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Relevant bibliographies by topics / Geodynamics

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Academic literature on the topic 'Geodynamics'

Author: Grafiati

Published: 4 June 2021

Last updated: 11 January 2025

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Journal articles on the topic "Geodynamics"

1

Nesterenko, Maksim, Aleksey Tsviak, and Vladimir Belov. "Natural and technogenic geodynamic processes in the south ural." E3S Web of Conferences 208 (2020): 01018. http://dx.doi.org/10.1051/e3sconf/202020801018.

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In this paper is presented hydro-geodynamics and geodynamics in the South Urals. Seismicity and geodynamics induced by hydrocarbon production by summarizing the published case studies are considered. Changes in hydro-and gas dynamics affect changes in the geodynamics of the crust. Natural and technogenic changes in bowels of the Earth are usually entail tectonic movements and deformations of earth’s surface, which is one of the important factors determining environmental changes and requiring mandatory consideration in engineering-geological surveys and exploitation of deposits. The approach is based on identified changes in hydrogeodinamics, stress-deformation state and seismic activity in areas of mineral resources of oil and gas fields. Negative geodynamic processes occurring on the territory of the Eastern Orenburg Region are identified. The analysis of the geodynamic state of the subsurface of the Eastern Orenburg Region is carried out. Based on the analysis, conclusions are made about possible causes of the geodynamic processes. An effective method for observing geodynamic processes using a seismological network is proposed and justified. A method of organizing a geodynamic polygon on a mineral field under development using a network of seismic stations has been developed.

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Lozyniak, P. Yu, A. V. Nazarevych, and L. Ye Nazarevych. "GEODYNAMICS." GEODYNAMICS 2(11)2011, no. 2(11) (September 20, 2011): 170–72. http://dx.doi.org/10.23939/jgd2011.02.170.

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In the paper on the base of analyzing of Neogene sediments` structure of Transcarpathian depression the Neogene geodynamics of the region is traced. Based on comparisons with modern data it is concluded that modern geodynamic regime of depressions` lithosphere is some continuing of transformation of Neogene geodynamic process from subcarpathian to the zonal ones with the growing of display of processes with transversal pattern and with their spatial migration (in general – from the southeast to the northwest). It is shown that the middle subcarpathian belt of heightened seismic activity in depressions is closely related to disjunctive dislocations of Neogene initiation of its axial zone.

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AKSENOV, Vladimir, Vyacheslav BEGLYAKOV, and Dmitry DUBINKIN. "SUBSTANTIATION OF THE NEED TO CREATE A NEW SCIENTIFIC DIRECTION – GEODYNAMICS OF UNDERGROUND APPARATUSES." Sustainable Development of Mountain Territories 13, no. 4 (December 20, 2021): 637–43. http://dx.doi.org/10.21177/1998-4502-2021-13-4-637-643.

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The article presents the new basic functional systems of underground devices of the “geokhod” class, as well as the problems faced by developers at all stages of the creation of experimental and prototypes of the new class of underground devices “geokhod”. The development of systems of a new class of underwater vehicles is hindered by the lack of special scientific and methodological support. The authors of the article propose the creation of a new scientific specialty “Geodynamics of underground apparatuses”. The article presents the formula of the scientific specialty “Geodynamics of underground apparatuses”; priority tasks of the scientific specialty “ Geodynamics of underground apparatuses “, within which research is carried out and primaryresults are obtained. But so far, the state of scientific and methodological support in this area is a deterrent. The development of a new scientific direction “Geodynamics of underground apparatuses” will make it possible to fill this gap. Similarly, with the Aerodynamics of aircraft, and Geodynamics of underground vehicles as a science should include the basics of two main components: geodynamics and dynamics of movement of underground vehicles. Geodynamics of underground apparatuses should determine the forces and moments acting on underground apparatuses and on the basis of this determine the rational forms of interacting surfaces. It is noted that in all known definitions and problems of geodynamics there is no binding to the definition of the interaction of the machine and the geoenvironment. The concept of “geomedia” is defined by the example of geokhod mining. The geomedia is heterogeneous and anisotropic in its properties. When a solid body interacts with a medium, the formation of an interaction surface is inevitable. For the process of motion of a solid body in a solid medium, there are two real surfaces: the surface of a moving body and the surface of the medium, the shape and dimensions of which may not coincide, perhaps even often cannot coincide. By analogy with the aerodynamic shape, it is proposed to introduce the concept of “geodynamic shape”. To reduce the forces of resistance to the movement of the underground apparatus in the geomedia and to ensure its stability, it is important not only the rational external form of the underground apparatus and its systems, but also the rational form of the surface of the geo-environment – the Geodynamic shape of the surface. In conclusion, the main tasks of Geodynamics of underground apparatuses are formulated.

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Bogusz, Janusz, Aleksander Brzezinski, Wieslaw Kosek, and Jolanta Nastula. "Earth rotation and geodynamics." Geodesy and Cartography 64, no. 2 (December 1, 2015): 201–42. http://dx.doi.org/10.1515/geocart-2015-0013.

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Abstract This paper presents the summary of research activities carried out in Poland in 2011-2014 in the field of Earth rotation and geodynamics by several Polish research institutions. It contains a summary of works on Earth rotation, including evaluation and prediction of its parameters and analysis of the related excitation data as well as research on associated geodynamic phenomena such as geocentre motion, global sea level change and hydrological processes. The second part of the paper deals with monitoring of geodynamic phenomena. It contains analysis of geodynamic networks of local, and regional scale using space (GNSS and SLR) techniques, Earth tides monitoring with gravimeters and water-tube hydrostatic clinometer, and the determination of secular variation of the Earth’ magnetic field.

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Valentina, Svalova. "Geodynamics of the Caucasus – Anatolian-Arabian region and Turkey-Syria Earthquakes 2023." Journal of Basic & Applied Sciences 19 (May 2, 2023): 40–59. http://dx.doi.org/10.29169/1927-5129.2023.19.04.

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The activation of natural disasters in the world requires the development of new approaches to the study of geological processes, in particular, at the boundaries of lithospheric plates, characterized by earthquakes, increased seismicity, volcanism, landslide processes, tsunamis and other dangerous natural processes and hazards. Earthquake of M 7.8 struck south -eastern Turkey and north - western Syria on 6 February 2023. The M 7.8 earthquake is the largest in Turkey since the 1939 Erzincan earthquake, and the second-strongest recorded in the country, after the 1668 North Anatolia earthquake. More than 52,800 deaths were confirmed: more than 46,100 in Turkey, and more than 6,700 in Syria. It is the deadliest natural disaster in Turkey's modern history. The earthquakes caused over US$100 billion in damages. The geodynamic models construction for the deep structure of natural hazards regions is an important contribution to the study of active continental margins, which is necessary for the earthquake forecast, prediction and prognosis, assessing geoecological risks and preparing population actions in the event of natural disasters and catastrophes. The Caucasus - Arabian region is a complex highly-stressed geodynamic structure, characterized by increased heat flow, high seismicity, magmatism and volcanism. The geodynamics of the Caucasus - Arabian region is determined by the collision of the Eurasian and Arabian lithosphere plates, as well as the complex history of the development of the Alpine-Himalayan belt and surrounding territories. The problem solution of geological structures formation and evolution in various complex geodynamic settings and natural hazards forecast and prognosis requires an analysis of all available geological - geophysical data, as well as the formulation and solution of problems of mechanical and mathematical modeling. Slow lithospheric deformations are simulated by models of viscous flow in multi-layered, incompressible, high-viscosity Newtonian fluid, using Navier-Stocks equation and discontinuity equation. The solution of the inverse problem of geodynamics by the direct method is developed. The first inverse problem of geodynamics was solved - the restoration of the velocity fields, pressures and stresses at the depth of the lithosphere according to the available data on the velocities on the surface. The second inverse problem of geodynamics has been posed and solved - the determination of the movement of boundaries at the depth of the lithosphere based on the given movements of the surface. The solutions obtained can be used to analyze deep geodynamic problems, and together with geothermal modeling, geological and geophysical methods and seismic tomography can serve as a reliable apparatus for studying deep geodynamics due to the formation and evolution of geological structures and the lithosphere stress-strain state researches. The solution of the problem is analyzed on the example of the Caucasus - Arabian region geodynamics. The Geodynamic concept of geoenvironment has been developed. Geodynamic models of the regions of hazardous natural processes in order to predict and prevent natural disasters and catastrophes are constructed. An algorithm for creating monitoring systems is suggested.

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Zhanibekov, Bobir, Mirali Kamalovich, Bakhtiyar Toshmukhamdov, Munira Abdunabieva, and Dilafruz Abdusamatova. "Geodynamic issues of ore deposits in Central Asia." E3S Web of Conferences 497 (2024): 02032. http://dx.doi.org/10.1051/e3sconf/202449702032.

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The focus of this study is on a pressing issue in ore geology, specifically the geodynamics of ore formation. The paper delineates a comprehensive methodology for examining the geodynamic context in regions hosting endogenous mineralization. The foundation for reconstructing geodynamics lies in geological and structural investigations into the circumstances surrounding mineralization, complemented by outcomes from physical modeling. Tectonic tension and deformation analyses of ore fields and deposits further contribute crucial insights. The study underscores that understanding the geodynamic setting is paramount for elucidating the processes leading to ore formation. This involves a detailed examination of geological structures, conditions of mineralization, and physical modeling results. By adopting this approach, the research provides a robust framework for reconstructing the geodynamic conditions prevalent during the period of ore formation. As a practical application of this methodology, the paper presents results from the reconstruction of the geodynamic situation during the ore formation period in a gold deposit situated in Western Uzbekistan. These findings contribute to a deeper comprehension of the geodynamic processes associated with the formation of valuable mineral deposits, thereby enhancing our ability to interpret and potentially predict similar occurrences in ore geology.

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Ćatić, Jasmin, and Dževad Krdžalić. "Application of Scientific Software GAMIT/GLOBK for Geodynamics in Bosnia and Herzegovina." Geodetski glasnik, no. 50 (December 31, 2019): 95–110. http://dx.doi.org/10.58817/2233-1786.2019.53.50.95.

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Global Navigation Satellite Systems (GNSS) are used for different purposes in geodesy, like engineering geodesy, land management, real estate cadastre, land surveying, etc. However, high-precision GNSS measurements are used primarly for determination of reference networks, and for investigation of geodynamical phenomena as tectonic plates movements, which is the focus of this paper. An active GNSS network of Bosnia and Herzegovina (BIHPOS) was used for calculation of coordinates and velocities of networks' stations. Data from 23 stations were processed using scientific software GAMIT/GLOBK (version 10.7), developed on MIT (Massachusetts Institute of Technology). A sub-centimeter accuracy of coordinates is achieved and accuracy of calculated velocities is better than 1 mm/year. Station velocities interpretate geodynamics of Bosnia and Herzegovina. Six IGS stations were used, as reference datum stations. Reference stations analysis results are in good match with EUREF Permanent GNSS Network velocities, while BIHPOS stations velocities (at 13 stations in Bosnia and Herzegovina) show very similar trend to the velocities obtained from regional geodynamic campaigns (CERGOP).

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Baryshev, Alexander, and Galina Khachatryan. "Geodynamics, diamondiferous system tectonics and minerageny." Domestic geology, no. 6 (January 22, 2021): 88–108. http://dx.doi.org/10.47765/0869-7175-2020-10033.

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The paper presents a unique geodynamic evolution concept of all processes and structures ensuring carbon source formation and movement for diamond crystals growth in the mantle, and diamondiferous medium supply to the surface. Geodynamic basis for diamond formation is exogenetic source sinking in old subduction zones evolving along convection cell edges. The supply is ongoing in an advection system, with transtension combined with convection playing a key role. The paper shows periods of spatial pipe cluster location and tectonophysical pattern of this phenomenon. Based on geodynamics, the authors suggest improving a taxonomical scheme of the diamondiferous system due to its fractal structure, from a mineragenic province to a pipe cluster. Specific examples are presented to highlight major structural elements of diamondiferous taxons (systems) and their formation patterns. Debatable issues of kimberlite nature are discussed.

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Shljahovyj, V. V. "GEODYNAMICS." GEODYNAMICS 1(6)2007, no. 1(6) (September 20, 2007): 60–66. http://dx.doi.org/10.23939/jgd2007.01.060.

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The digital computer geodynamic complex is used for registration of earth tides, the seismic information and other geophysical fields. It consists from high-sensitivity tidal gravimeter, autocompensatory seismotiltmeter, 24-bits ADC, computer systems of registration and the system of registration of meteoparameters. The complex is connected from a computer information network of an observatory to Internet.

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Malytskyi, D. V., R. M. Pak, E. M. Kozlovskyi, O. O. Muila, and O. I. Khytryak. "GEODYNAMICS." GEODYNAMICS 1(6)2007, no. 1(6) (September 20, 2007): 72–80. http://dx.doi.org/10.23939/jgd2007.01.072.

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This article is considered for the displacement field on the free surface of a layered medium. The relations of a wave field are checked by MATLAB. Matrix and recurrent methods give the same results for numerical calculations.

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Dissertations / Theses on the topic "Geodynamics"

1

Rands, Peter N. "European geodynamics using satellite geodesy." Thesis, University of Newcastle Upon Tyne, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.316076.

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Toth, John. "Geodynamics of the Central Andes." Thesis, University of Liverpool, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.262590.

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Ingle, Stéphanie. "Chemical geodynamics of the early kerguelen plume." Doctoral thesis, Universite Libre de Bruxelles, 2003. http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/211324.

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Hooks, Benjamin Patrick. "Geodynamics of Terrane Accretion within Southern Alaska." Fogler Library, University of Maine, 2009. http://www.library.umaine.edu/theses/pdf/HooksBP2009.pdf.

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Davies, David Rhodri. "Applying multi-resolution numerical methods to geodynamics." Thesis, Cardiff University, 2008. http://orca.cf.ac.uk/54899/.

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Computational models yield inaccurate results if the underlying numerical grid fails to provide the necessary resolution to capture a simulation's important features. For the large-scale problems regularly encountered in geodynamics, inadequate grid resolution is a major concern. The majority of models involve multi-scale dynamics, being characterized by fine-scale upwelling and downwelling activity in a more passive, large-scale background flow. Such configurations, when coupled to the complex geometries involved, present a serious challenge for computational methods. Current techniques are unable to resolve localized features and, hence, such models cannot be solved efficiently. This thesis demonstrates, through a series of papers and closely-coupled appendices, how multi-resolution finite-element methods from the forefront of computational engineering can provide a means to address these issues. The problems examined achieve multi-resolution through one of two methods. In two-dimensions (2-D), automatic, unstructured mesh refinement procedures are utilized. Such methods improve the solution quality of convection dominated problems by adapting the grid automatically around regions of high solution gradient, yielding enhanced resolution of the associated flow features. Thermal and thermo-chemical validation tests illustrate that the technique is robust and highly successful, improving solution accuracy whilst increasing computational efficiency. These points are reinforced when the technique is applied to geophysical simulations of mid-ocean ridge and subduction zone magmatism. To date, successful goal-orientated/error-guided grid adaptation techniques have not been utilized within the field of geodynamics. The work included herein is therefore the first geodynamical application of such methods. In view of the existing three-dimensional (3-D) spherical mantle dynamics codes, which are built upon a quasi-uniform discretization of the sphere and closely coupled structured grid solution strategies, the unstructured techniques utilized in 2-D would throw away the regular grid and, with it, the major benefits of the current solution algorithms. Alternative avenues towards multi-resolution must therefore be sought. A non-uniform structured method that produces similar advantages to unstructured grids is introduced here, in the context of the pre-existing 3-D spherical mantle dynamics code, TERRA. The method, based upon the multigrid refinement techniques employed in the field of computational engineering, is used to refine and solve on a radially non-uniform grid. It maintains the key benefits of TERRA's current configuration, whilst also overcoming many of its limitations. Highly efficient solutions to non-uniform problems are obtained. The scheme is highly resourceful in terms RAM, meaning that one can attempt calculations that would otherwise be impractical. In addition, the solution algorithm reduces the CPU-time needed to solve a given problem. Validation tests illustrate that the approach is accurate and robust. Furthermore, by being conceptually simple and straightforward to implement, the method negates the need to reformulate large sections of code. The technique is applied to highly advanced 3-D spherical mantle convection models. Due to its resourcefulness in terms of RAM, the modified code allows one to efficiently resolve thermal boundary layers at the dynamical regime of Earth's mantle. The simulations presented are therefore at superior vigor to the highest attained, to date, in 3-D spherical geometry, achieving Rayleigh numbers of order 109. Upwelling structures are examined, focussing upon the nature of deep mantle plumes. Previous studies have shown long-lived, anchored, coherent upwelling plumes to be a feature of low to moderate vigor convection. Since more vigorous convection traditionally shows greater time-dependence, the fixity of upwellings would not logically be expected for non-layered convection at higher vigors. However, such configurations have recently been observed. With hot-spots widely-regarded as the surface expression of deep mantle plumes, it is of great importance to ascertain whether or not these conclusions are valid at the dynamical regime of Earth's mantle. Results demonstrate that at these high vigors, steady plumes do arise. However, they do not dominate the planform as in lower vigor cases: they coexist with mobile and ephemeral plumes and display ranging characteristics, which are consistent with hot-spot observations on Earth. Those plumes that do remain steady alter in intensity throughout the simulation, strengthening and weakening over time. Such behavior is caused by an irregular supply of cold material to the core-mantle boundary region, suggesting that subducting slabs are partially responsible for episodic plume magmatism on Earth. With this in mind, the influence of the upper boundary condition upon the planform of mantle convection is further examined. With the modified code, the CPU-time needed to solve a given problem is reduced and, hence, several simulations can be run efficiently, allowing a relatively rapid parameter space mapping of various upper boundary conditions. Results, in accordance with the investigations on upwelling structures, demonstrate that the surface exerts a profound control upon internal dynamics, manifesting itself not only in convective structures, but also in thermal profiles, Nusselt numbers and velocity patterns. Since the majority of geodynamical simulations incorporate a surface condition that is not at all representative of Earth, this is a worrying, yet important conclusion. By failing to address the surface appropriately, geodynamical models, regardless of their sophistication, cannot be truly applicable to Earth. In summary, the techniques developed herein, in both 2- and 3-D, are extremely practical and highly efficient, yielding significant advantages for geodynamical simulations. Indeed, they allow one to solve problems that would otherwise be unfeasible.

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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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Martin, Erin Lee. "Understanding Neoproterozoic geodynamics through Hafnium isotope arrays." Thesis, Curtin University, 2020. http://hdl.handle.net/20.500.11937/80148.

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The Neoproterozoic supercontinent Rodinia assembled by the collision of a global-scale subduction girdle at the end of the Mesoproterozoic. A new subduction girdle is not established until the assembly of Gondwana some 500 Ma later, at the end of the Neoproterozoic. Thus, the global Hf isotope record suggests that the Neoproterozoic was dominated by the degree-1 condition, which facilitated Gondwana amalgamation, but it is not clear that degree-2 mantle convection facilitated the breakup of Rodinia.

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Lee, Hyongki. "Radar Altimetry Methods for Solid Earth Geodynamics Studies." The Ohio State University, 2008. http://rave.ohiolink.edu/etdc/view?acc_num=osu1221761881.

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Meredith, David. "2-D and 3-D computer modelling of lithosphere dynamics and sedimentary basin formation." Thesis, Keele University, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.288437.

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Daniel, Andrew John. "The geodynamics of spreading centre subduction in southern Chile." Thesis, University of Liverpool, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.320503.

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Books on the topic "Geodynamics"

1

Gerald, Schubert, and Turcotte Donald Lawson, eds. Geodynamics. 2nd ed. Cambridge: Cambridge University Press, 2002.

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M, Atkinson Peter, ed. GeoDynamics. Boca Raton: CRC Press, 2005.

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Henri-Claude, Nataf, and Aubouin Jean, eds. Geodynamics. Lisse [Netherlands]: A.A. Balkema Publishers, 2001.

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GeoComputation. GeoDynamics. Boca Raton, FL: CRC Press, 2005.

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Morra, Gabriele. Pythonic Geodynamics. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-55682-6.

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Lallemand, Serge, and Francesca Funiciello, eds. Subduction Zone Geodynamics. Berlin, Heidelberg: Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-540-87974-9.

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Serge, Lallemand, and Funicello Francesca, eds. Subduction zone geodynamics. Berlin: Springer, 2009.

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A, Ziegler Peter, ed. Geodynamics of rifting. Amsterdam: Elsevier, 1992.

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Dobret͡sov, Nikolaĭ Leontʹevich. Deep-level geodynamics. Rotterdam: A.A. Balkema, 1998.

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Serge, Lallemand, and Funicello Francesca, eds. Subduction zone geodynamics. Berlin: Springer, 2009.

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Book chapters on the topic "Geodynamics"

1

Forte, Alessandro M. "Geodynamics." In Encyclopedia of Solid Earth Geophysics, 1–2. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-10475-7_214-1.

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Freymueller, Jeff. "Geodynamics." In Springer Handbook of Global Navigation Satellite Systems, 1063–106. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-42928-1_37.

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Forte, Alessandro M. "Geodynamics." In Encyclopedia of Solid Earth Geophysics, 340–41. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-8702-7_214.

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Forte, Alessandro M. "Geodynamics." In Encyclopedia of Solid Earth Geophysics, 452–54. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-58631-7_214.

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Morra, Gabriele. "Applications to Geodynamics." In Lecture Notes in Earth System Sciences, 201–7. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-55682-6_12.

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Chamley, Hervé. "Clay and Geodynamics." In Clay Sedimentology, 527–61. Berlin, Heidelberg: Springer Berlin Heidelberg, 1989. http://dx.doi.org/10.1007/978-3-642-85916-8_20.

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Alizadeh, Akif, Fakhraddin A. Kadirov, Samir Mammadov, Michael Floyd, Robert Reilinger, and Lev V. Eppelbaum. "Geodynamics and Seismology." In Geosciences of Azerbaijan, 219–58. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-40493-6_6.

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Ghosh, Parthasarathi, and Dhurjati P. Sengupta. "Geodynamics of Gondwanaland." In Geodynamics of the Indian Plate, 213–32. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-15989-4_7.

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"geodynamics." In Dictionary Geotechnical Engineering/Wörterbuch GeoTechnik, 594. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-41714-6_70601.

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"Geodynamics." In Learned and Applied Soil Mechanics, 135. Taylor & Francis, 2002. http://dx.doi.org/10.1201/noe9058093578-25.

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Conference papers on the topic "Geodynamics"

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Komatina, M., and S. Komatina-Petrovic. "Geodynamics of Serbia." In 5th Congress of Balkan Geophysical Society. European Association of Geoscientists & Engineers, 2009. http://dx.doi.org/10.3997/2214-4609-pdb.126.6564.

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Hamilton, Warren B. "GEODYNAMICS THROUGH TIME." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283437.

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Korotaev, M. V., A. M. Nikishin, A. V. Ershov, and M. F. Brunet. "Black Sea Basin - Geodynamics and Modelling." In 64th EAGE Conference & Exhibition. European Association of Geoscientists & Engineers, 2002. http://dx.doi.org/10.3997/2214-4609-pdb.5.p074.

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Mladenovic, M. "On Some Problems Related to Geodynamics." In 5th Congress of Balkan Geophysical Society. European Association of Geoscientists & Engineers, 2009. http://dx.doi.org/10.3997/2214-4609-pdb.126.6566.

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Morra, Gabriele. "THE EASY WAY TO COMPUTATIONAL GEODYNAMICS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-283865.

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Cohen, Steven C., and John J. Degnan. "Geodynamics Applications Of Spaceborne Laser Ranging." In OE/LASE '89. SPIE, 1989. http://dx.doi.org/10.1117/12.951874.

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Chipizubov, AV. "Modern geodynamics of the Baikal region." In Geological and geophysical environment and the various manifestations of seismicity. LJournal, 2015. http://dx.doi.org/10.18411/svfu1230915-35.

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Chen, Xinbao, ChaoKui Li, Dongshui Zhang, and Ning Qian. "Visualization Methods by using graphs for Geodynamics*." In 2014 3rd International Workshop on Earth Observation and Remote Sensing Applications (EORSA). IEEE, 2014. http://dx.doi.org/10.1109/eorsa.2014.6927884.

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Koci, Rrexhep. "GEODYNAMICS AND EROSION ALONG THE ALBANIAN COASTLINE." In 17th International Multidisciplinary Scientific GeoConference SGEM2017. Stef92 Technology, 2017. http://dx.doi.org/10.5593/sgem2017/11/s01.026.

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Meçaj, M., E. Dushi, and R. Koçi. "The present geodynamics and kinematics of albanides." In 10th Congress of the Balkan Geophysical Society. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201902654.

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Reports on the topic "Geodynamics"

1

Andrews, J. T., and W. R. Peltier. Summary [Chapter 8: Quaternary Geodynamics in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131624.

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Andrews, J. T. Introduction [Chapter 8: Quaternary Geodynamics in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131626.

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Keen, C. E., and C. Beaumont. Chapter 9: Geodynamics of Rifted Continental Margins. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/132714.

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Bower, D. R., J. J. Labreque, A. Lambert, and E. M. Mitchell. Charlevoix geodynamics observatory data inventory (1979-1986). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/315273.

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Andrews, J. T. Postglacial Emergence and Submergence [Chapter 8: Quaternary Geodynamics in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131630.

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Peltier, W. R. Models of Glacial Isostasy [Chapter 8: Quaternary Geodynamics in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131632.

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Bower, D. R. Well-level monitoring at the Charlevoix geodynamics observatory 1979-1986. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/315276.

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Lambert, A., J. O. Liard, P. N. Courtier, A. K. Goodacre, and R. K. McConnell. The Geological Survey of Canada absolute gravity program: applications in geodesy and geodynamics. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/122728.

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Andrews, J. T. Nature of the Last Glaciation in Canada [Chapter 8: Quaternary Geodynamics in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131628.

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Gable, C., B. J. Travis, R. J. O`Connell, and H. A. Stone. Interface deformation in low reynolds number multiphase flows: Applications to selected problems in geodynamics. Office of Scientific and Technical Information (OSTI), June 1995. http://dx.doi.org/10.2172/80379.

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