Gotowe bibliografie tematyczne / Crustal dynamics

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Gotowa bibliografia na temat „Crustal dynamics”

Autor: Grafiati

Data publikacji: 6 września 2023

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Artykuły w czasopismach na temat "Crustal dynamics"

Mead, Gilbert. "Crustal dynamics research opportunity". Eos, Transactions American Geophysical Union 66, nr 16 (1985): 172. http://dx.doi.org/10.1029/eo066i016p00172-03.

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Coates, Robert J. "The Crustal Dynamics Project". Symposium - International Astronomical Union 129 (1988): 337–38. http://dx.doi.org/10.1017/s0074180900134928.

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The Crustal Dynamics Project has been developing, deploying, and operating very-long-baseline interferometry (VLBI) systems and satellite laser ranging (SLR) systems for highly accurate geodetic measurements of global plate motion, plate stability, regional crustal deformation, and earth rotation/polar motion. Over the past 10 years, the measurement accuracies of these systems have been improved by a factor of 10 to the cm level. Plans are to continue these developments to reach mm level accuracies. The present deployment of the VLBI systems is primarily in the Northern Hemisphere. This network has produced measurements of the relative plate motion between the North American, Eurasian, and Pacific plates; the stability of the same plates; and the regional deformation at the North American/Pacific plate boundary in California and Alaska.

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Campbell, James, i Axel Nothnagel. "European VLBI for crustal dynamics". Journal of Geodynamics 30, nr 3 (luty 2000): 321–26. http://dx.doi.org/10.1016/s0264-3707(99)00068-x.

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Zhong, Shijie. "Dynamics of crustal compensation and its influences on crustal isostasy". Journal of Geophysical Research: Solid Earth 102, B7 (10.07.1997): 15287–99. http://dx.doi.org/10.1029/97jb00956.

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Fadel, Islam, Mark van der Meijde i Hanneke Paulssen. "Crustal Structure and Dynamics of Botswana". Journal of Geophysical Research: Solid Earth 123, nr 12 (grudzień 2018): 10,659–10,671. http://dx.doi.org/10.1029/2018jb016190.

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Riguzzi, Federica, i Carlo Doglioni. "Gravity and crustal dynamics in Italy". Rendiconti Lincei. Scienze Fisiche e Naturali 31, S1 (11.02.2020): 49–58. http://dx.doi.org/10.1007/s12210-020-00881-2.

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Sagert, I., O. Korobkin, I. Tews, B. J. Tsao, H. Lim, M. Falato i J. Loiseau. "Modeling Solids in Nuclear Astrophysics with Smoothed Particle Hydrodynamics". Astrophysical Journal Supplement Series 267, nr 2 (1.08.2023): 47. http://dx.doi.org/10.3847/1538-4365/acdc94.

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Abstract Smoothed particle hydrodynamics (SPH) is a frequently applied tool in computational astrophysics to solve the fluid dynamics equations governing the systems under study. For some problems, for example when involving asteroids and asteroid impacts, the additional inclusion of material strength is necessary in order to accurately describe the dynamics. In compact stars, that is white dwarfs and neutron stars, solid components are also present. Neutron stars have a solid crust, which is the strongest material known in nature. However, their dynamical evolution, when modeled via SPH or other computational fluid dynamics codes, is usually described as a purely fluid dynamics problem. Here, we present the first 3D simulations of neutron star crustal toroidal oscillations including material strength with the Los Alamos National Laboratory SPH code FleCSPH. In the first half of the paper, we present the numerical implementation of solid material modeling together with standard tests. The second half is on the simulation of crustal oscillations in the fundamental toroidal mode. Here, we dedicate a large fraction of the paper to approaches that can suppress numerical noise in the solid. If not minimized, the latter can dominate the crustal motion in the simulations.

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Björnsson, Axel. "Dynamics of crustal rifting in NE Iceland". Journal of Geophysical Research 90, B12 (1985): 10151. http://dx.doi.org/10.1029/jb090ib12p10151.

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Himwich, W. E. "NASA/Crustal Dynamics Project Geodetic Data Analysis". Symposium - International Astronomical Union 129 (1988): 357–58. http://dx.doi.org/10.1017/s0074180900134989.

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The VLBI group in NASA's Crustal Dynamics Project (CDP) maintains an integrated system for analyzing geodetic VLBI data. This system includes: CALC, calibration programs, SOLVE, GLOBL, and the Data Base System. CALC is the program which contains the models used to calculate the theoretical delay. SOLVE is used to analyze single experiments. GLOBL is used to analyze large groups of experiments. The Data Base System is a self-documenting data storage system used to pass data between programs and archive the data. Kalman filtering is being investigated for operational use in geodetic data analysis.

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Jung, S., i A. Möller. "Crustal dynamics: Links between geochronology and petrology". Chemical Geology 241, nr 1-2 (czerwiec 2007): 1–3. http://dx.doi.org/10.1016/j.chemgeo.2007.01.025.

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Rozprawy doktorskie na temat "Crustal dynamics"

Barker, Shaun, i sbarker@eos ubc ca. "Dynamics of fluid flow and fluid chemistry during crustal shortening". The Australian National University. Research School of Earth Sciences, 2007. http://thesis.anu.edu.au./public/adt-ANU20090711.074630.

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In this thesis, an integrated structural and chemical approach has been used to investigate the spatial and temporal evolution of fluid chemistry, and fluid flow pathways, during crustal shortening. The Taemas Vein Swarm is hosted in a limestone-shale sequence, the Murrumbidgee Group, in the Eastern Belt of the Lachlan Orogen, in New South Wales, Australia. The Taemas Vein Swarm (TVS) is composed of calcite ± quartz veins, hosted in a series of faults and fractures, which extends over an area of approximately 20 km2. The Murrumbidgee Group is composed of several formations, comprising massive grey micritic limestones, redbed sandstones and shales,and thinly interbedded (1020 cm scale) limestones and shales. ¶ The sedimentary sequence has been folded into a series of upright, open to close folds, and was probably deformed during either mid-late Devonian, or early Carboniferous, crustal shortening. To the east, the Murrumbidgee Group is overthrust by a Silurian volcanic sedimentary sequence along the Deakin-Warroo Fault System. Crosscutting and overprinting relationships demonstrate that vein growth was synchronous with folding, with different vein types related to different fold mechanisms at various stages of fold growth. ¶ Flexural slip folding led to the development of bedding-concordant veins (hereafter called bedding-parallel veins). Flexural flow in semicompetent to incompetent beds caused en echelon extension vein arrays to grow. Decoupling between beds, and dilatancy at fold hinges led to significant vein growth. In addition, fold lock-up led to limb-parallel stretching, and the growth of bedding-orthogonal extension fractures. ¶ Vein growth is inferred to have occurred in a compressional tectonic regime (i.e. sigma3=vertical). Oxygen isotope quartz-calcite thermometry suggests that veins formed at temperatures of 100200 oC. The depth of vein formation may have been between about 5 and 8 km. Vein textures indicate that growth of veins occurred during multiple cycles of permeability enhancement and destruction. Subhorizontal extension fractures, and faults at unfavourable angles for reactivation, imply that fluid pressures exceeded lithostatic levels during the growth of some veins. Coexisting extension and shear fractures imply that differential stress levels varied over time. ¶ Flexural slip continued throughout folding at Taemas, despite some fold limbs being at angles extremely unfavourable for reactivation ( > 60). As folds approached frictional lock-up, flexural slip continued to occur when supralithostatic fluid pressures were developed. Therefore, large, bedding-discordant faults were not developed to accommodate strain during folding, explaining a deficiency of larger faults in the TVS. ¶ Infiltration of overpressured fluids occurred into the base of the Murrumbidgee Group, and was channelled into a distributed mesh of small faults and fractures. At the point that a connected backbone flow network developed in the TVS, highpressure fluids would no longer be available to allow continuing flexural slip on fold limbs approaching lockup. Thereafter, larger faults would develop, which would adjust the fault population in the TVS to a more typical displacement-frequency distribution. This had not occurred in the Taemas area by the time crustal shortening ceased. An abundance of small faults, and fracturing driven by invasion of overpressured fluid, implies that the TVS formed via an earthquake swarm process. ¶ Modern analytical techniques, utilising laser ablation sampling technology, allow high-spatial resolution chemical data to be collected from syntectonic veins. Insights into the role that fluid-mineral interface processes may have on the chemistry of minerals grown in syntectonic veins were provided by an experimental study. Moderate sized ( < 1−5 mm) synthetic calcite crystals were successfully grown to investigate the uptake of rare earth elements (REE) into calcite. Changes in crystal morphology are linked to variable solution chemistry, which has important implications for the interpretation of hydrothermal vein textures. High-spatial resolution chemical analyses of synthetic calcite crystals demonstrate significant fluctuations in REE concentrations over distances of < 200 μm within calcite crystals. Time-equivalent regions on different crystal faces have significantly different REE concentrations, indicating that fluctuations in calcite trace element composition cannot be interpreted exclusively in terms of changing bulk fluid composition. Rare earth element anomalies (Eu/Eu* and Ce/Ce*) are not significantly influenced by compositional zoning, and may be robust indicators of changes in solution bulk chemistry and fluid oxidation state. ¶ Changes in isotopic ratios (13C, 18O and 87Sr/86Sr), and trace element concentrations in veins from the TVS are related to variations in fluid source, flow pathways and chemical conditions (e.g. trace element complexation, precipitation rate, fluid oxidation) during hydrothermal fluid flow. This integrated structural, textural and chemical approach has direct application to the examination of hydrothermal veins in fracture-hosted ore deposits, and may allow the fluid source and/or chemical conditions conducive to the formation of high-grade ore to be discerned. ¶ Vein 18O compositions systematically increase upwards through the Murrumbidgee Group, caused by progressive reaction of an externally derived, low-18O fluid (of probable meteoric origin) with host limestones. Vein 18O and 87Sr/86Sr compositions vary spatially and temporally within the same outcrop, and within individual veins, which is inferred to be caused by the ascent of packages of fluid along constantly changing flow pathways. Fluid-buffered oxygen isotope ratios at the earliest stages of deformation imply that the TVS formed via an invasion percolation process. Fluid pathways are inferred to have changed constantly, with fractures toggleswitching between high-permeability and low-permeability states, due to repeated fracture opening and sealing events.

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Musumeci, Carla. "Crustal structure and dynamics in southeastern Sicily (Italy) by using seismological data". Doctoral thesis, Università di Catania, 2013. http://hdl.handle.net/10761/1329.

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Introduction: Through receiver function analysis, this study inquires into some of the most basic properties of the crust below southeastern Sicily (Italy), mostly represented by the Hyblean Plateau. Method: This is accomplished, using P-to-S receiver function (P-RF) technique which involves coordinate rotation and deconvolution, by stacking waveforms from 335 teleseismic events, magnitude 6.0 and larger, to determine the delay in arrival time for several phases of the P-wave coda, relative to the initial P-wave arrival. This information is used to establish a linear relationship between thickness and VP/VS ratio, each of which is stacked using the slant stacking approach for a given station to identify the best-fit thickness and wave speed for the crust below that station. To determine their accuracy these results are compared with previous studies, as well as with synthetically generated receiver functions based on 1D crustal models including dipping layers. Results: The good regional coverage and the fairly dense station spacing (~20 km) leaded to a fairly complete image of the crust-mantle boundary over the entire region that shows strong lateral variations of the crustal thickness with Moho depth varying between 29 and 38 km. In particular, a thinner crust is observed in the central-eastern part of the Hyblean Foreland beneath SSY (Solarino) station and thickening further to the south beneath HMDC (Modica) station (up to 38 km) and to the north beneath HLNI (Lentini) station (up to 35 km). Sharp transitions between thinned and thickened crust are most likely the result of complicated 3D structures attributed to regional geodynamics. Discussion: Since all the 8 considered broadband stations lie in a geodinamically complex area, reliable estimates of the crustal thicknesses below these stations are key requisite for understanding the geologic and tectonic processes that have been dominant in the region, providing valuable information for the numerous earth science disciplines.

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Obana, Koichiro. "Development of Seafloor Positioning System with GPS-acoustic Link for Crustal Dynamics Observation". 京都大学 (Kyoto University), 1999. http://hdl.handle.net/2433/181958.

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Peter, Yannick Fabien. "Present-day crustal dynamics in the Adriatic-Aegean plate boundary zone inferred from continuous GPS-measurements /". Zürich, 2000. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=13700.

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Tung, Sui, i 董帥. "Co-seismic and post-seismic gravity variation associated with the 2008 M=8 Wenchuan earthquake : implication for crustal dynamics". Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2013. http://hdl.handle.net/10722/197833.

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Longmen Shan Mountain Belt is a prominent orogeny along the eastern margin of the Tibetan plateau. Its current deformation has significant implications for the Cenozoic tectonics of the Tibetan plateau. The M=8 Wenchuan earthquake substantially ruptured the Longmen Shan mountain in 2008. Numerous tectonics and rheological implications are concluded by this event on crustal dynamics along the eastern margin of the Tibetan plateau. Several high-resolution gravity surveys were conducted before and after the event to investigate the regional isostasy and crustal dynamics. From 2008 to 2011, four gravimetric surveys were carried out along two profiles across southern and northern Longmen Shan from the Sichuan Basin to the Songpan-Graze Terrane. The Bouguer gravity anomalies drop from -162 mGal to -431 mGal in the Aba Basin with a steep gradient of 0.84 mGal/km. There is a significant increase of crustal thickness from 40 km in the Sichuan to more than 60 km in the Tibetan plateau. Negative isostatic anomaly of -30 mGal over 150 km of the Songpan-Graze Terrane infers an over-compensation of excess crustal thickness up to 20 km. Hence, upward isostatic rebound is resulted and coupled with on-going crustal movement. Gravity values change significantly before and after the Wenchuan earthquake, ranging from -1.2 mGal to 0.7 mGal near the epicentral area. Significant thrust slip of 7.5m and normal slip of 4.5 m were simulated along the Beichuan fault and Wenchuan fault by an elastic dislocation theory. The co-existence of thrusting and normal faulting implies both compressional and extensional settings along Longmen Shan. The normal slip corroborates a large-scale crustal extension, lending support to a model with the inflation of lower crustal flow. The two-year post-seismic gravity variations were more than 0.1 mGal near the epicentral area. About 25% of them could be attributed to viscoelastic mantle relaxation. The dynamics topography along the eastern margin of the plateau is proposed to be a consequence of lower crustal flow squeezed by isostatic rebound and topographic load. The strong Yangtze Block is thought to obstruct the crustal flow horizontally and direct it to flow upward beneath Longmen Shan. The steep topography and seismicity along Longmen Shan are then resulted probably from the vertical stress induced in this upward flow.
published_or_final_version
Earth Sciences
Doctoral
Doctor of Philosophy

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Cartwright-Taylor, A. L. G. "Deformation-induced electric currents in marble under simulated crustal conditions : non-extensivity, superstatistical dynamics and implications for earthquake hazard". Thesis, University College London (University of London), 2015. http://discovery.ucl.ac.uk/1471386/.

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This thesis investigates electric current signals generated spontaneously in specimens of Carrara marble during deformation under crustal conditions. It extends previous work where similar currents were observed during uniaxial deformation of marble. Since marble is a non-piezoelectric material, one of the main questions is how these currents are related to the mechanical processes of deformation. Another question is whether it is possible to extract from these electric currents information about the deformation dynamics. This is particularly important in light of recent claims that geoelectric anomalies observed in the field are related to crustal deformation and can inform us about changes in the organisation of the fault network in a focal region prior to an earthquake. Using an approach that combines rock deformation experiments and statistical modelling, I examine how these electric currents evolve with deformation at the laboratory scale and make several original discoveries regarding their behaviour. To establish how the current signals varied with experimental condition and deformation mechanism across the brittle-ductile transition, I conducted constant strain rate triaxial compression experiments recording differential electric current flow through the rock samples at various confining pressures, strain rates and pore fluid conditions. I acquired mechanical data, ultrasonic velocities and acoustic emissions simultaneously, along with electric current, to constrain the relationship between electric current and deformation. For the statistical modelling, I used a novel entropy-based model, derived from non-extensive statistical mechanics (Tsallis, 1988), which has the advantage of including a term to account for interactions in the system. Interactions are effectively modelled by the non-extensive q-parameter. Small (nanoAmpere) electric currents are generated and sustained during deformation under all the conditions tested. Spontaneous electric current flow in the dry samples is seen only in the region of permanent deformation and is due to the presence of localised electric dipoles. This current flow is correlated to the damage induced by microcracking, with a contribution from other intermittent ductile mechanisms. Current and charge densities are consistent with proposed models of crack separation charging and migrating charged edge dislocations. The onset of current flow occurs only after a 10% reduction in P-wave velocity, implying that some degree of crack damage and/or crack connectivity is required before current will flow through the samples. Electric current evolution exhibits three separate time-scales of behaviour, the absolute and fluctuating components of which can be related to the evolution of stress, deformation mechanism, damage and localisation of deformation leading up to sample failure. In the brittle regime, electric current exhibits a precursory change as the stress drop accelerates towards failure, which is particularly distinct at dynamic strain rates. Current and charge production depend strongly on the experimental conditions. Power-law relationships are seen with confining pressure and strain rate, with the first corresponding to increased microcrack suppression and the second to time-dependent differences in deformation mechanism across the brittle-ductile transition. In the presence of an ionic pore fluid, electrokinetic effects dominate over solid-state mechanisms but development of the crack network and charge contribution from solid-state deformation processes drive the variation in electrokinetic parameters. Current flow in the dry samples is approximately proportional to stress within 90% of peak stress. In the fluid-saturated samples, proportionality holds from 40% peak stress, with a significant increase in the rate of current production from 90% peak stress, and is associated with fluid flow during dilatancy. This proportionality, together with the power-law relationship between current and strain rate is reminiscent of power-law creep, where deformation rate varies as a power-law function of stress, and suggests that the electric signals could be used as a proxy for stress. High frequency fluctuations in the electric current signal can be described by `fat-tailed' q-Gaussian statistics, consistent with an origin in non-extensive statistical mechanics. These distributions can be explained as arising from superstatistical dynamics (Beck, 2001; Beck and Cohen, 2003), i.e., the superposition of local mechanical relaxations in the presence of a slowly varying driving force. The macroscopic distribution parameters provide an excellent prediction of the experimentally observed mean energy dissipation rate of the system (as modelled by the superstatistical β-parameter), particularly at slow strain rates. Furthermore, characteristic q-values are obtained for different deformation regimes across the brittle-ductile transition, and the evolution of q during deformation reveals a two-stage precursory anomaly prior to sample failure, consistent with the stress intensity evolution as modelled from fracture mechanics. These findings indicate that the dynamics of rock deformation are reflected in the statistical properties of the recorded electric current. My findings support the notion that electric currents in the crust can be generated purely from deformation processes themselves. Scaling up the laboratory results to large stressed rock volumes at shallow crustal pressures and constant crustal strain rates, deformation induced transient telluric current systems may be as large as 1 MA, even accounting for >99% dissipation, which corresponds to a huge accumulated net charge of 10 ZC. This implies that a significant amount of charge from deforming tectonic regions contributes to the Earth's telluric currents and electric field, although due to conduction away from the stressed rock volume, it is unlikely that accumulated charge of this quantity would ever be measured in the field. Electric current evolution and its precursory characteristics can be related to models for electric earthquake precursors and fault-zone damage organisation, developed from field observations, providing experimental support for them. However, given the oscillatory nature of the current evolution observed during cataclastic flow processes in the laboratory, there is a high probability of false alarms. Furthermore, the potential for electric anomalies to be useful as earthquake precursors remains contentious due to the difficulties of separating deformation-induced signals from other telluric noise and the wider issue of establishing a statistically significant link with earthquakes.

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Wobbe, Florian [Verfasser], Vikram [Akademischer Betreuer] Unnithan, Karsten [Akademischer Betreuer] Gohl, Klaus [Akademischer Betreuer] Grosfeld, Carmen [Akademischer Betreuer] Gaina i Primio Rolando [Akademischer Betreuer] Di. "Crustal and lithosphere dynamics of the Southern Pacific and the West Antarctic margin / Florian Wobbe. Betreuer: Vikram Unnithan ; Karsten Gohl. Gutachter: Vikram Unnithan ; Klaus Grosfeld ; Carmen Gaina ; Rolando Di Primio". Bremen : IRC-Library, Information Resource Center der Jacobs University Bremen, 2014. http://d-nb.info/1087315581/34.

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Mazza, Sarah Elizabeth. "Thermal Structure of Mid-Crustal Shear Zones". Thesis, Virginia Tech, 2013. http://hdl.handle.net/10919/23284.

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Analysis of quartz c-axis fabrics and microstructures from ductily deformed rocks allows for the examination of the kinematics associated with crustal deformation. This thesis expands on the current knowledge of the kinematic evolution of the Himalayas and Scottish Caledonides, by examining samples from the Main Central Thrust (MCT) (Himalayas) and the Sgurr Beag Thrust (SBT) (Scottish Caledonides). Metamorphic temperatures (Tm) associated above the MCT are inverted; chapter one attempts to test if deformation temperatures (Td) correlate to Tm, indicating that ductile shearing occurred during peak Tm. In the Scottish Caledonides, Td and Tm increase from foreland to hinterland, potentially indicating a right way up thermal structure; chapter two presents Td and Tm associated with the region around the SBT. Above the MCT, quartz c-axis fabrics yield Td ranging between 500-650 "C, corresponding to the temperatures of dynamic recrystallization for subgrain rotation (SGR) and grain boundary migration (GBM). Up to 1000m above the MCT, Td and Tm are within error of each other, suggesting that shearing occurred during peak Tm; while further away from the MCT Tm is significantly hotter than Td, suggesting that shearing continued past Tm. Deformation associated with the upper part of the Moine thrust sheet and the SBT yields quartz c-axis fabrics with Td ranging between 395-583 "C, corresponding to the regional dynamic recrystallization. Tm calculations original to this study yield pressure-temperature constraints of 4.8-5.8 kbar and 586-625 "C. Tm is within error of Td, suggesting that deformation and metamorphism were synchronous.
Master of Science

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Brommer, Axel. "Strukturelle Entwicklung und Petrogenese des nördlichen Kristallingürtels der Shackleton Range, Antarktis: Proterozoische und Ross-orogene Krustendynamik am Rand des Ostantarktischen Kratons = Structural evolution and petrogenesis of the northern crystalline belt of the Shackleton Range, Antarctica: Proterozoic and Ross-orogenic crustal dynamics along the margin of the East Antarctic Craton /". Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung, 1998. http://www.gbv.de/dms/bs/toc/252821556.pdf.

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Porritt, R. W., i S. Yoshioka. "Evidence of Dynamic Crustal Deformation in Tohoku, Japan, From Time-Varying Receiver Functions". AMER GEOPHYSICAL UNION, 2017. http://hdl.handle.net/10150/626288.

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Temporal variation of crustal structure is key to our understanding of Earth processes on human timescales. Often, we expect that the most significant structural variations are caused by strong ground shaking associated with large earthquakes, and recent studies seem to confirm this. Here we test the possibility of using P receiver functions (PRF) to isolate structural variations over time. Synthetic receiver function tests indicate that structural variation could produce PRF changes on the same order of magnitude as random noise or contamination by local earthquakes. Nonetheless, we find significant variability in observed receiver functions over time at several stations located in northeastern Honshu. Immediately following the Tohoku-oki earthquake, we observe high PRF variation clustering spatially, especially in two regions near the beginning and end of the rupture plane. Due to the depth sensitivity of PRF and the timescales over which this variability is observed, we infer this effect is primarily due to fluid migration in volcanic regions and shear stress/strength reorganization. While the noise levels in PRF are high for this type of analysis, by sampling small data sets, the computational cost is lower than other methods, such as ambient noise, thereby making PRF a useful tool for estimating temporal variations in crustal structure.

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Książki na temat "Crustal dynamics"

United States. National Aeronautics and Space Administration., red. Crustal dynamics project. Washington, D.C: National Aeronautics and Space Administration, 1994.

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W, Ryan J., i Goddard Space Flight Center, red. Crustal Dynamics Project data analysis-- 1987. Greenbelt, Md: National Aeronautics and Space Administration, Goddard Space Flight Center, 1987.

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W, Ryan J., i Goddard Space Flight Center, red. Crustal Dynamics Project data analysis-- 1987. Greenbelt, Md: National Aeronautics and Space Administration, Goddard Space Flight Center, 1988.

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W, Ryan J., i United States. National Aeronautics and Space Administration. Scientific and Technical Information Branch., red. Crustal Dynamics Project data analysis--1986. [Washington, DC]: National Aeronautics and Space Administration, Scientific and Technical Information Branch, 1987.

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E, Noll Cary, i Crustal Dynamics Project (U.S.), red. Crustal Dynamics Project: Catalogue of site information. Washington, D.C: National Aeronautics and Space Administration, Scientific and Technical Information Division, 1988.

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Noll, Carey E. Crustal dynamics project: Catalogue of site information. Redaktor Goddard Space Flight Center. Greenbelt, Md: Goddard Space Flight Center, 1988.

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Crustal Dynamics Project (U.S.) i United States. National Aeronautics and Space Administration. Scientific and Technical Information Branch., red. Crustal Dynamics Project: Catalogue of site information. [Washington, DC]: National Aeronautics and Space Administration, Scientific and Technical Information Branch, 1985.

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M, Short Nicholas, i United States. National Aeronautics and Space Administration. Scientific and Technical Information Division., red. The Crustal dynamics intelligent user interface anthology. [Washington, DC]: National Aeronautics and Space Administration, Scientific and Technical Information Division, 1988.

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National Research Council (U.S.). Geophysics Study Committee., red. The Role of fluids in crustal processes. Washington, D.C: National Academy Press, 1990.

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Smith, David E., i Donald L. Turcotte, red. Contributions of Space Geodesy to Geodynamics: Crustal Dynamics. Washington, D. C.: American Geophysical Union, 1993. http://dx.doi.org/10.1029/gd023.

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Części książek na temat "Crustal dynamics"

Taron, Joshua, Steven E. Ingebritsen, Stephen Hickman i Colin F. Williams. "Dynamics of permeability evolution in stimulated geothermal reservoirs". W Crustal Permeability, 363–72. Chichester, UK: John Wiley & Sons, Ltd, 2016. http://dx.doi.org/10.1002/9781119166573.ch28.

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Coastes, J. Robert. "The Crustal Dynamics Project". W The Impact of VLBI on Astrophysics and Geophysics, 337–38. Dordrecht: Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-2949-4_116.

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Bender, Peter L. "Improved Methods for Measuring Present Crustal Movements". W Dynamics of Plate Interiors, 155–62. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gd001p0155.

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Himwich, W. E. "NASA/CRUSTAL Dynamics Project Geodetic Data Analysis". W The Impact of VLBI on Astrophysics and Geophysics, 357–58. Dordrecht: Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-2949-4_122.

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Bosworth, John M., Robert J. Coates i Thomas L. Fischetti. "The development of NASA's Crustal Dynamics Project". W Contributions of Space Geodesy to Geodynamics: Technology, 1–20. Washington, D. C.: American Geophysical Union, 1993. http://dx.doi.org/10.1029/gd025p0001.

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Artyushkov, E. V., A. E. Shlesinger i A. L. Yanshin. "The Origin of Vertical Crustal Movements within Lithospheric Plates". W Dynamics of Plate Interiors, 37–51. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gd001p0037.

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Zerbini, Susanna. "Crustal motions from short-arc analysis of LAGEOS data". W Contributions of Space Geodesy to Geodynamics: Crustal Dynamics, 371–87. Washington, D. C.: American Geophysical Union, 1993. http://dx.doi.org/10.1029/gd023p0371.

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Campbell, J., H. Hase, A. Nothnagel, H. Schuh, N. Zarraroa, A. Rius, E. Sardon, V. Tornatore i P. Tomasi. "First results of European crustal motion measurements with VLBI". W Contributions of Space Geodesy to Geodynamics: Crustal Dynamics, 397–405. Washington, D. C.: American Geophysical Union, 1993. http://dx.doi.org/10.1029/gd023p0397.

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Smith, David E., i Miriam Baltuck. "Introduction". W Contributions of Space Geodesy to Geodynamics: Crustal Dynamics, 1–4. Washington, D. C.: American Geophysical Union, 1993. http://dx.doi.org/10.1029/gd023p0001.

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Stein, Seth. "Space geodesy and plate motions". W Contributions of Space Geodesy to Geodynamics: Crustal Dynamics, 5–20. Washington, D. C.: American Geophysical Union, 1993. http://dx.doi.org/10.1029/gd023p0005.

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Streszczenia konferencji na temat "Crustal dynamics"

Royden, L. "Some Aspects of Crustal Deformation and Subduction Zone Dynamics within the Mediterranean Region." W 64th EAGE Conference & Exhibition. European Association of Geoscientists & Engineers, 2002. http://dx.doi.org/10.3997/2214-4609.201405739.

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Esin, Nikolay, Nikolay Esin, Nikolay Esin, Nikolay Esin, Olga Sorokina i Olga Sorokina. "VERTICAL MOVEMENTS OF THE COAST AND SHELF OF THE BLACK AND MEDITERRANEAN SEAS DURING THE HOLOCENE". W Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b9376952568.74055827.

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Vertical movement of Earth crust can modify the shape of the eustatic sea level curves. A method allows calculation of the eustatic sea level course using the known local curves. We were able to divide a number of local curves of the Mediterranean Sea to the eustatic and tectonic components. The data about dynamics of the vertical crustal movements in 27 points of the Mediterranean coast and shelf during the Holocene were obtained. It was found that the velocities of raising and dipping are unstable over time and can reach value of 10 mm/year. Satellite measurements have recorded the velocities of vertical movements in the range of -10 to +20 mm/year for some parts of Black Sea coast. Such movements of the Earth's crust undoubtedly have a large impact on coastal processes and should be considered in designing coastal structures.

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Whyte, Colin, Karl E. Karlstrom, Laura J. Crossey, David A. Gonzales i Thomas H. Darrah. "EVALUATING MANTLE-CRUSTAL GAS DYNAMICS OF SOUTHWESTERN US CO2 SPRINGS USING HELIUM ISOTOPES AND HEAVY NOBLE GASES". W GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-287315.

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Veiga, Robert E. "SAGE II Measurements of Volcanic Aerosols". W Optical Remote Sensing of the Atmosphere. Washington, D.C.: Optica Publishing Group, 1993. http://dx.doi.org/10.1364/orsa.1993.the.17.

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Volcanic injections of gaseous and crustal constituents directly into the stratosphere occur with low frequency. The mineralogical aerosols quickly settle out while the gases, primarily SO2, are converted into aerosols. Once in the stratosphere, the optical properties and the global dispersion of volcanic aerosols can be inferred using in situ particle samplers, photometers, lidars, and satellite instruments. Satellite remote sensing offers the opportunity to study atmospheric dynamics over the short term using the aerosols as a quasi-conserved tracer.

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Weil, Arlo Brandon, i Adolph Yonkee. "DEFORMATION PATTERNS ACROSS THE LARAMIDE AND SIERRA PAMPEANAS THICK-SKINNED FORELAND SYSTEMS; RELATIONS TO PLATE DYNAMICS, LITHOSPHERIC STRESS TRANSMISSION, AND CRUSTAL ARCHITECTURE". W GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-316407.

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Santi, M., A. L. Muller i J. P. Ibanez. "Kinematic and Dynamic Modeling for Rift Formation in Crustal Extensional Mechanisms". W 79th EAGE Conference and Exhibition 2017. Netherlands: EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201701174.

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Fan, T. H., i F. B. Cheung. "Modeling of Transient Turbulent Natural Convection in a Melt Layer With Solidification". W ASME 1996 International Mechanical Engineering Congress and Exposition. American Society of Mechanical Engineers, 1996. http://dx.doi.org/10.1115/imece1996-0087.

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Abstract The phenomenon of turbulent natural convection in a horizontal heat-generating melt layer with solidification taking place at the cooled upper and lower boundaries is investigated theoretically. The objective is to determine the transient behavior of the crust at the upper and lower surfaces and the effect of crust formation on the turbulent natural convection process in the melt layer. Various surface temperatures, latent heats, and the heat source strengths are considered along with the effects of the Stefan number and Rayleigh number. Special attention is given to the interaction between the melt pool heat transfer and the crust dynamics. Numerical results are presented for the transient crust thickness, transient temperature distribution, eddy heat transport, and the heat transfer characteristics at the solid-liquid interface during the freezing process. The present study provides basic information needed to predict the transient behavior of a melt pool in a reactor lower head following a severe core-meltdown accident.

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Horowitz, Charles. "Molecular Dynamics Simulations of the Crust of Accreting Neutron Stars". W 10th Symposium on Nuclei in the Cosmos. Trieste, Italy: Sissa Medialab, 2009. http://dx.doi.org/10.22323/1.053.0061.

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LINK, B. "THE DYNAMICS OF VORTEX PINNING IN THE NEUTRON STAR CRUST". W Proceedings of the International Symposium EXOCT07. WORLD SCIENTIFIC, 2008. http://dx.doi.org/10.1142/9789812797049_0064.

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Raporty organizacyjne na temat "Crustal dynamics"

Pitarka, Arben. Rupture Dynamics Simulations for Shallow Crustal Earthquakes. Office of Scientific and Technical Information (OSTI), luty 2019. http://dx.doi.org/10.2172/1499970.

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Pitarka, A. Rupture Dynamics Simulations of Shallow Crustal Earthquakes on Reverse Slip Faults. Office of Scientific and Technical Information (OSTI), luty 2020. http://dx.doi.org/10.2172/1599564.

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Bastien, R. Current status of data acquisition and management in the crustal dynamics section. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/315220.

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Rassat, Scot D., Charles W. Stewart, Beric E. Wells, William L. Kuhn, Zenen I. Antoniak, Judith M. Cuta, Kurtis P. Recknagle i in. Dynamics of Crust Dissolution and Gas Release in Tank 241-SY-101. Office of Scientific and Technical Information (OSTI), styczeń 2000. http://dx.doi.org/10.2172/965217.

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SD Rassat, CW Stewart, BE Wells, WL Kuhn, ZI Antoniak, JM Cuta, KP Recknagle i in. Dynamics of Crust Dissolution and Gas Release in Tank 241-SY-101. Office of Scientific and Technical Information (OSTI), styczeń 2000. http://dx.doi.org/10.2172/750394.

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Pitarka, A. Dynamic Rupture Modeling of the 1999 Chi-Chi, Taiwan Earthquake Using 3DFinite Element Method. Sensitivity Analysis of Slip Rate Function to ModelParameters of Crustal Weak-Zone. Office of Scientific and Technical Information (OSTI), luty 2022. http://dx.doi.org/10.2172/1845214.

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Kuster, K., C. M. Lesher i M. G. Houlé. Geology and geochemistry of mafic and ultramafic bodies in the Shebandowan mine area, Wawa-Abitibi terrane: implications for Ni-Cu-(PGE) and Cr-(PGE) mineralization, Ontario and Quebec. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329394.

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The Shebandowan Ni-Cu-(PGE) deposit occurs in the Shebandowan greenstone belt in the Wawa-Abitibi terrane. This deposit is one of a few economic Ni-Cu-(PGE) deposits in the Superior Province and one of a very few deposits worldwide that contains both Ni-Cu-(PGE) and Cr-(PGE) mineralization. The mafic-ultramafic successions in the area comprise abundant flows and sills of tholeiitic basalt and lesser Al-undepleted komatiite (MgO &gt;18 wt%, Al2O3/TiO2 = 15-25), the latter indicating separation from mantle sources at shallow levels. Siliceous high-Mg basalts (MgO 8-12 wt%, SiO2 &gt; 53 wt%, TiO2 &lt; 1.2 wt%, La/Sm[MN] &lt; 1-2) are relatively abundant in the area and likely represent crustally contaminated komatiites. Ultramafic bodies in the Shebandowan mine area comprise at least three or four komatiitic sills (A-B, C, D) and at least two komatiitic flows (E, F), all of which are altered to serpentinites or talc-carbonate schists with relict igneous chromite and rare relict igneous orthopyroxene-clinopyroxene. Unit A-B contains pentlandite-pyrrhotite-chalcopyrite-pyrite-magnetite mineralization, occurring as massive sulfides, sulfide breccias, or stringers, and subeconomic chromite mineralization in contorted massive bands varying from a few millimetres up to 10 metres thick. The localization of massive and semi-massive Ni-Cu-(PGE) ores along the margins of Unit A and the paucity of disseminated and net-textured ores suggest tectonic mobilization. Chromite is typically zoned with Cr-Mg-Al-rich (chromite) cores and Fe-rich (ferrichromite/magnetite) rims due to alteration and/or metamorphism, but rarely contains amoeboid magnetite cores. The thickness of chromite in Unit B is too great to have crystallized in cotectic proportion from the komatiitic magma and a model involving dynamic upgrading of magnetite xenoliths derived from interflow oxide facies iron formations is being tested.

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