Relevant bibliographies by topics / Microseisms

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Microseisms'

Author: Grafiati
Published: 4 June 2021
Last updated: 29 July 2024

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Journal articles on the topic "Microseisms"

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Davydov, V. A. "STUDY OF SEISMIC RESPONSE OF SOILS IN MICROSEISMIC SOUNDINGS OF DAMS." Bulletin of Kamchatka Regional Association «Educational-Scientific Center». Earth Sciences 2(58) (2023): 90–100. http://dx.doi.org/10.31431/1816-5524-2023-2-58-90-100.

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The basic fundamentals of spectral analysis of horizontal and vertical components of microseismic noise for studying the geological structure of dams are presented. The issues of constructing deep sections of three dynamic parameters of microseisms are considered. The aim of the work is to study the seismic reaction of soils during microseismic sounding of hydraulic structures. The main objectives of the research include the comparison of deep sections of soil reinforcement coefficients with sections of transmission ratios and data from other geophysical methods. As a result of microseismic so
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Wang, Siyin, Yan Xu, Chaodi Xie, and Aitang Li. "Study TOMAS Cyclone Using Seismic Array and Single Station." Applied Sciences 13, no. 2 (2023): 918. http://dx.doi.org/10.3390/app13020918.

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The continuous data from the YL array and four AU stations during the lifetime of the cyclone TOMAS in March 2010 were downloaded from IRIS. By performing frequency-wave number (F-K) analysis on the array data, it was found that the orientation of the maximum energy of the secondary microseisms (0.1~0.5 Hz) was consistent with the movement of TOMAS when the central wind speed reached the typhoon level. The high wind speed of the cyclone could generate secondary microseisms as well as the high swell. However, the large global earthquake can affect the microseismic observations using F-K. The AU
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Park, Seongjun, and Tae-Kyung Hong. "Typhoon-Induced Microseisms around the South China Sea." Seismological Research Letters 91, no. 6 (2020): 3454–68. http://dx.doi.org/10.1785/0220190310.

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Abstract Microseisms in frequencies of 0.05–0.5 Hz are a presentation of solid earth response to the ocean waves that are developed by atmospheric pressure change. The South China Sea provides a natural laboratory with a closed ocean environment to examine the influence of regional factors on microseism development as well as the nature of microseisms. The microseisms induced by typhoons crossing over the South China Sea are investigated. Typhoons are typical transient sources of varying strengths and locations. Primary microseisms develop nearly stationary in the northeastern South China Sea
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Besedina, A. N., Ts A. Tubanov, P. A. Predein, D. P. D. Sanzhieva, and G. N. Ivanchenko. "Lake Baikal Microseisms Based on Regional Seismic Network Data." Физика земли, no. 3 (June 6, 2024): 30–50. http://dx.doi.org/10.31857/s0002333724030041.

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Seismic ambient noise in the regional seismic network in the central part of the Baikal rift is studied. The probabilistic approach is used to thoroughly investigate the pattern of diurnal variations in microseisms and to analyze amplitude level and frequency content of spatial anomalies and temporal changes (seasonal and annual). Based on the 2020–2021 data, a regional probabilistic model of the microseismic noise is built in a wide range of periods. The study of microseisms in the frequency band of about 1 Hz revealed a seasonal anomaly against the level of the global minimum in the microsei
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Cessaro, Robert K. "Sources of primary and secondary microseisms." Bulletin of the Seismological Society of America 84, no. 1 (1994): 142–48. http://dx.doi.org/10.1785/bssa0840010142.

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Abstract Low-frequency (0.01 to 0.2 Hz) seismic noise, arising from pelagic storms, is commonly observed as microseisms in seismic records from land and ocean bottom detectors. One principal research objective, in the study of microseisms, has been to locate their sources. This article reports on an analysis of primary and secondary microseisms (i.e., near and double the frequency of ocean swell) recorded simultaneously on three land-based long-period arrays (Alaskan Long Period Array, Montana Large Aperture Seismic Array, and Norwegian Seismic Array) during the early 1970s. Reliable microseis
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Lepore, Simone, and Marek Grad. "Relation between ocean wave activity and wavefield of the ambient noise recorded in northern Poland." Journal of Seismology 24, no. 6 (2020): 1075–94. http://dx.doi.org/10.1007/s10950-020-09963-y.

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AbstractThe temporal and spatial variations of the wavefield of ambient noise recorded at ‘13 BB star’ array located in northern Poland were related to the activity of high, long-period ocean waves generated by strong storms in the Northern Indian Ocean, the Atlantic Ocean, and the Northern Pacific Ocean between 2013 and 2016. Once pre-processed, the raw noise records in time- and frequency-domains, and spectral analysis and high-resolution three-component beamforming techniques were applied to the broadband noise data. The power spectral density was analysed to quantify the noise wavefield, o
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Gao, Hong, Chaomin Mu, and Hui Sun. "Microseism Detection Method in Coal Mine Based on Spatiotemporal Characteristics and Support Vector Regression Algorithm." Applied Sciences 13, no. 17 (2023): 9917. http://dx.doi.org/10.3390/app13179917.

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In view of the inconsistency of guided wave energy in distributed acoustic sensing coal mine maps and the difficulty in distinguishing the vibration levels of coal mines, which leads to the poor sensitivity and accuracy of microseism detection, a coal mine microseism detection method based on time–space characteristics and a support vector regression algorithm is proposed to ensure the safety of coal mine operations. The spatiotemporal sliding window was used to collect the coal mine data in real-time, and the continuous attribute discretization algorithm based on entropy was used to discretiz
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Dolgikh, Grigory I., Vladimir A. Chupin, Egor S. Gusev, and Galina A. Timoshina. "Cyclonic Process of the “Voice of the Sea” Microseism Generation and Its Remote Monitoring." Remote Sensing 13, no. 17 (2021): 3452. http://dx.doi.org/10.3390/rs13173452.

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The article presents the results of microseismic signals of the “voice of the sea” registration by a two-coordinate laser strainmeter during the passage of typhoons through and near the water area of the Sea of Japan. It was established that the “voice of the sea” microseisms appear and disappear almost simultaneously with primary microseisms, i.e., the powerful “voice of the sea” microseisms exist only in the presence of powerful wind waves, generated by a passing typhoon. According to the processing results of the obtained experimental data, the “voice of the sea” microseisms generation area
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Huang, Lei, Yanchun Xu, Shiqi Liu, et al. "Research on the Development Law of Pre-Mining Microseisms and Risk Assessment of Floor Water Inrush: A Case Study of the Wutongzhuang Coal Mine in China." Sustainability 14, no. 15 (2022): 9774. http://dx.doi.org/10.3390/su14159774.

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Coal-mining areas are widely distributed in Northern China, but are under threat from confined water in the mining operation, resulting in a series of floor water- inrush hazards. Therefore, it is significant to effectively evaluate the floor water inrush to ensure safe and efficient coal mining. The 182602 working face of the Wutongzhuang coal mine served as the background for our research. The concept of “pre-mining microseisms” was proposed, and based on this, microseismic monitoring equipment was arranged on site. The correlation between microseismic events and the water abundance of an aq
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Chen, Haidong, Dawei Fang, Hongtao Gu, and Wenzhuo Huang. "Comprehensive Evaluation of Shale Reservoir Reconstruction based on Microseismic and Multidisciplinary Integration." Adsorption Science & Technology 2022 (September 22, 2022): 1–18. http://dx.doi.org/10.1155/2022/5095254.

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Microseismic can build a bridge between engineering operations such as drilling and fracturing and stratum evaluation such as earthquake, geology, and logging by fully excavating fracture time, spatial development characteristics, and focal information. For the postseismic evaluation of microseisms, a comprehensive evaluation system integrating microseisms and multidisciplines is established in this paper: through deep excavation of microseismic information such as the time and space distribution of microseismic events, quantitative statistics, magnitude-frequency gradient ( B -value) and S-P
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Dissertations / Theses on the topic "Microseisms"

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Zupo, Maria <1983&gt. "Secondary Microseisms Characterization and Green’s Function Extraction at the Larderello-Travale Geothermal Field (Italy)." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2015. http://amsdottorato.unibo.it/6973/1/Zupo_Maria_tesi.pdf.

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Over the past ten years, the cross-correlation of long-time series of ambient seismic noise (ASN) has been widely adopted to extract the surface-wave part of the Green’s Functions (GF). This stochastic procedure relies on the assumption that ASN wave-field is diffuse and stationary. At frequencies <1Hz, the ASN is mainly composed by surface-waves, whose origin is attributed to the sea-wave climate. Consequently, marked directional properties may be observed, which call for accurate investigation about location and temporal evolution of the ASN-sources before attempting any GF retrieval.
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Zupo, Maria <1983&gt. "Secondary Microseisms Characterization and Green’s Function Extraction at the Larderello-Travale Geothermal Field (Italy)." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2015. http://amsdottorato.unibo.it/6973/.

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Over the past ten years, the cross-correlation of long-time series of ambient seismic noise (ASN) has been widely adopted to extract the surface-wave part of the Green’s Functions (GF). This stochastic procedure relies on the assumption that ASN wave-field is diffuse and stationary. At frequencies <1Hz, the ASN is mainly composed by surface-waves, whose origin is attributed to the sea-wave climate. Consequently, marked directional properties may be observed, which call for accurate investigation about location and temporal evolution of the ASN-sources before attempting any GF retrieval.
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Sethi, Shipra. "Secondary microseisme Love wave generation." Thesis, Université de Paris (2019-....), 2019. https://theses.md.univ-paris-diderot.fr/SETHI_Shipra_va2.pdf.

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Le bruit sismique est l'oscillation continue de la Terre enregistrée à chaque station en l'absence de tremblement de terre. Il résulte de l'interaction entre l'atmosphère, les océans et la terre solide. Le signal dominant, appelé microséismes secondaires dans la bande de fréquences 0,1-0,3 Hz, a pour origine l'interaction non linéaire entre des ondes de gravité océaniques de même fréquence et de directions opposées. Les fluctuations de pression qui en résultent près de la surface de l'océan génèrent un signal sismique. Le signal dominant est constitué d'ondes de Rayleigh (R). Plusieurs études
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Davy, Céline. "Analyse du bruit microsismique associé à la houle dans l'océan Indien." Thesis, La Réunion, 2015. http://www.theses.fr/2015LARE0024/document.

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Les données sismologiques enregistrées sur les îles océaniques offrent l'opportunité d'analyser la houle via sa signature dans le "bruit" microsismique. Nous avons d'abord analysé les sources de bruit « secondaires », qui sont générées par l'interaction entre des vagues de même période dans une tempête, un cyclone ou par le phénomène de réflexion des vagues sur la côte. L'analyse des « microséismes secondaires », à l'échelle du bassin océanique, permet d'assurer un suivi spatio-temporel de la source qui les génère, même si elle est distante de plusieurs milliers de km des stations sismiques d'
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Reshetnikov, Anton [Verfasser]. "Microseismic reflection imaging / Anton Reshetnikov." Berlin : Freie Universität Berlin, 2013. http://d-nb.info/1045195065/34.

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Pugh, David James. "Bayesian source inversion of microseismic events." Thesis, University of Cambridge, 2016. https://www.repository.cam.ac.uk/handle/1810/253751.

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Rapid stress release at the source of an earthquake produces seismic waves. Observations of the particle motions from such waves are used in source inversion to characterise the dynamic behaviour of the source and to help in understanding the driving processes. Earthquakes either occur naturally, such as in volcanic eruptions and natural geothermal fields, or are linked to anthropogenic activities including hydrofracture of gas and oil reservoirs, mining events and extraction of geothermal fluids. Source inversion is very sensitive to uncertainties in both the model and the data, especially fo
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Leaney, W. Scott. "Microseismic source inversion in anisotropic media." Thesis, University of British Columbia, 2014. http://hdl.handle.net/2429/50045.

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Sedimentary rocks and shales in particular are known to be anisotropic, sometimes strongly so, and hydraulic fracturing is now common practice in shale plays to enhance the extraction of hydrocarbons. One of the ways to understand the hydraulic fracturing process is through the micro--earthquakes that it generates; it is therefore of interest to study the impact that anisotropy may have on hydraulically induced seismicity. This thesis is concerned with the inclusion of anisotropy into the geophysical forward and inverse problems of microseismic sources. Ray theory is used for the forward pr
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Baggaley, Paul Andrew. "Field measurements of electroseismic phenomena generated by active and passive acoustic sources." Thesis, Keele University, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.246874.

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Kat, Michael P. "Comparative studies of microseismic source location techniques." Thesis, McGill University, 1988. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=61709.

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Bishop, Ian. "Passive microseismic monitoring of a hydrofracture field trial." Thesis, Cardiff University, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.636105.

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A sandstone formation, part of the reservoir rock comprising the Beckingham Oilfield, Nottinghamshire, was fractured by the injection of water under pressure through perforated casing, at depths of 1 km. The formation breakdown, and the repeated injection of water over a period of two weeks, was monitored by five triaxial sondes situated about the injection interval and several surface mounted geophones. Four of these sondes were situated in the treatment borehole, the fifth, in an observation borehole, approximately 280 m away. No seismicity was observed in the observation well or on the surf
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Books on the topic "Microseisms"

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Ezio, Faccioli, ed. Elementi per una guida alle indagini di microzonazione sismica. Consiglio nazionale delle ricerche, 1986.

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Zaalishvili, V. B. Seĭsmicheskoe mikroraĭonirovanie territorii gorodov, naselënnykh punktov i bolʹshikh stroitelʹnykh ploshchadok. Izd-vo "Nauka", 2009.

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L, Swanson P., ed. Accuracy and precision of microseismic event locations in rock burst studies. U.S. Dept. of the Interior, Bureau of Mines, 1992.

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Swanson, P. L. Characteristics of mining-induced seismicity and rock bursting in a deep hard-rock mine. U.S. Dept. of the Interior, Bureau of Mines, 1991.

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Swanson, P. L. Characteristics of mining-induced seismicity and rock bursting in a deep hard-rock mine. U.S. Dept. of the Interior, Bureau of Mines, 1991.

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Bradley, Christopher R. Very low frequency seismo-acoustic noise below the sea floor (0.2-10 Hz). Woods Hole Oceanographic Institution, Massachusetts Institute of Technology, 1994.

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Geological Survey (U.S.), ed. Microearthquake seismology in USGS volcano and earthquake hazards studies, 1953-1995. U.S. Dept. of the Interior, U.S. Geological Survey, 1996.

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Hente, B. Automatische Bearbeitung von Seismogrammen zur mikroseismischen Überwachung des Salzbergwerks Asse. GSF-Forschungszentrum für Umwelt und Gesundheit, 1992.

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Yaramanci, U. Hochfrequenz Mikroseismizität im Steinsalz der Asse um den 945-m-Bereich. GSF-Forschungszentrum für Umwelt und Gesundheit, 1991.

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Ratcliffe, Nicholas M. Bedrock geology and seismotectonics of the Oscawana Lake Quadrangle, New York. U.S. G.P.O., 1992.

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Book chapters on the topic "Microseisms"

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Tabulevich, Valentina N. "Excitation of Microseisms and Infrasound Vibrations." In Microseismic and Infrasound Waves. Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-642-76170-6_2.

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Lyubushin, A. "Multifractal Parameters of Low-Frequency Microseisms." In Synchronization and Triggering: from Fracture to Earthquake Processes. Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-642-12300-9_15.

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Sobolev, G., and A. Lyubushin. "Periodical Oscillations of Microseisms before the Sumatra Earthquake of December 26, 2004." In Synchronization and Triggering: from Fracture to Earthquake Processes. Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-642-12300-9_13.

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Akamatsu, Junpei, Hiroshi Yasui, Keiichi Nishimura, and Masao Komazawa. "Application of Microseisms to Microzoning of an Urban Area in a Sedimentary Basin." In Earthquake Hazard and Risk. Springer Netherlands, 1996. http://dx.doi.org/10.1007/978-94-009-0243-5_19.

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Yamamoto, Tokuo, Thomas Nye, and Dean Goodman. "Concurrent Observations of Directional Spectra of Ocean Surface Waves and Microseisms from an Ocean Subbottom Seismometer (OSS) Array." In Shear Waves in Marine Sediments. Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3568-9_28.

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Zhang, Zhiyong. "Characterization and Monitoring of an Unstable Rock Face by Microseismic Methods." In Civil and Environmental Engineering for the Sustainable Development Goals. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-99593-5_8.

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AbstractUnstable rock slopes are likely to cause rockfalls, threatening human lives and properties, industrial activities, and transportation infrastructures in mountain areas. There is an increasing demand to forecast and mitigate the potential damage of rockfalls by developing a reliable early warning system. In this thesis, an unstable mountain slope in northern Italy was selected as the research target. A microseismic monitoring network has been operating since 2013 as a field research laboratory to study the microseismic monitoring technique in the perspective of developing rockfall early warning systems. Locating microseismic events is a basic step of this technique to obtain the location of developing cracks as possible precursors of rockfalls. However, it is still a challenging task due to the heterogeneity of fractured rock slopes. The main purpose of this thesis is to address the issues related to event localization for microseismic monitoring strategy applied to the unstable rock face. Graphical Abstract
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Akram, Jubran. "Microseismic Data Processing." In Understanding Downhole Microseismic Data Analysis. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-34017-9_3.

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Akram, Jubran. "Microseismic Data Interpretation." In Understanding Downhole Microseismic Data Analysis. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-34017-9_5.

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Mostafa, Ahmed E., Sheelagh Carpendale, Emilio Vital Brazil, David Eaton, Ehud Sharlin, and Mario Costa Sousa. "FractVis: Visualizing Microseismic Events." In Advances in Visual Computing. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-41939-3_37.

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Flach, D., and B. Hente. "Microseismic monitoring in salt." In Design and Instrumentation of In Situ Experiments in Underground Laboratories for Radioactive Waste Disposal. Routledge, 2022. http://dx.doi.org/10.1201/9781315140964-40.

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Conference papers on the topic "Microseisms"

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Khogoeva, E. E. "DYNAMICS OF THE EMISSION RESPONSE OF THE GEOLOGICAL MEDIUM ACCORDING TO MARINE SEISMIC DATA." In All-Russian Youth Scientific Conference with the Participation of Foreign Scientists Trofimuk Readings - 2021. Novosibirsk State University, 2021. http://dx.doi.org/10.25205/978-5-4437-1251-2-83-86.

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The present work is devoted to the study of the process of the induced emission of microseisms in an oil reservoir after the passage of elastic waves through it from shotpoint oscillations during seismic exploration. Based on the example of marine seismic data, proven the absence of spectral anomalies of microseisms at the beginning of the traces, before the arrival of waves from the source, and the occurrence of anomalies of medium-frequency microseisms in the 17–23 Hz range at late times of the seismic gathers, after the passage of reflected and multiple waves, were established. The position
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Fedin, Konstantin V., Yury I. Kolesnikov, and Luckymore Ngomayezwe. "Maping the Barsukovskaya cave by passive seismic method of standing waves." In Недропользование. Горное дело. Направления и технологии поиска, разведки и разработки месторождений полезных ископаемых. Экономика. Геоэкология. Федеральное государственное бюджетное учреждение науки Институт нефтегазовой геологии и геофизики им. А.А. Трофимука Сибирского отделения Российской академии наук, 2020. http://dx.doi.org/10.18303/b978-5-4262-0102-6-2020-073.

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The karst cave was mapped using microseisms recorded on the earth's surface. The research method is based on the effect of standing waves generation by microseisms over the cave. The accumulation of amplitude spectra of microseisms allows one to determine the frequencies of the first few modes of these waves. A map of frequency of lowest mode was constructed at the survey site. This map shows the structure of the cave in plan, as confirmed by a comparison with the cave scheme drawn up earlier by cavers.
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Uetake, Tomiichi. "Microseisms observed during typhoon passage." In The 14th SEGJ International Symposium, Online, 18–21 October 2021. Society of Exploration Geophysicists and Society of Exploration Geophysicists of Japan, 2021. http://dx.doi.org/10.1190/segj2021-076.1.

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Kerman, Bryan R., Robert F. Mereu, and Denis Roy. "Wind-induced Microseisms from Large Lakes." In Proceedings of the III International Meeting on Natural Physical Processes Related to Sea Surface Sound. WORLD SCIENTIFIC, 1996. http://dx.doi.org/10.1142/9789814447102_0010.

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Kalinina, A. V., S. M. Ammosov, R. E. Tatevosyan, A. M. Turchkov, A. N. Oshkin, and A. A. Vyaznikovtsev. "Using Microseisms in Seismic Microzonation for Critical Facilities." In Engineering and Mining Geophysics 2021. European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.202152127.

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Vesnaver, Aldo, Lara Lovisa, and Gualtiero Böhm. "Full 3D relocation of microseisms for reservoir monitoring." In SEG Technical Program Expanded Abstracts 2008. Society of Exploration Geophysicists, 2008. http://dx.doi.org/10.1190/1.3059185.

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Brusil, Carlos, Felipe Grijalva, Roman Lara-Cueva, Mario Ruiz, and Byron Acuna. "A Semi-Supervised Approach for Microseisms Classification from Cotopaxi Volcano." In 2019 IEEE Latin American Conference on Computational Intelligence (LA-CCI). IEEE, 2019. http://dx.doi.org/10.1109/la-cci47412.2019.9037033.

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Kadirov, Fakhraddin, Gulam Babayev, and Azer Gadirov. "Analysis of horizontal to vertical spectra of microseisms for Baku city." In 2012 IV International Conference "Problems of Cybernetics and Informatics" (PCI). IEEE, 2012. http://dx.doi.org/10.1109/icpci.2012.6486352.

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Lara-Cueva, Roman A., and Diana Aguinaga. "On Using Spectral Estimation for Feature Extraction of Microseisms at Cotopaxi Volcano." In 2019 14th Iberian Conference on Information Systems and Technologies (CISTI). IEEE, 2019. http://dx.doi.org/10.23919/cisti.2019.8760775.

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Forrest, Gary Stone, Tom Olsen, Aleksey Sergeevich Kazantsev, Timothy James Dombrowski, Ernest Gomez, and Wayne Rowe. "Using Microseisms to Monitor Hydraulic Fractures Within the Bakken Formation of North Dakota." In SPE Unconventional Gas Conference. Society of Petroleum Engineers, 2010. http://dx.doi.org/10.2118/131778-ms.

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Reports on the topic "Microseisms"

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Sánchez- Sesma, Francisco José, Hiroshi Kawase, and Joseline Mena Negrete. Working Paper PUEAA No. 5. The collaboration between Mexico and Japan in earthquake engineering and seismology. Universidad Nacional Autónoma de México, Programa Universitario de Estudios sobre Asia y África, 2022. http://dx.doi.org/10.22201/pueaa.003r.2022.

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Despite their remoteness from each other, Japan and Mexico share a critical characteristic: the seismic hazard. In the past, both nations have been hit by great earthquakes that have caused serious human and material losses. Although the prediction of earthquakes is not yet possible, the development of early warning systems and their constant innovation is a priority, especially the studies of the horizontal-to-vertical spectral relationship of microseisms, which can help the study and understanding of earthquakes’ nature, as well as their impact on infrastructure. It is for mutual benefit to
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Lucero, Marcus A. Microseismic tracer particles for hydraulic fracturing. Office of Scientific and Technical Information (OSTI), 2012. http://dx.doi.org/10.2172/1188153.

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Vladut, T. I. Practice of microseismic monitoring for mining activities. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/304812.

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Fehler, Michael C., Leigh S. House, and Norma J. McFarland. Locations of microseismic events for experiment 2066. Office of Scientific and Technical Information (OSTI), 1987. http://dx.doi.org/10.2172/1244409.

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Guza, R. T. Surface Gravity Waves And Ambient Microseismic Noise. Defense Technical Information Center, 1992. http://dx.doi.org/10.21236/ada256498.

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Draelos, Timothy, and Dylan Fox. Microseismic Event Denoising: Removal of Borehole Waves. Office of Scientific and Technical Information (OSTI), 2020. http://dx.doi.org/10.2172/1747001.

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Vladut, T. I. Study of microseismic emissions from a pit slope. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/304772.

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Daley, T., J. Peterson, and V. Korneev. GEO-SEQ Subtask 2.3.4: Microseismic Monitoring and Analysis. Office of Scientific and Technical Information (OSTI), 2011. http://dx.doi.org/10.2172/1016704.

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Vladut, T. I. State-of-the-art of microseismic application for mining. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/304870.

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Matzel, Eric M. Real-time Microseismic Processing for Induced Seismicity Hazard Detection. Office of Scientific and Technical Information (OSTI), 2016. http://dx.doi.org/10.2172/1332471.

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