geodynamics

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ge·o·dy·nam·ics

 (jē′ō-dī-năm′ĭks)
n.
1. (used with a sing. verb) The branch of dynamics that is concerned with the causes and effects of forces and motions involving the earth's interior, including rotation, plate tectonics, volcanic eruptions, and seismic modeling.
2. (used with a pl. verb) The forces and motions involving the earth's interior.
American Heritage® Dictionary of the English Language, Fifth Edition. Copyright © 2016 by Houghton Mifflin Harcourt Publishing Company. Published by Houghton Mifflin Harcourt Publishing Company. All rights reserved.

geodynamics

(ˌdʒiːəʊdaɪˈnæmɪks)
n
(Geological Science) (functioning as singular) the branch of geology concerned with the forces and processes, esp large-scale, of the earth's interior, particularly as regards their effects on the crust or lithosphere
ˌgeodyˈnamic, ˌgeodyˈnamical adj
ˌgeodyˈnamicist n
Collins English Dictionary – Complete and Unabridged, 12th Edition 2014 © HarperCollins Publishers 1991, 1994, 1998, 2000, 2003, 2006, 2007, 2009, 2011, 2014

geodynamics

the science of the forces at work within the earth. — geodynamic, adj.
See also: Earth
-Ologies & -Isms. Copyright 2008 The Gale Group, Inc. All rights reserved.
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Seidu Mohammed said the centre was part of the space-based and geophysical tools that would help Nigeria in global geodetic and geodynamical activities and monitoring, prediction of seismic activities and mitigation mechanism.
The velocities of the Global Positioning System (GPS) stations are widely employed for numerous geodynamical studies.
Mesozoic and cenozoic volcanic rocks from central and southern Tibet: 39 Ar-40 Ar dating, petrological characteristics and geodynamical significance.
De Natale, "On the possible use of optical fiber Bragg gratings as strain sensors for geodynamical monitoring," Optics and Lasers in Engineering, vol.
Our scientists study geodynamical processes to gain insight into the structure and composition of the Earth and the redistribution of mass associated with both tidal and nontidal sources of forcing.
Even though this time window is quite wide comparatively to other periods of neotectonic activity considered for more active regions, it is appropriate for the current geodynamical setting of the Portuguese mainland, where the active faults have slow slip rates and long seismic cycles.
Following the standards of International GPS Service (IGS) aiming at precise geodynamical applications, at present, permanent GPS station VILNIUS is equipped with Ashtech GPS receiver Z-12 continuously tracking all visible GPS satellites making measurements using C/A-code, P-code and the carrier phase on both frequencies L1 and L2 and with Ashtech chock ring GPS antenna having Dorne Margolin element (Fig.