Relevant bibliographies by topics / Global seismology

Academic literature on the topic 'Global seismology'

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Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Global seismology"

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Gilbert, Freeman. "Theoretical Global Seismology." Eos, Transactions American Geophysical Union 80, no. 7 (1999): 79. http://dx.doi.org/10.1029/99eo00054.

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Ballai, I. "Global Coronal Seismology." Solar Physics 246, no. 1 (April 5, 2007): 177–85. http://dx.doi.org/10.1007/s11207-007-0415-3.

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Dahlen, F. A., Jeroen Tromp, and Thorne Lay. "Theoretical Global Seismology." Physics Today 52, no. 8 (August 1999): 61–62. http://dx.doi.org/10.1063/1.882788.

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Anonymous. "Reflection Seismology: A Global Perspective Reflection Seismology: The Continental Crust." Eos, Transactions American Geophysical Union 66, no. 47 (1985): 1184. http://dx.doi.org/10.1029/eo066i047p01184.

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Ni, J. "New trends in global seismology." Eos, Transactions American Geophysical Union 72, no. 35 (1991): 369. http://dx.doi.org/10.1029/90eo00285.

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Banerjee, D. "Observational review on global waves." Proceedings of the International Astronomical Union 3, S247 (September 2007): 369–76. http://dx.doi.org/10.1017/s1743921308015111.

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AbstractWith multi-wavelength observations from ground and space-based instruments it has been possible to detect waves in a number of different wavelengths simultaneously and to, consequently, study their propagation properties. High-resolution wave observations combined with forward MHD modelling can give an unprecedented insight into the connectivity of the magnetized solar atmosphere, which further gives us a realistic chance to construct the structure of the magnetic field in the stellar atmosphere. This type of exploration is also termed as magnetic seismology. In this review I will focus on global waves, like EIT waves. I will also address the possibility of finding out the properties of magnetic structures while studying the interaction of global waves with coronal loops. A Promising new way to probe stellar atmosphere is to use our knowledge of coronal seismology on the Sun and to apply it to more distant stars. It will also enable us to measure properties such as the lengths of loops linked with stellar flares and the strengths of coronal magnetic fields on stars. In the last part I will review the current status of the stellar coronal seismology.
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Schweitzer, Johannes, and Thorne Lay. "IASPEI: its origins and the promotion of global seismology." History of Geo- and Space Sciences 10, no. 1 (April 16, 2019): 173–80. http://dx.doi.org/10.5194/hgss-10-173-2019.

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Abstract. International cooperation in seismology emerged rapidly at the beginning of the 20th century following the successful recording of earthquakes at great distances. The International Seismological Association (ISA) founded in 1904 was dissolved in 1922 and evolved into the Seismology Section of the International Union of Geodesy and Geophysics (IUGG), ultimately becoming the International Association of Seismology and Physics of the Earth's Interior (IASPEI) to recognize the important role of the structure and physical properties of the Earth. Through the last hundred years, the commissions and working groups of the association have played a major role in setting international standards in such areas as the naming of seismic phases, data exchanges, travel-time tables, magnitude scales, and reference Earth models. The activities of IASPEI continue to have a focus on the societal impacts of earthquakes and tsunamis, with four regional commissions playing a major role in promoting high standards of seismological education, outreach, and international scientific cooperation.
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Albini, Paola, Roger M. W. Musson, Andrea Rovida, Mario Locati, Antonio A. Gomez Capera, and Daniele Viganò. "The Global Earthquake History." Earthquake Spectra 30, no. 2 (May 2014): 607–24. http://dx.doi.org/10.1193/122013eqs297.

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The study of earthquakes from historical sources, or historical seismology, was considered an early priority for the Global Earthquake Model (GEM) project, which commissioned a study of historical seismicity on a global scale. This was the Global Earthquake History (GEH) project, led jointly by the Istituto Nazionale di Geofisica e Vulcanologia (INGV; Milan, Italy) and the British Geological Survey (BGS; UK). GEH was structured around three complementary deliverables: archive, catalog, and the Web infrastructure designed to store both the archive and catalog. The Global Historical Earthquake Archive (GHEA) provides a complete account of the global situation in historical seismology for large earthquakes. From GHEA, the Global Historical Earthquake Catalogue (GHEC v1.0) was derived—a world catalog of earthquakes for the period 1000–1903, with magnitudes of Mw7 and over. Though much remains to be done, the data here presented show that the compilation of both archive and catalog contribute to an improved understanding of the Global Earthquake History.
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Mosser, B. "Giant planets seismology." Symposium - International Astronomical Union 181 (1997): 251–64. http://dx.doi.org/10.1017/s0074180900061192.

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The giant planets Jupiter and Saturn belong to the interesting category of possible goals for remote seismic analysis. Their first seismic observations and their analysis were attempted in 1987 and 1991 respectively, under Philippe Delache's initiative. The theoretical analysis of giant planets seismology reveals the strong signature of the dense planetary core and the tiny one of the hydrogen plasma phase transition. The asymptotic formalism makes possible to obtain pertinent information for the observation of planetary oscillations and for their analysis. Specific observational techniques were developed to detect the seismic signature of giant planets. However, the first observations (Schmider et al. 1991, Mosser et al. 1993) of Jovian oscillations remain tentative. Even if the Jovian origin of the signal is beyond doubt, the interpretation in terms of Jovian global modes remains speculative. The collision of comet SL9 onto Jupiter provided an unexpected and unique opportunity to search for oscillations excited by the cometary impacts (Mosser et al. 1996). Seismic observations of Saturn remain negative so far. Therefore, this review focuses on Jupiter. Finally, the almost 10-years long experience of seismic observations of Jupiter and Saturn has not yet provided new constraints for planetary interior models. However, guidelines for future observational projects dedicated to Jovian seismology can be drawn. The different techniques of observation are compared, and observational requirements are precisely described.
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Pavlis, G. L. ""Modern Global Seismology" by Thorne Lay and Terry Wallace." Seismological Research Letters 66, no. 6 (November 1, 1995): 92. http://dx.doi.org/10.1785/gssrl.66.6.92.

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Dissertations / Theses on the topic "Global seismology"

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

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

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In Chapter 2, we consider the hydrostatic equilibrium figure of a rotating earth model with arbitrary radial density profile. We derive an exact non-linear partial differential equation describing the equilibrium figure. Perturbation theory is used to obtain approximate forms of this equation, and we show that the first-order theory is equivalent to Clairaut's equation. In Chapter 3, a method for parametrizing the possible equilibrium stress fields of a laterally heterogeneous earth model is described. In this method a solution of the equilibrium equations is first found that satisfies some desirable physical property. All other solutions can be written as the sum of this equilibrium stress field and a divergence-free stress tensor field whose boundary tractions vanish. In Chapter 4, we consider the minor vector method for the stable numerical solution of systems of linear ordinary differential equations. Results are presented for the application of the method to the calculation of seismic displacement fields in spherically symmetric, self-gravitating earth models. In Chapter 5, we present a new implementation of the direct solution method for calculating normal mode spectra in laterally heterogeneous earth models. Numerical tests are presented to demonstrate the validity and effectiveness of this method for performing large mode coupling calculations. In Chapter 6, we consider the theoretical basis for the viscoelastic normal mode method which is used in studies of seismic wave propagation, post-glacial rebound, and post-seismic deformation. We show how the time-domain solution to the viscoelastodynamic equation can be written as a normal mode sum in a rigorous manner.
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Peter, Daniel B. "Finite-frequency effects in global seismology : forward modeling and implications on tomographic imaging /." Zürich : ETH, 2008. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=17807.

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Chambers, Kit. "Seismological modelling of global earth structure." Thesis, University of Oxford, 2005. http://ora.ox.ac.uk/objects/uuid:68d66555-8948-404e-888e-48952ccf989d.

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Upper mantle discontinuities from PP- and SS-precursors The 410km discontinuity is examined using two global datasets of precursors to the PP and SS phases. The precursor amplitudes are used to constrain the impedance contrast, and examine lateral variations in the reflection coefficient of the discontinuity. P- and S-wave reflection amplitudes vary over different scale lengths, which could be due to the presence of melt, water or other chemical heterogeneities in the transition zone. Models for 410-topography are also derived, and the relationship between topography and transition zone seismic velocity anomalies examined. A moderate negative correlation exists between long wavelength 410-topography and transition zone velocity anomalies. However, when shorter wavelengths are included the relationship becomes more complex, and in some regions positive correlations are seen. This suggests that long wavelength variation of discontinuity topography and seismic velocity, is due to thermal effects. However, at shorter wavelengths the influence of chemical heterogeneities becomes important. Different spectra for thermal and chemical heterogeneity suggests that chemical anomalies can survive in convecting mantle. Lower mantle reflectors and S-wave scattering The lowermost mantle is investigated using a phase stripping technique and two migration methods: a backprojection, and a scheme with weights based on the Generalised Radon Transform. Resolution of the results is tested by migrating synthetic datasets. In some regions the results can be simulated using fairly simple distributions of point scatterers, but elsewhere the results require more complicated structures. The results identify several important properties of the D" region including reflectors within the D" region and a complex pattern of positive and negative scattering potentials near the core-mantle boundary. The results also show the presence of an intermittent D" discontinuity which is not a continuous, nor a global, feature. This suggests that the D" discontinuity is caused by either localised structures, such as thermal or chemical heterogeneity, or a global boundary with a variable impedance contrast.
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Chao, Kevin Tzu-Kai. "Global search of triggered non-volcanic tremor." Diss., Georgia Institute of Technology, 2012. http://hdl.handle.net/1853/44779.

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Deep non-volcanic tremor is a newly discovered seismic phenomenon with low amplitude, long duration, and no clear P- and S-waves as compared with regular earthquake. Tremor has been observed at many major plate-boundary faults, providing new information about fault slip behaviors below the seismogenic zone. While tremor mostly occurs spontaneously (ambient tremor) or during episodic slow- slip events (SSEs), sometimes tremor can also be triggered during teleseismic waves of distance earthquakes, which is known as "triggered tremor". The primary focus of my Ph.D. work is to understand the physical mechanisms and necessary conditions of triggered tremor by systematic investigations in different tectonic regions. These include Taiwan, California, southwest Japan, Alaska and the Aleutian Arc, Cascadia, and New Zealand. In the first chapter of my dissertation, I conduct a systematic survey of triggered tremor beneath the Central Range (CR) in Taiwan for 45 teleseismic earthquakes from 1998 to 2009 with Mw ≥ 7.5. Triggered tremors are visually identified as bursts of high-frequency (2-8 Hz), non-impulsive, and long-duration seismic energy that are coherent among many seismic stations and modulated by the teleseismic surface waves. A total of 9 teleseismic earthquakes has triggered clear tremor in Taiwan. The peak ground velocity (PGV) of teleseismic surface waves is the most important factor in determining tremor triggering potential, with an apparent threshold of ~0.1 cm/s, or 7-8 kPa. However, such threshold is partially controlled by the background noise level, preventing triggered tremor with weaker amplitude from being observed. In addition, I find a positive correlation between the PGV and the triggered tremor amplitude, which is consistent with the prediction of the 'clock-advance' model. This suggests that triggered tremor can be considered as a sped-up occurrence of ambient tremor under fast loading from the passing surface waves. Finally, the incident angles of surface waves also play an important rule in controlling the tremor triggering potential. The next chapter focuses on a systematic comparison of triggered tremor around the Calaveras Fault (CF) in northern California (NC), the Parkfield-Cholame section of the San Andreas Fault (SAF) in central California (CC), and the San Jacinto Fault (SJF) in southern California (SC). Out of 42 large (Mw ≥7.5) earthquakes between 2001 and 2010, only the 2002 Mw 7.9 Denali fault earthquake triggered clear tremor in NC and SC. In comparison, abundant triggered and ambient tremor has been observed in CC. Further analysis reveal that the lack of triggered tremor observations in SC and NC is not simply a consequence of their different background noise levels as compared to CC, but rather reflects different background tremor rates in these regions. In the final chapter, I systematically search for triggered tremor following the 2011 Mw9.0 Tohoku-Oki earthquake in the regions where ambient or triggered tremor has been found before. The main purpose is to check whether triggered tremor is observed in regions when certain conditions (e.g., surface wave amplitudes) are met. Triggered tremor is observed in southwest Japan, Taiwan, the Aleutian Arc, south-central Alaska, northern Vancouver Island, the Parkfield-Cholame section of the SAF in CC and the SJF in SC, and the North Island of New Zealand. Such a widespread triggering of tremor is not too surprising because of the large amplitude surface waves (minimum peak value of ~0.1 cm/s) and the associated dynamic stresses (at least ~7-8 kPa), which is one of the most important factors in controlling the triggering threshold. The triggered tremor in different region is located close to or nearby the ambient tremor active area. In addition, the amplitudes of triggered tremor have positive correlations with the amplitudes of teleseismic surface waves among many regions. Moreover, both Love and Rayleigh waves participate in triggering tremor in different regions, and their triggering potential is somewhat controlled by the incident angles. In summary, systematically surveys of triggered tremor in different tectonic regions reveal that triggered tremor shares similar physical mechanism (shear failure on the fault interface) as ambient tremor but with different loading conditions. The amplitude of the teleseismic surface wave is one of the most important factors in controlling the tremor triggering threshold. In addition, the frequency contents and incident angles of the triggering waves, and local fault geometry and ambient conditions also play certain roles in determining the triggering potential. On the other hand, the background noise level and seismic network coverage and station quality also could affect the apparent triggering threshold. Because triggered tremor occurs almost instantaneously during the teleseismic surface waves, and the tremor amplitude is somewhat controlled by the amplitude of the triggering waves, the occurrence time and the size of the triggered tremor could be somewhat predictable, so long as we know the amplitude and period of surface waves and associated time-varying dynamic stresses. Hence, further analysis of triggered tremor may provide important new clues on the nucleation and predictability of seismic events.
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Cai, Zhiyuan. "Global Mohorovicic Discontinuity Estimates Based on Isostatic Theories Using Gravity Data and Seismic Models." The Ohio State University, 2020. http://rave.ohiolink.edu/etdc/view?acc_num=osu159455139426099.

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Convers, Jaime Andres. "Global investigations of radiated seismic energy and real-time implementation." Diss., Georgia Institute of Technology, 2013. http://hdl.handle.net/1853/50356.

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This dissertation contains investigations of radiated seismic energy measurements from large earthquakes and duration determinations as significant properties of the dynamic earthquake rupture and its applications in the identification of very large and slow source rupturing earthquakes. This includes a description of earthquake released seismic energy from 1997 to 2010 and identification of slow source tsunami earthquakes in that time period. The implementation of these measurements in real-time since the beginning of 2009, with a case study of the Mentawai 2010 tsunami earthquake are also discussed. Further studies of rupture duration assessments and its technical improvements for more rapid and robust solutions are investigated as well, with application to the Tohoku-Oki 2011 earthquake an a case of directivity in the 2007 Mw 8.1 Solomon islands earthquake. Finally, the set of routines and programs developed for implementation at Georgia Tech and IRIS to produce the real-time results since 2009 presented in this study are described.
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Adedeji, Elijah A. "3D Post-stack Seismic Inversion using Global Optimization Techniques: Gulf of Mexico Example." ScholarWorks@UNO, 2016. http://scholarworks.uno.edu/td/2231.

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Seismic inversion using a global optimization algorithm is a non-linear, model-driven process. It yields an optimal solution of the cost function – reflectivity/acoustic impedance, when prior information is sparse. The inversion result offers detailed interpretations of thin layers, internal stratigraphy, and lateral continuity and connectivity of sand bodies. This study compared two stable and robust global optimization techniques, Simulated Annealing (SA) and Basis Pursuit Inversion (BPI) as applied to post-stack seismic data from the Gulf of Mexico. Both methods use different routines and constraints to search for the minimum error energy function. Estimation of inversion parameters in SA is rigorous and more reliable because it depends on prior knowledge of subsurface geology. The BPI algorithm is a more robust deterministic process. It was developed as an alternative method to incorporating a priori information. Results for the Gulf of Mexico show that BPI gives a better stratigraphic and structural actualization due to its capacity to delineate layers thinner than the tuning thickness. The SA algorithm generates both absolute and relative impedances, which provide both qualitative and quantitative characterization of thin-bed reservoirs.
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Yang, Qian. "Applications of Satellite Geodesy in Environmental and Climate Change." Scholar Commons, 2016. http://scholarcommons.usf.edu/etd/6440.

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Satellite geodesy plays an important role in earth observation. This dissertation presents three applications of satellite geodesy in environmental and climate change. Three satellite geodesy techniques are used: high-precision Global Positioning System (GPS), the Gravity Recovery and Climate Experiment (GRACE) and Interferometric Synthetic Aperture Radar (InSAR). In the first study, I use coastal uplift observed by GPS to study the annual changes in mass loss of the Greenland ice sheet. The data show both spatial and temporal variations of coastal ice mass loss and suggest that a combination of warm atmospheric and oceanic condition drove these variations. In the second study, I use GRACE monthly gravity change estimates to constrain recent freshwater flux from Greenland. The data show that Arctic freshwater flux started to increase rapidly in the mid-late 1990s, coincident with a decrease in the formation of dense Labrador Sea Water, a key component of the deep southward return flow od the Atlantic Meridional Overturning Circulation (AMOC). Recent freshening of the polar oceans may be reducing formation of Labrador Sea Water and hence may be weakening the AMOC. In the third study, I use InSAR to monitor ground deformation caused by CO2 injection at an enhanced oil recovery site in west Texas. Carbon capture and storage can reduce CO2 emitted from power plants, and is a promising way to mitigate anthropogenic warming. From 2007 to 2011, ~24 million tons of CO2 were sequestered in this field, causing up to 10 MPa pressure buildup in a reservoir at depth, and surface uplift up to 10 cm. This study suggests that surface displacement observed by InSAR is a cost-effective way to estimate reservoir pressure change and monitor the fate of injected fluids at waste disposal and CO2 injection sites.
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Rogister, Yves. "Modes normaux de modèles de Terre en rotation." Habilitation à diriger des recherches, Université de Strasbourg, 2012. http://tel.archives-ouvertes.fr/tel-00773648.

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The normal-mode spectrum of rotating Earth models is made up of the seismic modes, the rotational modes and the spectrum of the liquid core. The local equations for the infinitesimal elastic-gravitational deformation, based on a Lagrangian perturbation of a spherically-averaged Earth model using the theory of hydrostatic equilibrium, are first established. A comparison is made between this approach and the classical global angular momentum approach to Earth rotation variations. The splitting of the seismic modes by rotation and ellipticity is then computed. Numerical investigation also shows that, by changing the structure of the liquid core, the rotational modes and core spectrum interact to give rise to avoided crossings, which provide a physically plausible mechanism to explain the observed double frequency of the Chandler wobble. The analogy with other oscillatory physical systems allows for a better understanding of the avoided crossing phenomenon.
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Books on the topic "Global seismology"

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Jeroen, Tromp, ed. Theoretical global seismology. Princeton, N.J: Princeton University Press, 1998.

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Lay, Thorne. Modern global seismology. San Diego: Academic Press, 1995.

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Çemen, İbrahim, and Yücel Yılmaz. Active Global Seismology. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781118944998.

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Barazangi, Muawia, and Larry Brown, eds. Reflection Seismology: A Global Perspective. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/gd013.

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Arrays and array methods in global seismology. Dordrecht: Springer, 2010.

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Gu, Yu Jeffrey, ed. Arrays and Array Methods in Global Seismology. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-3680-3.

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Levin, Boris. Seĭsmichnostʹ Tikhookeanskogo regiona: Vyi︠a︡vlenie globalʹnykh zakonomernosteĭ = Seismicity of the Pacific Region : global feature detection. Moskva: "I︠A︡nus-K", 2012.

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McLeod, David Brian. An atmospheric transmission gradient monitor for global solar seismology. Birmingham: University of Birmingham, 1991.

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1945-, Nolet Guust, ed. Seismic tomography: With applications in global seismology and exploration geophysics. Dordrecht, Holland: D. Reidel, 1987.

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Murray, Mark Hunter. Global positioning system measurement of crustal deformation in central California. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1991.

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Book chapters on the topic "Global seismology"

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Schneider, John F., Jephraim Oro, Anselm Smolka, Peter Suhadolc, and Zhongliang Wu. "Seismology, Global Earthquake Model." In Encyclopedia of Solid Earth Geophysics, 1–8. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-10475-7_164-1.

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Suhadolc, Peter. "Seismology, Global Earthquake Model." In Encyclopedia of Solid Earth Geophysics, 1334–40. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-8702-7_164.

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Schneider, John F., Jephraim Oro, Anselm Smolka, Peter Suhadolc, and Zhongliang Wu. "Seismology, Global Earthquake Model." In Encyclopedia of Solid Earth Geophysics, 1661–69. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-58631-7_164.

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Çemen, İbrahim, and Yücel Yılmaz. "Neotectonics and Earthquake Potential of the Eastern Mediterranean Region." In Active Global Seismology, 1–8. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781118944998.ch1.

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Askan, Aysegul, Shaghayegh Karimzadeh, and Mustafa Bilal. "Seismic Intensity Maps for the Eastern Part of the North Anatolian Fault Zone (Turkey) Based on Recorded and Simulated Ground-Motion Data." In Active Global Seismology, 273–87. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781118944998.ch10.

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Yılmaz, Yücel. "Morphotectonic Development of Anatolia and the Surrounding Regions." In Active Global Seismology, 9–91. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781118944998.ch2.

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Celâl Şengör, A. M. "Diversion of River Courses Across Major Strike-Slip Faults and Keirogens." In Active Global Seismology, 93–101. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781118944998.ch3.

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Mahatsente, Rezene, Süleyman Alemdar, and İbrahim Çemen. "Effect of Slab-Tear on Crustal Structure in Southwestern Anatolia." In Active Global Seismology, 103–19. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781118944998.ch4.

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Göğüş, Oğuz H., Russell N. Pysklywec, and Claudio Faccenna. "Geodynamical Models for Continental Delamination and Ocean Lithosphere Peel Away in an Orogenic Setting." In Active Global Seismology, 121–39. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781118944998.ch5.

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Yılmaz, Yücel. "Major Problems of Western Anatolian Geology." In Active Global Seismology, 141–87. Hoboken, NJ, USA: John Wiley & Sons, Inc., 2017. http://dx.doi.org/10.1002/9781118944998.ch6.

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Conference papers on the topic "Global seismology"

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Laske, Gabi. "Resolution issues in global surface wave seismology." In International Symposium on Optical Science and Technology, edited by Michael A. Fiddy and Rick P. Millane. SPIE, 2000. http://dx.doi.org/10.1117/12.409258.

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Prabowo, Aditya Rio, Jung Min Sohn, Dong Myung Bae, and Agus Setiyawan. "Crashworthiness Assessment of Thin-Walled Bottom Structures During Powered-Hard Grounding Accidents." In ASME 2018 37th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2018. http://dx.doi.org/10.1115/omae2018-77492.

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Advance development in engineering and technology has been massively triggered by establishment of the free market memorandum between countries across the globe. Explicitly, this agreement affects ship and offshore industries, where stakeholder and investor demand a wide range of accidental damage assessment. Achievement of this objective is highly influenced by sustainable research on maritime accidents. Ship grounding is categorized in impact phenomena, and record has evidenced grounding as the most risky accident. Since it is capable to evoke massive losses, estimation of structural performance and limit under grounding is required. This work aims to evaluate crashworthiness of a thin-walled tanker structures in encountering ship grounding. A series of benchmark simulations based on pioneer experimental test is re-performed as calibration of numerical configuration for grounding analysis. Several scenarios are designed in this stage by varying mesh sizes on the idealized test geometry. Preparation for the grounding analysis is presented in the next stage. Considering its characteristic as impact load, powered-hard scenario is taken into account as the worst possible damage on the structures. It is assumed that grounding happens suddenly when the tanker is in a voyage and interacts with a hard object. A medium-carbon steel is embedded with the Det Norske Veritas - Germanischer Lloyd (DNVGL) fracture criterion. In this study, an oceanic obstruction is defined as seabed reef geometry with the properties are adopted based on data of ocean crustal seismology. Varieties of location, angle and elevation are applied to accidental grounding scenarios. The assessment of structural crashworthiness brings an insight into the effect sensitivity of the parameters on the double bottom behavior. Brief recommendation for grounding simulation is provided in final conclusion to give adequate references in applying numerical input and configuration, especially using the finite element (FE) method.
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Reports on the topic "Global seismology"

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Map showing global distribution of seismicity, 1977-1986, prepared by National Earthquake Information Center, World Data Center A for Seismology. US Geological Survey, 1988. http://dx.doi.org/10.3133/gp989.

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Map showing global distribution of first-motion focal mechanisms, 1981-1985, prepared by National Earthquake Information Center, World Data Center A for Seismology. US Geological Survey, 1988. http://dx.doi.org/10.3133/gp990.

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Map showing global distribution of moment-tensor focal mechanisms, 1981-1985, prepared by National Earthquake Information Center, World Data Center A for Seismology. US Geological Survey, 1988. http://dx.doi.org/10.3133/gp991.

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