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Статті в журналах з теми "Evolution of seismicity"
Ma, Xu, Erik Westman, Dave Counter, Farid Malek, and Brent Slaker. "Passive Seismic Imaging of Stress Evolution with Mining-Induced Seismicity at Hard-Rock Deep Mines." Rock Mechanics and Rock Engineering 53, no. 6 (March 16, 2020): 2789–804. http://dx.doi.org/10.1007/s00603-020-02076-5.
Повний текст джерелаAochi, Hideo, Julie Maury, and Thomas Le Guenan. "How Do Statistical Parameters of Induced Seismicity Correlate with Fluid Injection? Case of Oklahoma." Seismological Research Letters 92, no. 4 (April 28, 2021): 2573–90. http://dx.doi.org/10.1785/0220200386.
Повний текст джерелаBadawy, A., S. M. Abdel-Monem, K. Sakr, and Sh M. Ali. "Seismicity and kinematic evolution of middle Egypt." Journal of Geodynamics 42, no. 1-3 (August 2006): 28–37. http://dx.doi.org/10.1016/j.jog.2006.04.003.
Повний текст джерелаNasir, Asma, Esther Hintersberger, and Kurt Decker. "The temporal evolution of seismicity and variability of b-values along the Vienna Basin Transfer Fault System." Austrian Journal of Earth Sciences 116, no. 1 (January 1, 2023): 1–15. http://dx.doi.org/10.17738/ajes.2023.0001.
Повний текст джерелаVallianatos, Filippos, Georgios Michas, and George Hloupis. "Seismicity Patterns Prior to the Thessaly (Mw6.3) Strong Earthquake on 3 March 2021 in Terms of Multiresolution Wavelets and Natural Time Analysis." Geosciences 11, no. 9 (September 9, 2021): 379. http://dx.doi.org/10.3390/geosciences11090379.
Повний текст джерелаMignan, A. "Static behaviour of induced seismicity." Nonlinear Processes in Geophysics Discussions 2, no. 6 (December 10, 2015): 1659–74. http://dx.doi.org/10.5194/npgd-2-1659-2015.
Повний текст джерелаDenlinger, Roger P., and Daniel R. H. O’Connell. "Evolution of Faulting Induced by Deep Fluid Injection, Paradox Valley, Colorado." Bulletin of the Seismological Society of America 110, no. 5 (August 18, 2020): 2308–27. http://dx.doi.org/10.1785/0120190328.
Повний текст джерелаLipovsky, Bradley Paul, Colin R. Meyer, Lucas K. Zoet, Christine McCarthy, Dougal D. Hansen, Alan W. Rempel, and Florent Gimbert. "Glacier sliding, seismicity and sediment entrainment." Annals of Glaciology 60, no. 79 (June 3, 2019): 182–92. http://dx.doi.org/10.1017/aog.2019.24.
Повний текст джерелаFan, Gang, Jun Wang, Shunchao Qi, Gongda Lu, Xingguo Yang, and Jiawen Zhou. "Spatiotemporal Evolution of Earthquakes in Longmenshan Fault and Adjacent Area, before and after the 2008 Wenchuan Earthquake." Shock and Vibration 2021 (November 24, 2021): 1–13. http://dx.doi.org/10.1155/2021/9400276.
Повний текст джерелаJia, Ke, Shiyong Zhou, Jiancang Zhuang, Changsheng Jiang, Yicun Guo, Zhaohui Gao, Shesheng Gao, Yosihiko Ogata, and Xiaodong Song. "Nonstationary Background Seismicity Rate and Evolution of Stress Changes in the Changning Salt Mining and Shale-Gas Hydraulic Fracturing Region, Sichuan Basin, China." Seismological Research Letters 91, no. 4 (May 20, 2020): 2170–81. http://dx.doi.org/10.1785/0220200092.
Повний текст джерелаДисертації з теми "Evolution of seismicity"
Firoozfar, Alireza. "Caspian Sea level changes, seismicity assessment and beach evolution." Thesis, Kingston University, 2012. http://eprints.kingston.ac.uk/23704/.
Повний текст джерелаHenderson, Jeremy. "Fracture mechanics and the evolution of seismicity in an intra-plate setting." Thesis, University of Edinburgh, 1992. http://hdl.handle.net/1842/14047.
Повний текст джерелаSchoenball, Martin [Verfasser], and T. [Akademischer Betreuer] Kohl. "Evolution of Stress and Seismicity in Fractured Geothermal Reservoirs / Martin Schoenball. Betreuer: T. Kohl." Karlsruhe : KIT-Bibliothek, 2014. http://d-nb.info/1051848261/34.
Повний текст джерелаBiryol, Berk Cemal. "Neotectonics And Evolution Of The Eskipazar Basin, Karabuk." Master's thesis, METU, 2004. http://etd.lib.metu.edu.tr/upload/12605211/index.pdf.
Повний текст джерела#8764
2.6 My). Common basin margin-bounding faults of the Eskipazar Basin are the Kadilar fault set, the Beytarla Fault Zone, the Budaklar fault set, the Arslanlar fault set, the Dibek fault, the Karkin fault, the Boztepe fault and the Acisu fault. These faults display well preserved fault scarps, in places. Morphological expressions of these faults and their geometrical relationships to regional stress system indicate that these faults are mostlystrike-slip faults with normal component. However the Kadilar fault set displays a different characteristic, being the major fault controlling the basin to the west and it is indeed an oblique slip normal fault. Long term seismicity and their epicentral distribution in and very close to the study area suggest that the Eskipazar basin is located in an area of seismic quiescence, nevertheless the morphotectonic expressions of the faults exposing in the basin suggest that these faults are active. Since the most of settlements are located on different lithologies of poorly consolidated deposits of the Eskipazar formation susceptible to landslides, the area is open to future earthquake hazard. Therefore, structures and settlements have to be constructed on strong ground away from active faults.
Minetto, Riccardo. "Essaims sismiques : comparaison des séismes naturels et induits." Electronic Thesis or Diss., Université Grenoble Alpes, 2023. http://www.theses.fr/2023GRALU009.
Повний текст джерелаA seismic sequence is a cluster of earthquakes that occur in close spatial and temporal proximity. One type of seismic sequence is a seismic swarm, which is typically characterized by earthquakes whose location changes over time and by the absence of a single, dominant, large earthquake.In this thesis, I investigate the spatio-temporal evolution of natural and induced seismic swarms with the aim of identifying the physical processes that drive them and characterizing the properties of the activated fault systems. More specifically, I focus on three key aspects of the seismic activity: temporal evolution of the seismicity rate, earthquake location and frequency-magnitude distribution. The study focuses on two seismic swarms. The first one, of natural origin, occurred in the Maurienne valley (French Alps) between 2017 and 2019, while the second one was induced by hydraulic fracturing operations at Preston New Road, UK, in 2019. To ensure a high-resolution analysis of these sequences, I first created improved catalogs, which incorporate newly detected events and more accurate magnitudes and hypocenter locations.The migration of earthquakes during the Maurienne swarm suggests that this sequence may have been triggered by a combination of multiple pulses of high-pressure fluids and earthquake-to-earthquake interactions. Additionally, the proportion of small and large events (i.e., the b-value of the Gutenberg-Richter law) varies in space, and this change may be linked to the size of the active fault systems.In addition to the study of the seismic activity, I applied ambient noise interferometry to assess if stress changes during the Maurienne swarm produced detectable variations in seismic wave velocity. The velocity changes appear to be primarily influenced by a seasonal process possibly related to pore pressure variations due to rainfall. However, during the main period of seismic activity, such changes may also be accentuated by the continuous ground shaking resulting from the prolonged occurrence of earthquakes.The Preston New Road sequence is characterized by a seismicity rate and a frequency-magnitude distribution that gradually evolve as fluids are repeatedly injected and the seismogenic volume expands in size. This suggests that the seismic activity during an injection stage depends on the injection history of past stages.The Maurienne and Preston New Road sequences are just two examples of the broader phenomenon of seismic and induced swarms. Nonetheless, these two sequences illustrate that induced and natural swarms can exhibit similar patterns in their spatio-temporal evolution, such as earthquake migration and the dependence of the b-value on the scale of the fault system. This emphasizes the potential of applying the knowledge gained from studying one type of swarm to improve our understanding of the other
Caracausi, Antonio. "Noble gases as geochemical tracers of Earth's dynamic and evolution." Electronic Thesis or Diss., Université de Lorraine, 2019. http://www.theses.fr/2019LORR0339.
Повний текст джерелаIn my project, I used the nobles gases (He, Ne, Ar, Kr and Xe) to investigate natural processes occurring in different geodynamical contexts (i.e., subduction, continental collision, rifting), showing how the use of the noble gases is fundamental to constrain the origin of volatiles, and to investigate the Earth interior. Furthermore, I also used these volatiles to recognize the processes (water-gas-rock interaction) that occur during the fluids up rise from the Earth’s interior to the atmosphere and quantitatively constrain the extents of these processes. The results of my project are summarized in five main topics: 1) Insights into the degassing history of Earth’s mantle from high precision noble gas analysis of magmatic gas 2) Noble Gas and Carbon Isotope Systematics at the Seemingly Inactive Ciomadul Volcano (Romania): Evidence for Volcanic Degassing 3) Mantle‐Derived Fluids in the East Java Sedimentary Basin, Indonesia 4) Outgassing of Mantle Volatiles in Compressional Tectonic Regime Away From Volcanism: The Role of Continental Delamination 5) Continental degassing of helium in an active tectonic setting (northern Italy): the role of seismicity
Almakari, Michelle. "Réactivation Hydro-Mécanique d’une Faille Rate & State ˸ Glissement, Sismicité et Évolution de Perméabilité." Electronic Thesis or Diss., Paris Sciences et Lettres (ComUE), 2019. http://www.theses.fr/2019PSLEM065.
Повний текст джерелаThis PhD thesis is dedicated to the study of injection induced fault reactivation using a coupled hydro-mechanical rate and state modelof a fault. Even though the principal mechanisms behind induced fault reactivation are well known, different aspects are not yet fully explored, nor understood. In the first part of this thesis, we explore successively the role of the injection protocol (in particular, injection maximum pressure and injection pressure rate), and the fault frictional parameters on the rate of induced events and their magnitude content, for different heterogeneous 2-D fault configurations. We first point out a temporal correlation between the seismicity rate and the pore pressure rate governing the fault. We then show a dependence of the rate and magnitude content of the seismic events on the injection parameters, as well as the existence of an important trade-off between them, which could not be addressed using the Dietrich(1994)’s seismicity rate model. Concerning the frictional parameters, we show that for the faults tested in this study, the ones having a more stable frictional behavior exhibit a lower induced seismicity rate and seismic moment released. In the last part of this study, the variation of the hydraulic diffusivity during fluid injection with shear slip and effective stress reduction is addressed. For this, we use laboratory injection experiments on an Andesite rock sample, during which the pore pressure was measured at two locations along the fault plane. In an inversion framework, we estimate the best model and the associated uncertainties of an effective diffusivity history that could explain the experimental data. Using this information, we could extend our hydro-mechanical model, which would allow the computation of pore pressure, diffusivity and slip changes along the experimental fault
shyh-yang, Sheu, and 許世陽. "Spatio-Temporal Evolution of Displacements, Stresses and Seismicity Patterns in Earthquake Process." Thesis, 2004. http://ndltd.ncl.edu.tw/handle/82250187313028371479.
Повний текст джерела國立中正大學
地震研究所
92
The rheology of the Earth’s lithosphere is one of the important factors in causing time dependent deformation and stress variations following the large earthquake. For the analysis of tectonics beneath Taiwan, there is evidence to suggest that the lower crust underneath Taiwan display a ductile behavior. If so, then the ductile behavior of the lower crust must be involved in studies of postseismic deformations, transfer of stress and earthquake triggering. So far, this situation was never explored in this area. Consideration of models with viscous flow in the lower crust will help improve the understanding of information about the mechanics of controlling the time-dependent process and will be needed in order to accurately decipher this problem. The crust around the rupture zone of the 1999 Chi-Chi earthquake has tangible broad-scale postseismic deformations with a short relaxation time. In this work, we first study the mechanism of crustal early (97 days and 15 months after quake) postseismic deformation due to dip-slip earthquake. Taking into account the fault slip model, we calculate postseismic surface displacements caused by Chi-Chi earthquake in the central Taiwan using a three-dimensional finite element method for different assumed multi-layered Earth’s models. In order to determine the mechanism for early postseismic deformation and the evolution of stress for 2-year period following the earthquake the comparison of GPS data and theoretical calculations allows us to establish reasonable regional Earth’s model and rheological parameters of lower crust and upper mantle. Concerning the comparison of model result with real field observations, including spatial distribution of GPS surface measurements and aftershocks response to time dependent stress field, we could provide a more realistic rheological Earth’s model and explain phenomena previously not understood. Moreover, pattern dynamics will be applied to detect a non-local seismicity pattern prior to large-size earthquakes in Taiwan. We attempt to evaluate seismicity pattern of the future earthquake in Taiwan employing the catalogue for 1973-2000. Based on the exploration of the possible mechanism containing both the viscoelastic response model and the afterslip model in the early postseismic deformation of 1999 Chi-Chi quake, we compare theoretical surface displacements for each of the two models that we evaluate. The results reveal that there is little double, that while neither of these models alone are able to predict the GPS measurements well in a 97-day period, the combination of the two models improve the predictions considerably. We conclude that the afterslip mainly dominated Chi-Chi postseismic deformation in the rupture area, while the viscoelastic model did so elsewhere. Further consideration of tectonic loading in conjuction with postseismic deformation within the central Taiwan suggests that this effect may be negligible after 97 days, but it is significant for the long-term effect that we examined with 15-month GPS data. Combined with a Coulomb failure criterion we seek to validate our calculations of the static coseismic stress changes and time-dependent postseismic stress changes by comparing them to the observed seismicity rate changes associated with the Chi-Chi earthquake. In these calculations, we have considered the effect of a regional compressional stress field whose maximum principal axis is horizontal and oriented N119°E. The results show that static coseismic stress changes explain the apparent triggering of aftershocks by mainshock, especially those that occurred in the upper crust after the first several Maxwell times of the mainshock. The relaxation of the stress in the lower part of the crust can transfer stress up to the upper crust with a roughly steady rate. This means that the viscoelastic relaxation may be responsible for the triggering of aftershocks in the upper part (10 km) of crust in the long term. Finally, we investigate the non-local seismicity patterns in Taiwan by pattern dynamics. Most of the larger-size earthquakes occurred in areas of probability increase, yielding evidence for space-time patterns of seismic activity which reflect the existence of correlations in underlying stress or strain field.
Chan, Chung-Han, and 詹忠翰. "Stress Evolution Associate with Seismicity during Coseismic and Postseismic Periods of the 1999 Chi-Chi, Taiwan, Earthquake." Thesis, 2006. http://ndltd.ncl.edu.tw/handle/6433u2.
Повний текст джерела國立中央大學
地球物理研究所
94
In the past decade, many studies had proved the influences of static stress changes on spatial or temporal distribution of the aftershocks and further large earthquakes. By contrast, other studies have deepened the argument by resolving stress changes on aftershock focal mechanisms, which removes the assumption that the aftershocks are optimally oriented for failure. The 21st September 1999 Chi-Chi, Taiwan, earthquake (Mw=7.6) produced a remarkable set of data and clearly exhibits stress transfer. Large amount of GPS static measurements and strong motion acceleration records recorded this event. Such a data set offers a unique opportunity to understand the earthquake process and the generation of ground motions. Furthermore, 7 of continuous monitoring GPS stations were set up near the Chelungpu fault, mostly within three weeks after the occurrence of Chi-Chi mainshock and about 80 campaign-surveyed stations were resurveyed up to 7 times from September 1999 to December 2000. We explore how Coulomb stress transfer might control aftershock distribution, long-term seismicity, and postseismic slip in a ramp-flat thrust fault system. The Mw=7.6 Chi-Chi shock, with a surface-cutting 30°-dipping ramp fault merging into a near-horizontal d?collement, is representative of continental thrust systems throughout the world, and so inferences drawn from this uniquely well-recorded event may be widely applicable elsewhere. The 3D distribution of aftershocks and their focal mechanisms are consistent with the calculated spatial distribution of Coulomb stress changes. Here one compares the percentage of planes on which failure is promoted after the main shock relative to the percentage beforehand. For Chi-Chi we find a 28% increase for thrust and an 18% increase for strike-slip mechanisms, commensurate with increases reported for other large main shocks. However, perhaps the chief criticism of static stress triggering is the difficulty in observing predicted seismicity rate decreases in the stress shadows, or sites of Coulomb stress decrease. Detection of sustained drops in seismicity rate demands a long catalog with a low magnitude of completeness and a high seismicity rate, conditions that are met at Chi-Chi. We find four lobes with statistically significant seismicity rate declines of 40–90% for 50 months, and they coincide with the stress shadows calculated for strikeslip faults, the dominant faulting mechanism. The rate drops are evident in uniform cell calculations, 100-month time series, and by visual inspection of the M≧3 seismicity. An additional reason why detection of such declines has proven so rare emerges from this study: there is a widespread increase in seismicity rate during the first 3 months after Chi-Chi, and perhaps many other main shocks, that might be associated with a different mechanism. And nearly all the M≧6 aftershocks are found to be promoted by several bars as a result of the mainshock. We further consider whether the stresses imparted by the coseismic slip could have triggered postseismic slip on the fault. We find a fair correlation between the inferred postseismic slip and regions of calculated stress increase on the ramp and d?collement. The correlation of stress with slip is best if the fault friction is very high (μ?=0.8) along the uppermost 5 km of the ramp, and if friction is exceedingly low (μ?=0.0) along the d?collement. Finally, we search for a change in aftershock distribution and rate caused by the postseismic d?collement slip. We find a marked decrease in aftershocks with respect to Omori decay where the postseismic slip is calculated to further depress the Coulomb stress, and an increase of seismicity and the rate of M ≧ 5.0 earthquakes in the corresponding positively stressed zones. The GPS observations suggest significant slip on the hanging wall of the Chelungpu fault, while little surface deformation is observed on the footwall. Repeated precise leveling survey across central Taiwan also shows significant uplift on the hanging wall of the Chelungpu faults during Aug. 2002 to Mar. 2004. we consider both of the afterslip and viscoelastic rebound behaviors during postseismic period to compare with geodesy data. They show good correlation between GPS observation on the hanging wall with the calculation deformation based on afterslip. On the footwall, by contrast, the calculation deformation based on viscoelastic rebound seems fit the observation better. We also estimate the stress evolution along the faults near the Chelungpu fault. During coseismic period, the shear stress along Changhua fault seems promoted by mainshock, while the normal stress is dropped. For the Shiaomao and Hsuilikeng faults, the normal stress is promoted, while the shear stress is dropped. During 15 mo. after Chi-Chi, the shear stress is dropped at shallow part of the Changhua fault, while it is enhanced at deep part. It also shows the normal stress along all of the faults is promoted them to failure. 50 years after Chi-Chi, the shear stress at deeper part of the Changhua, Shiaomao and most part of Hsuilikeng is promoted to failure. For the normal stress, except at shallow part of the Changhua fault, it shows stress dropped at rest of the faults.
Книги з теми "Evolution of seismicity"
Boschi, E., E. Mantovani, and A. Morelli, eds. Recent Evolution and Seismicity of the Mediterranean Region. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-2016-6.
Повний текст джерелаNATO Advanced Research Workshop on Recent Evolution and Seismicity of the Mediterranean Region (1992 Erice, Italy). Recent evolution and seismicity of the Mediterranean region. Dordrecht: Kluwer Academic, 1993.
Знайти повний текст джерелаUnited States. National Aeronautics and Space Administration., ed. Lithospheric structure, seismicity, and contemporary deformation of the United States Cordillera. [Washington, DC: National Aeronautics and Space Administration, 1985.
Знайти повний текст джерелаUnited States. National Aeronautics and Space Administration, ed. Lithospheric structure, seismicity, and contemporary deformation of the United States Cordillera. [Washington, DC: National Aeronautics and Space Administration, 1985.
Знайти повний текст джерелаMantovani, E., E. Boschi, and A. Morelli. Recent Evolution and Seismicity of the Mediterranean Region. Springer, 2012.
Знайти повний текст джерелаBoschi, E. Recent Evolution and Seismicity of the Mediterranean Region. Ingramcontent, 2013.
Знайти повний текст джерелаSorkhabi, Rasoul. Tectonic Evolution, Collision, and Seismicity of Southwest AsiaIn Honor of Manuel Berberian’s Forty-Five Years of Research Contributions. Geological Society of America, 2017. http://dx.doi.org/10.1130/spe525.
Повний текст джерелаЧастини книг з теми "Evolution of seismicity"
Udías, Agustín. "Seismicity of the Mediterranean Basin." In Geological Evolution of the Mediterranean Basin, 55–63. New York, NY: Springer New York, 1985. http://dx.doi.org/10.1007/978-1-4613-8572-1_3.
Повний текст джерелаRiznichenko, Yurii Vladimirovich. "A Model of Space-Time Evolution of Seismicity." In Problems of Seismology, 120–46. Berlin, Heidelberg: Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-662-09446-4_4.
Повний текст джерелаYamashita, Teruo, and Akito Tsutsumi. "Effects of Fluid Migration on the Evolution of Seismicity." In Involvement of Fluids in Earthquake Ruptures, 153–84. Tokyo: Springer Japan, 2017. http://dx.doi.org/10.1007/978-4-431-56562-8_6.
Повний текст джерелаŞengör, A. M. C. "Some Current Problems on the Tectonic Evolution of the Mediterranean During the Cainozoic." In Recent Evolution and Seismicity of the Mediterranean Region, 1–51. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-2016-6_1.
Повний текст джерелаGiardini, D., B. Palombo, and E. Boschi. "The Determination of Earthquake Size and Source Geometry in the Mediterranean Sea." In Recent Evolution and Seismicity of the Mediterranean Region, 213–38. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-2016-6_10.
Повний текст джерелаPapadopoulos, G. A. "Tectonic and Seismic Processes of Various Space and Time Scales in the Greek Area." In Recent Evolution and Seismicity of the Mediterranean Region, 239–49. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-2016-6_11.
Повний текст джерелаSlejko, D. "A Review of the Eastern Alps — Northern Dinarides Seismotectonics." In Recent Evolution and Seismicity of the Mediterranean Region, 251–60. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-2016-6_12.
Повний текст джерелаUdias, A., and E. Buforn. "Regional Stresses in the Mediterranean Region Derived from Focal Mechanisms of Earthquakes." In Recent Evolution and Seismicity of the Mediterranean Region, 261–68. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-2016-6_13.
Повний текст джерелаDrakopoulos, J., and G. N. Stavrakakis. "Source Process of Some Large Earthquakes in Greece and its Tectonic Implication." In Recent Evolution and Seismicity of the Mediterranean Region, 269–94. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-2016-6_14.
Повний текст джерелаCocco, M., G. Selvaggi, M. Bona, and A. Basili. "Recent Seismic Activity and Earthquake Occurrence Along the Apennines." In Recent Evolution and Seismicity of the Mediterranean Region, 295–312. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-2016-6_15.
Повний текст джерелаТези доповідей конференцій з теми "Evolution of seismicity"
Dineva, Savka, and Mirjana Boskovic. "Evolution of seismicity at Kiruna Mine." In Eighth International Conference on Deep and High Stress Mining. Australian Centre for Geomechanics, Perth, 2017. http://dx.doi.org/10.36487/acg_rep/1704_07_dineva.
Повний текст джерелаHui, Gang, Shengnan Chen, and Fei Gu. "A Novel Coupled Approach to Investigate the Spatiotemporal Evolution of Fracturing-Induced Seismicity: Case Study." In SPE Hydraulic Fracturing Technology Conference and Exhibition. SPE, 2021. http://dx.doi.org/10.2118/204156-ms.
Повний текст джерелаThin, Iain, Nicole Edkins, L. Jeschke, and Adrian Winchester. "The Evolution of Seismicity and Subsequent Learning Experiences in Deep Lead, Mount Isa Mines, Xstrata Zinc." In Sixth International Symposium on Rockburst and Seismicity in Mines. Australian Centre for Geomechanics, Perth, 2005. http://dx.doi.org/10.36487/acg_repo/574_2.
Повний текст джерелаRuiz Barajas, Sandra, Guillermo E. Alvarado, Belén Benito Oterino, and Álvaro Climent. "ANÁLISIS DE SISMICIDAD ASOCIADA AL LLENADO DE EMBALSES. CASO DEL CENTRO DE PRODUCCIÓN DE PIRRÍS (COSTA RICA)." In 1st Congress in Geomatics Engineering. Valencia: Universitat Politècnica València, 2017. http://dx.doi.org/10.4995/cigeo2017.2017.6666.
Повний текст джерелаZhao, Xiaoxi, and Birendra Jha. "Role of Inelasticity in Production-Induced Subsidence and Fault Reactivation in the Groningen Field." In SPE Reservoir Simulation Conference. SPE, 2023. http://dx.doi.org/10.2118/212234-ms.
Повний текст джерелаYe, Zhi, and Ahmad Ghassemi. "Investigation of Micro-Seismicity and Permeability Evolution in Shale Fractures During Stimulation." In Unconventional Resources Technology Conference. Tulsa, OK, USA: American Association of Petroleum Geologists, 2019. http://dx.doi.org/10.15530/urtec-2019-342.
Повний текст джерелаVarden, Richard, and Hendrik Esterhuizen. "Kanowna Belle ‒ evolution of seismicity with increasing depth in an ageing mine." In Sixth International Seminar on Deep and High Stress Mining. Australian Centre for Geomechanics, Perth, 2012. http://dx.doi.org/10.36487/acg_rep/1201_15_varden.
Повний текст джерелаBerentsen, Cas, and C. Hans de Pater. "Seismicity Induced by Cooling of CCS Reservoirs." In SPE EuropEC - Europe Energy Conference featured at the 83rd EAGE Annual Conference & Exhibition. SPE, 2022. http://dx.doi.org/10.2118/209685-ms.
Повний текст джерелаNaderloo, M., A. Veltmeijer, A. Pluymakers, and A. Barnhoorn. "Experimental Investigation of the Effect of Stress Cycling on Seismicity Evolution During Fault Reactivation Process." In 83rd EAGE Annual Conference & Exhibition. European Association of Geoscientists & Engineers, 2022. http://dx.doi.org/10.3997/2214-4609.202210415.
Повний текст джерелаGiroud, Sébastien, Yama Tomonaga, Matthias Brennwald, and Rolf Kipfer. "Monitoring dissolved gases in thermal water to assess the potential relation between fluid evolution and seismicity." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.8935.
Повний текст джерелаЗвіти організацій з теми "Evolution of seismicity"
Elsworth, Derek, Ghazal Izadi, Quan Gan, Yi Fang, Josh Taron, and Eric Sonnenthal. THMC Modeling of EGS Reservoirs -- Continuum through Discontinuum Representations. Capturing Reservoir Stimulation, Evolution and Induced Seismicity. Office of Scientific and Technical Information (OSTI), July 2015. http://dx.doi.org/10.2172/1202233.
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Повний текст джерелаWozniakowska, P., D. W. Eaton, C. Deblonde, A. Mort, and O. H. Ardakani. Identification of regional structural corridors in the Montney play using trend surface analysis combined with geophysical imaging, British Columbia and Alberta. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328850.
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