorrelation." Doctoral thesis, Università degli Studi di Trieste, 2021. http://hdl.handle.net/11368/2996096.

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Nepal is an actively deforming region because of its tectonic setting as demon-strated by many destructive seismic events it hosted in the past with the most re-cent Gorkha 2015 magnitude 7.8 earthquake. For a better understanding of the crustal structure, of the physics of earthquakes as well as their detailed high-resolution location and monitoring, and to mitigate the real-time seismic hazard, an adequate 3-D regional velocity model is needed. So far, a country-wide 3-D velocity structure is unavailable. Here, we present a new high-resolution 3-D shear-wave velocity structure down to 60 km

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40

Rößler, Dirk, Frank Krüger, Matthias Ohrnberger, and Lutz Ehlert. "Automatic near real-time characterisation of large earthquakes." Universität Potsdam, 2008. http://opus.kobv.de/ubp/volltexte/2008/2019/.

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An der Universität Potsdam wird seit 2008 ein automatisiertes Verfahren angewandt, um Bruchparamter großer Erdbeben in quasi-Echtzeit, d.h. wenige Minuten nachdem sich das Beben ereignet hat, zu bestimmen und der Öffentlichkeit via Internet zur Verfügung zu stellen. Es ist vorgesehen, das System in das Deutsch-Indonesische Tsunamifrühwarnsystem (GITEWS) zu integrieren, für das es speziell konfiguriert ist. Wir bestimmen insbesondere die Dauer und die Ausdehnung des Erdbebens, sowie dessen Bruchgeschwindigkeit und -richtung. Dabei benutzen wir die Seismogramme der zuerst eintreffenden P Wellen

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41

Heit, Benjamin S. "Teleseismic tomographic images of the Central Andes at 21°S and 25.5°S an inside look at the Altiplano and Puna plateaus /." [S.l.] : [s.n.], 2005. http://www.diss.fu-berlin.de/2005/319/index.html.

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42

Beller, Stephen. "Imagerie lithosphérique par inversion de formes d’ondes télésismiques – Application aux Alpes Occidentales." Thesis, Université Côte d'Azur (ComUE), 2017. http://www.theses.fr/2017AZUR4007/document.

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Dans cette thèse, un algorithme d'inversion de formes d'ondes (FWI) est développé pour l'imagerie 3D des paramètres élastiques de la lithosphère à partir des enregistrements télésismiques dans le but d'accroître la résolution des images lithosphériques. La modélisation sismique est effectuée par un méthode hybride d'injection de champ d'ondes. Une première modélisation est effectuée dans une Terre globale avec le logiciel AxiSEM pour déterminer les champs d’ondes aux bords de la cible lithosphérique. Ces solutions sont ensuite propagées dans cette cible par une méthode aux éléments finis spect

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43

Santos, Rúben José Chaves Miguel dos. "Modelação de processos de rotura sísmica através de dados de observação da deformação superficial." Doctoral thesis, Universidade de Évora, 2013. http://hdl.handle.net/10174/11790.

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Nesta dissertação foi desenvolvida uma metodologia baseada no cruzamento de diferentes técnicas e de dados geodésicos e sísmicos, para estudar o processo de rotura de sismos. A metodologia consiste, numa primeira fase, em determinar o campo de deslocamento cossísmico produzido por um evento, através da técnica InSAR. Numa fase seguinte o modelo de deslocamentos cossísmicos é determinado através das equações de Okada utilizando o modelo de distribuição de deslizamentos obtido pela inversão das formas de onda registadas em estações de banda larga a distâncias telessísmicas. Para comparar o model

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44

Heuer, Barbara [Verfasser]. "Lithospheric and upper mantle structure beneath the western Bohemian Massif obtained from teleseismic P and S receiver functions / Geoforschungszentrum Potsdam in der Helmholtz-Gemeinschaft. Barbara Heuer." Potsdam : Geoforschungszentrum, 2006. http://d-nb.info/98226769X/34.

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45

Kufner, Sofia-Katerina [Verfasser]. "Lithospheric structure and seismotectonic setting of the Hindu Kush, the Tajik-Afghan basin and the western Pamir from analysis of local- and teleseismic data / Sofia-Katerina Kufner." Berlin : Freie Universität Berlin, 2016. http://d-nb.info/1122438737/34.

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46

Nooshiri, Nima [Verfasser], Torsten [Akademischer Betreuer] Dahm, Frederik [Akademischer Betreuer] Tilmann, Torsten [Gutachter] Dahm, Frank [Gutachter] Krüger, and Steven J. [Gutachter] Gibbons. "Improvement of routine seismic source parameter estimation based on regional and teleseismic recordings / Nima Nooshiri ; Gutachter: Torsten Dahm, Frank Krüger, Steven J. Gibbons ; Torsten Dahm, Frederik Tilmann." Potsdam : Universität Potsdam, 2020. http://d-nb.info/1218795182/34.

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47

Silvennoinen, H. (Hanna). "3D structure of the crust and upper mantle beneath Northern Fennoscandian shield." Doctoral thesis, University of Oulu, 2015. http://urn.fi/urn:isbn:9789526210681.

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Abstract The crustal and upper mantle structures of the Shield on the regional scale were investigated using the data of the POLENET/LAPNET passive seismic array and the previously published models of active and passive seismic experiments in the study area. This area is centred in northern Finland and it extends to surrounding areas in Sweden, Norway and northwestern Russia. The bedrock there is mostly of the Archaean origin and the lithosphere of the region was reworked by two orogenies during Palaeoproterozoic. One of the results of the thesis was a new map of the Moho depth of the study ar

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Moidaki, Moikwathai. "Crustal modification by tectonic events and upper mantle anisotropy beneath the Midcontinent Rift and New Madrid Seismic Zone: insights from receiver function studies and teleseismic shear wave splitting." Diss., Rolla, Mo. : Missouri University of Science and Technology, 2009. http://scholarsmine.mst.edu/thesis/pdf/Moidaki_09007dcc8064a755.pdf.

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Thesis (Ph. D.)--Missouri University of Science and Technology, 2009.<br>Vita. The entire thesis text is included in file. Title from title screen of thesis/dissertation PDF file (viewed April 29, 2009) Includes bibliographical references (p. 119-131).

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Läderach, Christine [Verfasser], Vera [Akademischer Betreuer] Schlindwein, and Cornelia [Akademischer Betreuer] Spiegel. "Seismicity of ultraslow spreading mid-ocean ridges at local, regional and teleseismic scales: A case study of contrasting segments / Christine Läderach. Gutachter: Vera Schlindwein ; Cornelia Spiegel. Betreuer: Vera Schlindwein." Bremen : Staats- und Universitätsbibliothek Bremen, 2012. http://d-nb.info/107215577X/34.

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Heit, Benjamin S. [Verfasser]. "Teleseismic tomographic images of the Central Andes at 21°S and 25.5°S : an inside look at the Altiplano and Puna plateaus / Geoforschungszentrum Potsdam, Stiftung des Öffentlichen Rechts. Benjamin S. Heit." Potsdam : Geoforschungszentrum, 2006. http://d-nb.info/97980258X/34.

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