Academic literature on the topic 'Geophysics Observations'

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Journal articles on the topic "Geophysics Observations"

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Doyle, H. "Geophysics in Australia." Earth Sciences History 6, no. 2 (1987): 178–204. http://dx.doi.org/10.17704/eshi.6.2.386k258604262836.

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Geophysical observations began in Australia with the arrival of the first European explorers in the late 18th Century and there have been strong connections with European and North American geophysics ever since, both in academic and exploration geophysics. Government institutions, particularly the Bureau of Mineral Resources, have played a large part in the development of the subject in Australia, certainly more so than in North America. Academic research in geophysics has been dominated by that at the Australian National University. Palaeomagnetic research at the Australian National Universi
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Pollitz, F. F. "GEOPHYSICS: A New Class of Earthquake Observations." Science 313, no. 5787 (2006): 619–20. http://dx.doi.org/10.1126/science.1131208.

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Loginov, D. S. "Cartographic support of geophysical research: current situation and prospects." Geodesy and Cartography 950, no. 8 (2019): 32–44. http://dx.doi.org/10.22389/0016-7126-2019-950-8-32-44.

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The features of cartographic supporting geophysical research at the present stage of cartography and exploration geophysics development are discussed. The current situation and prospects of using GIS and web technologies are characterized basing on the analysis of scientific and industrial experience of domestic and foreign public as well as private geological and geophysical organizations. The analysis was performed at key stages of geophysical research, including the analysis of geological and geophysical studying the work area, designing geophysical works, field works, processing and interp
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Ganiev, O. Z., T. A. Amashukeli, L. V. Farfuliak, and K. V. Petrenko. "Organization of the stationary seismological observations point." Geofizicheskiy Zhurnal 43, no. 5 (2021): 232–40. http://dx.doi.org/10.24028/gzh.v43i5.244085.

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The Institute of Geophysics of the NASU organizes and carries out continuous regional and local seismic observations on the territory of Ukraine. The article presents a universal modern model of seismic activity monitoring process, which is used in most international seismological agencies (USGS, EMSC, NEIC) and describes a typical stationary point of seismological observations of the National Seismological Network of the Institute of Geophysics of NAS of Ukraine. Seismological network of observations is a complex of systems consisting of stationary seismological points of registration of seis
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Zhang, Jie. "President's Page: Looking into the world of medical imaging from the perspective of a geophysicist." Leading Edge 41, no. 6 (2022): 372–73. http://dx.doi.org/10.1190/tle41060372.1.

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I have worked in the geophysical industry and in academia as a geophysicist for 25 years. During the same time frame, I have also worked for 24 years in the medical industry. I founded a geophysical imaging company in 1998, and a year later I cofounded a medical imaging company. During the last seven years, I have led two biomedical companies to develop treatment solutions for bacterial infections and cancers. My career path offers me a unique insight into the world of medical imaging from the perspective of a geophysicist. In the following, I would like to share some of my observations, based
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Bell, Ernest, Nicholas Schmerr, Ryan Porter, et al. "Active seismic exploration along a human lunar mission traverse analogue in the San Francisco volcanic field." Leading Edge 41, no. 10 (2022): 690–99. http://dx.doi.org/10.1190/tle41100690.1.

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Lunar surface activities during Apollo and terrestrial analogue lunar mission simulations have commonly focused on traverses that prioritize surface observations and sample collection activities. Along the way, geophysical measurements are often made. However, they are not necessarily made in a way that optimizes information about the physical subsurface properties, which is something that geophysics can provide. In 2010, NASA simulated a high-quality multiweek human lunar rover traverse analogue mission in the San Francisco volcanic field in Arizona. The traverse route and associated science
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Ozcep, F., and T. Ozcep. "Notes on the history of geophysics in the Ottoman Empire." History of Geo- and Space Sciences 5, no. 2 (2014): 163–74. http://dx.doi.org/10.5194/hgss-5-163-2014.

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Abstract. In Anatolia, the history of geophysical sciences may go back to antiquity (600 BC), namely the period when Thales lived in Magnesia (Asia Minor). In the modern sense, geophysics started with geomagnetic works in the 1600s. The period between 1600 and 1800 includes the measurement of magnetic declination, inclination and magnetic field strength. Before these years, there is a little information, such as how to use a compass, in the Kitab-i Bahriye (the Book of Navigation) of Piri Reis, who is one of the most important mariners of the Ottoman Empire. However, this may not mean that mag
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GUPTA, M. DAS, SOMESHWAR DAS, K. PRASANTHI, P. K. PRADHAN, and U. C. MOHANTY. "Validation of upper-air observations taken during the ARMEX-I and its impact on the global analysis-forecast system." MAUSAM 56, no. 1 (2022): 139–46. http://dx.doi.org/10.54302/mausam.v56i1.871.

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During ARMEX-I several special observations were taken over Arabian Sea region and adjoining west coast of India, which gave an opportunity to study this region more thoroughly. To handle such voluminous data, ARMEX data center has been established at National Centre for Medium Range Weather Forecasting (NCMRWF), in collaboration with India Meteorological Department (IMD) and Indian Institute Technology (IIT), Delhi. One of the tasks of this center is to produce reanalysis for ARMEX period, utilizing these observations. It is essential to assimilate every observation from all available sources
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Carter, W. E., and D. S. Robertson. "Very-Long-Baseline Interferometry Applied to Geophysics." Symposium - International Astronomical Union 156 (1993): 133–44. http://dx.doi.org/10.1017/s0074180900173115.

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Very-long-baseline Interferometry (VLBI) has opened for study a broad new spectrum of geophysical phenomena including: direct observation of the tectonic motions and deformations of the Earth's crustal plates, observations of unprecedented detail of the variations in the rotation of the Earth, and direct measurement of the elastic deformations of the Earth in response to tidal forces. These new measurements have placed significant constraints on models of the interior structure of the Earth; for example, measurements of the variations in the Earth's nutation have been shown to be particularly
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Meyers, Patrick, Daniel C. Bowden, Tanner Prestegard, et al. "Direct Observations of Surface‐Wave Eigenfunctions at the Homestake 3D Array." Bulletin of the Seismological Society of America 109, no. 4 (2019): 1194–202. http://dx.doi.org/10.1785/0120190026.

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Abstract Despite the theory for both Rayleigh and Love waves being well accepted and the theoretical predictions accurately matching observations, the direct observation of their quantifiable decay with depth has never been measured in the Earth’s crust. In this work, we present observations of the quantifiable decay with depth of surface‐wave eigenfunctions. This is done by making direct observations of both Rayleigh‐wave and Love‐wave eigenfunction amplitudes over a range of depths using data collected at the 3D Homestake array for a suite of nearby mine blasts. Observations of amplitudes ov
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Dissertations / Theses on the topic "Geophysics Observations"

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Shcherbenko, Gina Nicole. "Post-Seismic Strain and Stress Evolution from Continuous GPS Observations." Thesis, State University of New York at Stony Brook, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=1567846.

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<p> Strain evolution and stress evolution following the 4 April 2010 M7.2 El Mayor-Cucapah earthquake are modeled using an adaptation of the strain transient detection tool developed by <i>Holt and Shcherbenko</i> 2013. The evolution of stress is calculated from postseismic strains, which are modeled from continuous GPS horizontal displacements. Strain fields are modeled in 2 ways; the total strain field based on total observed cGPS displacements, and the residual strain field, which subtracts a reference field from the total model. The residual shows anomalous strains resulting from the posts
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De, Michele Marcello. "Observations seismo-tectoniques par télédétection satellitaire." Phd thesis, Université Pierre et Marie Curie - Paris VI, 2010. http://tel.archives-ouvertes.fr/tel-00656931.

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Pendant les 20 dernières années, notre connaissance de la déformation de la Terre a été complètement bouleversée par l'introduction de deux techniques de Géodésie spatiale. D'une part, ce que l'on appelle positionnement satellitaire ('point positioning') pas seulement à partir du système GPS (Global Positioning System) mais également à partir du système DORIS (Doppler Orbitography and Radio-positioning Integrated from Space). D'autre part, ont été développées des techniques d'imagerie satellitaire de corrélation d'images et d'interférométrie SAR (Synthetic Aperture Radar) ainsi que les méthode
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O'Toole, Thomas Bartholomew. "Studies of earthquakes and microearthquakes using near-field seismic and geodetic observations." Thesis, University of Oxford, 2013. http://ora.ox.ac.uk/objects/uuid:9dcaca2e-c141-4e8a-94f6-34a9ff50d061.

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The Centroid-Moment Tensor (CMT) method allows an optimal point-source description of an earthquake to be recovered from a set of seismic observations, and, for over 30 years, has been routinely applied to determine the location and source mechanism of teleseismically recorded earthquakes. The CMT approach is, however, entirely general: any measurements of seismic displacement fields could, in theory, be used within the CMT inversion formulation, so long as the treatment of the earthquake as a point source is valid for that data. We modify the CMT algorithm to enable a variety of near-field se
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Morrow, Eric. "Estimates of Land Ice Changes from Sea Level and Gravity Observations." Thesis, Harvard University, 2014. http://dissertations.umi.com/gsas.harvard:11385.

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Understanding how global ice volume on the Earth has changed is of significant importance to improving our understanding of the climate system. Fortunately, the geographically unique perturbations in sea level that result from rapid changes in the mass of, otherwise difficult to measure, land-ice reservoirs can be used to infer the sources and magnitude of melt water. We explore the history of land-ice mass changes through the effect that these mass fluxes have had on both global and regional gravity and sea-level fields.<br>Earth and Planetary Sciences
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Enderlin, Ellyn Mary. "Observations and Modeling of Greenland Outlet Glacier Dynamics." The Ohio State University, 2013. http://rave.ohiolink.edu/etdc/view?acc_num=osu1372609057.

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Dardel, Cécile. "Entre désertification et reverdissement du Sahel : Diagnostic des observations spatiales et in situ." Phd thesis, Université Paul Sabatier - Toulouse III, 2014. http://tel.archives-ouvertes.fr/tel-00944267.

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Le Sahel est une région semi-aride caractérisée par un fort gradient bioclimatique et qui est particulièrement sensible à la variabilité des précipitations. Les périodes de très forte sécheresse qui ont sévi sur l'ensemble du Sahel entre les années 1970 et 1980 ont eu des effets dévastateurs sur les écosystèmes, les populations et leurs ressources. La théorie d'une désertification du Sahel a été ravivée, ainsi que celle prédisant une avancée rapide du Sahara sur le reste du continent. Dès les années 1990, l'analyse des premiers indices de végétation satellitaires (NDVI) acquises à l'échelle du
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González-Caneda, María. "Investigation Of Source Parameters Of Earthquakes In Northern Sweden." Thesis, Uppsala universitet, Geofysik, 2019. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-380133.

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By studying the frequency domain of seismic signals generated by earthquakes, the source parameters can be recovered, i.e., the seismic moment (M0) and the stress drop (Δσ). This method is an advantage especially since if the source parameters are calculated from the time domain a full waveform inversion is needed, therefore this procedure facilitates the computation. Besides, the moment magnitude (Mw) can be calculated from the seismic moment and, in turn, the local magnitude (ML) can be obtained by using an algorithm that matches different ranges of moment magnitude with their corresponding
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Cotton, Julien. "Analyse et traitement de données sismiques 4D en continu et en temps réel pour la surveillance du sous-sol." Electronic Thesis or Diss., Paris Sciences et Lettres (ComUE), 2019. http://www.theses.fr/2019PSLEM023.

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La sismique réflexion 3D est largement utilisée dans l'industrie pétrolière. Cette méthode d’auscultation du sous-sol fournit des informations sur les structures géologiques et peut être utilisée pour construire des modèles de réservoir. Cependant, les propriétés dérivées des données sismiques 3D (et 2D) ne sont que statiques: elles ne permettent pas d’évaluer ce qui change avec le temps. L'ajout d'une dimension temporelle aux données 3D est obtenue par la répétition des mesures à plusieurs dates séparées de plusieurs mois voire même de plusieurs années. Ainsi, la sismique4D (time-lapse) perme
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Cordisco, Emmanuel. "Etude de la synergie des observations satellites pour la caractérisation du manteau neigeux." Phd thesis, Université Pierre et Marie Curie - Paris VI, 2005. http://tel.archives-ouvertes.fr/tel-00089376.

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La neige étant une composante importante du climat terrestre, il convient de l'étudier à l'échelle du globe pour en comprendre son rôle.<br /><br />Ces travaux visent ainsi à étudier le contenu en information sur le manteau neigeux à l'échelle globale des observations satellites réalisées à partir de différents instruments couvrant différents domaines du spectre électromagnétique (visible, infrarouge et micro-ondes). Des paramètres autres que la neige interférant dans la problématique, il est nécessaire de les déterminer afin d'encadrer leurs influences. Ensuite, on cherchera comment limiter l
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Eymin, Céline. "Etude des mouvements à la surface du noyau terrestre : du 17ème au 21ème siècle." Phd thesis, Université Pierre et Marie Curie - Paris VI, 2004. http://tel.archives-ouvertes.fr/tel-00007173.

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Afin d'étudier la dynamique du noyau terrestre, nous reconstruisons les mouvements à la surface du noyau liquide compatibles avec les observations du champ magnétique. La similitude des mouvements obtenus par deux méthodes indépendantes et les résultats de tests synthétiques confirment la pertinence de ces reconstructions. Deux types d'observations sont utilisées : des observations terrestres couvrant la période 1590-1990 et des observations satellitaires haute-résolution récentes. Une série temporelle des mouvements<br />historiques et un modèle détaillé des mouvements actuels sont obtenus. L
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Books on the topic "Geophysics Observations"

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Pragmatic inversion of geophysical data. Springer-Verlag, 1992.

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Bodhaine, Barry A. Geophysical monitoring for climatic change, no. 16: Summary report, 1987. Edited by Environmental Research Laboratories (U.S.). U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, 1988.

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Séminaire ORSTOM (1991 Université de Savoie). Du capteur aux banques de données: Techniques d'instrumentation en géophysique : Séminaire ORSTOM, Université de Savoie, Aussois, du 10 au 12 juin 1991. Editions de l'ORSTOM, 1993.

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Hitchman, A. P. First-order regional magnetic survey of Australia for epoch, 1990.0, 1986-89. Australian Govt. Pub. Service, 1990.

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Nikolaevich, Rykunov Lev, ed. Seĭsmologicheskie donnye nabli͡u︡denii͡a︡ v SSSR i za rubezhom. "Nauka,", 1986.

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King, A. Applications of geophysical methods for monitoring acid mine drainage. Canada Centre for Mineral and Energy Technology = Centre canadien de la technologie des minéraux et de l'énergie, 1994.

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Grau, Jordi Seguí. Análisis de la serie de temperatura del Observatorio del Ebro (1894-2002). Observatori de lʼEbre, 2003.

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March, Rod. Mass balance, meteorological, ice motion, surface altitude, and runoff data at Gulkana Glacier, Alaska, 1992 balance year. U.S. Geological Survey, 1996.

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March, Rod. Mass balance, meteorological, ice motion, surface altitude, and runoff data at Gulkana Glacier, Alaska, 1992 balance year. U.S. Geological Survey, 1996.

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March, Rod. Mass balance, meteorological, ice motion, surface altitude, and runoff data at Gulkana Glacier, Alaska, 1992 balance year. U.S. Dept. of the Interior, Geological Survey, 1996.

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Book chapters on the topic "Geophysics Observations"

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Bloxham, J. "The determination of fluid flow at the core surface from geomagnetic observations." In Mathematical Geophysics. Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-2857-2_9.

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Chadha, R. K. "Seismic Signals in Well Water Observations." In Encyclopedia of Solid Earth Geophysics. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-10475-7_188-1.

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Davis, Earl E., and Andrew T. Fisher. "Heat Flow, Seafloor: Methods and Observations." In Encyclopedia of Solid Earth Geophysics. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-10475-7_65-1.

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Cahalan, Robert F. "Landsat Observations of Fractal Cloud Structure." In Non-Linear Variability in Geophysics. Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-009-2147-4_22.

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Davis, Earl E., and Andrew T. Fisher. "Heat Flow, Seafloor: Methods and Observations." In Encyclopedia of Solid Earth Geophysics. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-8702-7_65.

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Chadha, R. K. "Seismic Signals in Well Water Observations." In Encyclopedia of Solid Earth Geophysics. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-58631-7_188.

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Davis, Earl E., and Andrew T. Fisher. "Heat Flow, Seafloor: Methods and Observations." In Encyclopedia of Solid Earth Geophysics. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-58631-7_65.

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Starchenko, S. V. "Simple Estimations for Planetary Convection Turbulence and Dynamo Magnetism from Optimized Scaling and Observations." In Springer Geophysics. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-90437-5_34.

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Diamond, P. J. "Observations of Cosmic Masers." In The Impact of VLBI on Astrophysics and Geophysics. Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-2949-4_75.

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Khalid, Zubair, and Abubakr Muhammad. "Compressive Sensing on the Sphere: Slepian Functions for Applications in Geophysics." In Compressive Sensing of Earth Observations. CRC Press, 2017. http://dx.doi.org/10.1201/9781315154626-2.

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Conference papers on the topic "Geophysics Observations"

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Cole, S., and M. Karrenbach. "Multi-well DAS Observations for Hydraulic Fracture Monitoring." In Fifth EAGE Workshop on Borehole Geophysics. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.2019x604059.

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Nikitin, A. A., and A. N. Lebedev. "Integrated processing and interpretation of multilevel geophysical observations." In Geophysics of the 21st Century - The Leap into the Future. European Association of Geoscientists & Engineers, 2003. http://dx.doi.org/10.3997/2214-4609-pdb.38.f120.

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Bychkov, S. G., A. A. Simanov, and V. V. Khokhlova. "Control of The Process of Subsidence of The Earth's Surface by Monitoring Gravimetric Observations." In Engineering and Mining Geophysics 2021. European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.202152028.

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Olhoeft, Gary R. "Geophysical Observations of Geological, Hydrological and Geochemical Heterogeneity." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 1994. Environment and Engineering Geophysical Society, 1994. http://dx.doi.org/10.4133/1.2922059.

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R. Olhoeft, Gary. "Geophysical Observations Of Geological, Hydrological And Geochemical Heterogeneity." In 7th EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 1994. http://dx.doi.org/10.3997/2214-4609-pdb.208.1994_009.

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Shapovalov, V. L., A. V. Morozov, D. R. Tagirova, and V. A. Yavna. "Forecasting Changes in The Water Level in The River Based on Long-Term Observations of Influencing Factors." In Engineering and Mining Geophysics 2021. European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.202152054.

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Shulakov, D. Y., F. G. Verkholantsev, and A. S. Zvereva. "Detailed Seismological Monitoring Technology Based on Observations in the Krasnoslobodsky Fault Zone of the Starobinsk Potash Deposit." In Engineering and Mining Geophysics 2020. European Association of Geoscientists & Engineers, 2020. http://dx.doi.org/10.3997/2214-4609.202051057.

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Tokarev, M., A. Pirogova, A. Roslyakov, et al. "Evaluation of Potential Geological Hazards in the Sea of Okhotsk from Conventional 3D Seismic Observations." In 3rd Applied Shallow Marine Geophysics Conference. EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201802684.

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Walters, Shelby L., Richard D. Miller, Joseph B. Dunbar, and Steve Smullen. "Repeatability Observations from a 2D Time‐Lapse Seismic Survey." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 2007. Environment and Engineering Geophysical Society, 2007. http://dx.doi.org/10.4133/1.2924750.

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Kovachev, S. A., A. A. Krylov, and S. G. Mironyuk. "Seismic Hazard Assessment Along The Gas Pipeline Route in The Russian Sector of The Black Sea Using Bottom Seismological Observations." In Engineering and Mining Geophysics 2021. European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.202152117.

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Reports on the topic "Geophysics Observations"

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Cenedese, Claudia, and Mary-Louise Timmermans. 2017 program of studies: ice-ocean interactions. Woods Hole Oceanographic Institution, 2018. http://dx.doi.org/10.1575/1912/27807.

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The 2017 Geophysical Fluid Dynamics Summer Study Program theme was Ice-Ocean Interactions. Three principal lecturers, Andrew Fowler (Oxford), Adrian Jenkins (British Antarctic Survey) and Fiamma Straneo (WHOI/Scripps Institution of Oceanography) were our expert guides for the first two weeks. Their captivating lectures covered topics ranging from the theoretical underpinnings of ice-sheet dynamics, to models and observations of ice-ocean interactions and high-latitude ocean circulation, to the role of the cryosphere in climate change. These icy topics did not end after the first two weeks. Sev
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Berndt, Christian. RV SONNE Fahrtbericht / Cruise Report SO277 OMAX: Offshore Malta Aquifer Exploration, Emden (Germany) – Emden (Germany), 14.08. – 03.10.2020. GEOMAR Helmholtz Centre for Ocean Research Kiel, 2021. http://dx.doi.org/10.3289/geomar_rep_ns_57_20.

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SO277 OMAX served two scientific projects. The objectives of the first project, SMART, were to develop multi-disciplinary methodologies to detect, quantify, and model offshore groundwater reservoirs in regions dominated by carbonate geology such as the Mediterranean Sea. To this end we acquired controlled-source electromagnetic, seismic, hydroacoustic, geochemical, seafloor imagery data off Malta. Preliminary evaluation of the geophysical data show that there are resisitivity anomalies that may represent offshore freshwater aquifers. The absence of evidence for offshore springs means that thes
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Lithologic, geophysical, and well-construction data for observation wells in the Melton Valley area, Oak Ridge Reservation, Tennessee. US Geological Survey, 1989. http://dx.doi.org/10.3133/wri884197.

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