Academic literature on the topic 'Induced seismicity'
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Journal articles on the topic "Induced seismicity"
Keranen, Katie M., and Matthew Weingarten. "Induced Seismicity." Annual Review of Earth and Planetary Sciences 46, no. 1 (May 30, 2018): 149–74. http://dx.doi.org/10.1146/annurev-earth-082517-010054.
Full textRoeloffs, Evelyn. "Induced seismicity." Tectonophysics 275, no. 4 (July 1997): 353–54. http://dx.doi.org/10.1016/s0040-1951(96)00281-8.
Full textKirály-Proag, Eszter, J. Douglas Zechar, Valentin Gischig, Stefan Wiemer, Dimitrios Karvounis, and Joseph Doetsch. "Validating induced seismicity forecast models-Induced Seismicity Test Bench." Journal of Geophysical Research: Solid Earth 121, no. 8 (August 2016): 6009–29. http://dx.doi.org/10.1002/2016jb013236.
Full textElsworth, Derek, Christopher J. Spiers, and Andre R. Niemeijer. "Understanding induced seismicity." Science 354, no. 6318 (December 15, 2016): 1380–81. http://dx.doi.org/10.1126/science.aal2584.
Full textYoon, Jeoung Seok, Günter Zimmermann, Arno Zang, and Ove Stephansson. "Discrete element modeling of fluid injection–induced seismicity and activation of nearby fault." Canadian Geotechnical Journal 52, no. 10 (October 2015): 1457–65. http://dx.doi.org/10.1139/cgj-2014-0435.
Full textLiu, Su Mei, and Xiang Dong Xie. "Reservoir-Induced Seismicity in the Three Gorges Reservoir Area." Applied Mechanics and Materials 501-504 (January 2014): 1477–85. http://dx.doi.org/10.4028/www.scientific.net/amm.501-504.1477.
Full textMcCann, D. M. "Induced seismicity in engineering." Geological Society, London, Engineering Geology Special Publications 5, no. 1 (1988): 397–404. http://dx.doi.org/10.1144/gsl.eng.1988.005.01.44.
Full textZhai, Guang, Manoochehr Shirzaei, and Michael Manga. "Widespread deep seismicity in the Delaware Basin, Texas, is mainly driven by shallow wastewater injection." Proceedings of the National Academy of Sciences 118, no. 20 (May 10, 2021): e2102338118. http://dx.doi.org/10.1073/pnas.2102338118.
Full textMignan, 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.
Full textRoberts, Jennifer J., Clare E. Bond, and Zoe K. Shipton. "Fracking bad language – hydraulic fracturing and earthquake risks." Geoscience Communication 4, no. 2 (June 11, 2021): 303–27. http://dx.doi.org/10.5194/gc-4-303-2021.
Full textDissertations / Theses on the topic "Induced seismicity"
Larsson, Kristina. "Mining induced seismicity in Sweden." Licentiate thesis, Luleå, 2004. http://epubl.luth.se/1402-1757/2004/80.
Full textLi, Junlun Ph D. Massachusetts Institute of Technology. "Study of induced seismicity for reservoir characterization." Thesis, Massachusetts Institute of Technology, 2013. http://hdl.handle.net/1721.1/84917.
Full textCataloged from PDF version of thesis.
Includes bibliographical references.
The main goal of the thesis is to characterize the attributes of conventional and unconventional reservoirs through passive seismicity. The dissertation is comprised of the development and applications of three new methods, each of which focuses on a different aspect of fractures/faults and the resulting seismicity. In general, the thesis work discusses reservoir characterization from two aspects: 1) understanding fractures and faults in reservoirs as seismic sources with induced seismicity, and then inferring other properties of the reservoirs, such as stress regime and velocity structure (Chapters 2, 3, 4); 2) understanding the fractures in reservoirs as seismic scatterers (Chapter 5). First, I introduce a new method to determine the source mechanisms of the induced earthquakes by incorporating high frequency waveform matching, first P-arrival polarities and average S/P amplitude ratios. The method is applied to 40 induced earthquakes from an oil/gas field in Oman monitored by a sparse near-surface seismic network and a deep borehole seismic network. The majority of the events have a strike direction parallel with the major NE-SW faults in the region, and some events trend parallel with the NW-SE conjugate faults. The results are consistent with the in-situ well breakout measurements and the current knowledge of the stress direction of this region. The source mechanisms of the studied events together with the hypocenter distribution indicate that the microearthquakes are caused by the reactivation of preexisting faults. Then I introduce a new method to locate microseismic events induced by hydraulic fracturing with simultaneous anisotropic velocity inversion using differential arrival times and differential back azimuths. We derive analytical sensitivities for the elastic moduli (Cij) and layer thickness L for the anisotropic velocity inversion. The method is then applied to a microseismic dataset monitoring a Middle Bakken completion in the Beaver Lodge area of North Dakota. Our results show: 1) moderate-to-strong anisotropy exists in all studied sedimentary layers, especially in both the Upper Bakken and Lower Bakken shale formations, where the Thomsen parameters (E and y) can be over 40%; 2) all events selected for high signal-to-noise ratio and used for the joint velocity inversion are located in the Bakken and overlying Lodgepole formations, i.e., no strong events are located in the Three Forks formation below the Bakken; 3) more than half of the strong events are in two clusters at about 100 and 150 meters above the Middle Bakken. Re-occurrence of strong, closely clustered events suggests activation of natural fractures or faults in the Lodgepole formation. Finally, I introduce a new hybrid method to model the shear (SH) wave scattering from arbitrarily shaped fractures embedded in a heterogeneous medium by coupling the boundary element method (BEM) and the finite difference method (FDM) in the frequency domain. The hybrid method can calculate scattering from arbitrarily shaped fractures very rapidly, thus Monte Carlo simulations for characterizing the statistics of fracture attributes can be performed efficiently. The advantages of the hybrid method are demonstrated by modeling waves scattered from tilted fractures embedded in complex media. Interesting behaviors of the scattered waves, such as frequency shift with the scattering order and coherent pattern of scattered waves through strong heterogeneities, are observed. This method can be used to analyze and interpret the scattered coda waves in the microseismic observations, e.g., the reverberating multiples in the Bakken microseismic data which cannot be explained by the determined layered anisotropic velocity model alone.
by Junlun Li.
Ph.D.
Holmgren, Joanna. "Induced Seismicity in the Dannemora Mine, Sweden." Thesis, Uppsala universitet, Geofysik, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-267361.
Full textBredenkamp, Ben. "Analysis and modelling of mining induced seismicity." Thesis, Stellenbosch : University of Stellenbosch, 2006. http://hdl.handle.net/10019.1/2257.
Full textEarthquakes and other seismic events are known to have catastrophic effects on people and property. These large-scale events are almost always preceded by smallerscale seismic events called precursors, such as tremors or other vibrations. The use of precursor data to predict the realization of seismic hazards has been a long-standing technical problem in different disciplines. For example, blasting or other mining activities have the potential to induce the collapse of rock surfaces, or the occurrence of other dangerous seismic events in large volumes of rock. In this study, seismic data (T4) obtained from a mining concern in South Africa were considered using a nonlinear time series approach. In particular, the method of surrogate analysis was used to characterize the deterministic structure in the data, prior to fitting a predictive model. The seismic data set (T4) is a set of seismic events for a small volume of rock in a mine observed over a period of 12 days. The surrogate data were generated to have structure similar to that of T4 according to some basic seismic laws. In particular, the surrogate data sets were generated to have the same autocorrelation structure and amplitude distributions of the underlying data set T4. The surrogate data derived from T4 allow for the assessment of some basic hypotheses regarding both types of data sets. The structure in both types of data (i.e. the relationship between the past behavior and the future realization of components) was investigated by means of three test statistics, each of which provided partial information on the structure in the data. The first is the average mutual information between the reconstructed past and futures states of T4. The second is a correlation dimension estimate, Dc which gives an indication of the deterministic structure (predictability) of the reconstructed states of T4. The final statistic is the correlation coefficients which gives an indication of the predictability of the future behavior of T4 based on the past states of T4. The past states of T4 was reconstructed by reducing the dimension of a delay coordinate embedding of the components of T4. The map from past states to future realization of T4 values was estimated using Long Short-Term Recurrent Memory (LSTM) neural networks. The application of LSTM Recurrent Neural Networks on point processes has not been reported before in literature. Comparison of the stochastic surrogate data with the measured structure in the T4 data set showed that the structure in T4 differed significantly from that of the surrogate data sets. However, the relationship between the past states and the future realization of components for both T4 and surrogate data did not appear to be deterministic. The application of LSTM in the modeling of T4 shows that the approach could model point processes at least as well or even better than previously reported applications on time series data.
Boonzaaier, Leandro. "Self-organised criticality and seismicity." Thesis, Stellenbosch : Stellenbosch University, 2002. http://hdl.handle.net/10019.1/53047.
Full textENGLISH ABSTRACT: In this thesis we give an overview of self-organised criticality and its application to studying seismicity. We recall some of the basic models and techniques for studying self-organised critical systems. We discuss one of these, the sandpile model, in detail and show how various properties of the model can be calculated using a matrix formulation thereof. A correspondence between self-organised critical systems and seismicity is then proposed. Finally, we consider the timeevolution of the sandpile model by using a time-to-failure analysis, originally developed in the study of seismicity and obtain results for the sandpile model that show similarities with that of the analyses of seismic data.
AFRIKAANSE OPSOMMING: In hierdie tesis gee ons 'n oorsig van self-organiserende kritikaliteit en die toepassing daarvan in die studie van seismisiteit. Ons beskryf die basiese modelle en tegnieke vir die studie van self-organiserende kritiese sisteme. Ons bespreek een van hierdie, die sandhoopmodel, in besonderheid en wys hoe om verskeie eienskappe van die model te bereken deur gebruik te maak van 'n matriks-formulering daarvan. Ons stel dan 'n korrespondensie tussen self-organiserende kritiese sisteme en seismisiteit voor. Ter afsluiting ondersoek ons die tydontwikkeling van die sand hoopmodel deur gebruik te maak van 'n deurbreektyd analise wat oorspronklik in die bestudering seismiese data ontwikkel is. Die resultate vir die analise van die sandhoopmodel toon ooreenkomste met dit wat verkry word vir seismiese data.
Hooper, Heather J. (Heather Julie) 1975. "Analysis and modeling of induced seismicity in petroleum reservoirs." Thesis, Massachusetts Institute of Technology, 2002. http://hdl.handle.net/1721.1/54445.
Full textIncludes bibliographical references (p. 53).
Since 1998, a producing oil field in Oman has been experiencing microearthquake activity. The aim of this project is to compare numerical models of wave propagation using simple source representations to a small subset of these microearthquakes, with three goals in mind: 1) to understand whether the microearthquakes are generated by movement along a known fault system in the field, or by some other mechanism; 2) if the source is fault related, to better understand what kind of movement is occurring on the fault; and 3) to see if this simple modeling method provides useful results, and forms a basis for future work. Synthetic waveforms are generated using a one-dimensional, discrete wavenumber numerical model (Bouchon, 1980) with two simple source representations: an explosive point source and a vertical force. Comparison of the synthetic waveforms to the microearthquake data indicates that the vertical force results in a better match than the explosive point source. In addition, a simple model consisting of the superposition of four vertical forces (representing vertical fault rupture), results in waveforms that are very similar to the recorded events. These results suggest that the source of the microearthquakes is motion along a near-vertical normal fault system that has been mapped in the field. These results are also consistent with work by Sze and Toksoz (2001) in which relocation of the same events imaged a near-vertical normal fault in the field. Further work using fault rupture source modeling may provide additional insight into the amount of fault motion that is occurring in relation to these events.
by Heather J. Hooper.
S.M.in Geosystems
Kondas, Sean Michael. "Crustal unloading as a source of induced seismicity in Plainfield, Connecticut:." Thesis, Boston College, 2020. http://hdl.handle.net/2345/bc-ir:109092.
Full textThesis advisor: Mark D. Behn
On January 12, 2015, a magnitude 3.1 mainshock occurred in Plainfield, Connecticut near Wauregan Tilcon Quarry, causing modified Mercalli II-IV intensities. Shortly after the event, a team from Weston Observatory installed portable seismographs in the epicentral area. The portable array detected hundreds of small earthquakes from around the quarry, with 26 events that were accurately located. P-wave first motion directions obtained from readings of the mainshock suggest a thrusting focal mechanism on a NNE-SSW trending fault. In this research, we collected 113 gravity measurements in the proximity of the quarry to verify and correct local fault geometry proposed by historic aeromagnetic and geologic mapping. Interpretations of the computed simple Bouguer anomaly are consistent with historic mapping, with a few exceptions. The gravity survey constrains a NNE-SSW trending fault that dips west underneath the quarry, inferred to be the Lake Char-Honey Hill Fault, and reduces ambiguity in the position of an undefined ESE-WNW trending fault, which appears to be on strike to intersect the quarry. A 3D boundary element program (3D~Def) is used to simulate quarry-induced stress changes on these faults in order to analyze the possibility of inducing seismicity through crustal unloading in the region. Quarry operations resulted in the removal of mass from the crust, which decreased lithostatic load. In a setting confined by a maximum horizontal compressional stress, decreasing the lithostatic load, orminimum principal stress (σ3), shifts a Mohr-Coulomb diagram toward failure. The boundary element model shows that following the excavation of materials at the quarry, positive Coulomb failure stress changes occur on the west dipping Lake Char-Honey Hill Fault. In agreement with past studies, our results suggest that quarrying operations can trigger seismic activity in specific settings with stress regime, fault orientations, and rock characteristics such as those that exist in the northeastern U.S. In order to mitigate the risk for future earthquakes related to quarrying operations, these factors must be considered before operations begin
Thesis (MS) — Boston College, 2020
Submitted to: Boston College. Graduate School of Arts and Sciences
Discipline: Earth and Environmental Sciences
Al-busaidi, Ahmed. "Distinct element modelling of hydraulically-induced fracture and associated seismicity." Thesis, University of Liverpool, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.406824.
Full textMartínez-Garzón, Patricia [Verfasser]. "Seismo-mechanical reservoir characterization from fluid-induced seismicity / Patricia Martínez-Garzón." Berlin : Freie Universität Berlin, 2014. http://d-nb.info/1056908165/34.
Full textSarkar, Sudipta. "Reservoir monitoring using induced seismicity at a petroleum field in Oman." Thesis, Massachusetts Institute of Technology, 2008. http://hdl.handle.net/1721.1/45765.
Full textIncludes bibliographical references.
This thesis presents methods of analysis and results from a petroleum reservoir monitoring application using induced seismicity data. The dissertation work is comprised of four major studies, each focusing on a different aspect of induced seismicity. First, methods and issues in location of induced seismicity are discussed, and strategies are proposed for determining accurate hypocenters of induced events. The importance of velocity model and how it impacts the depth determination of reservoir-induced events are demonstrated with real field data. A location method that is better-suited than other existing methods for this application is proposed. The accuracy and efficiency of this proposed location method is demonstrated with field data application.Secondly, event locations and interpretations are presented for about 1300 induced events recorded by a near-surface network over a seven year period at a petroleum field in Oman. The event hypocenters delineate two major northeast-southwest striking faults in the field, which are consistent with fault maps derived from reflection seismic interpretations. Spatiotemporal analysis of induced event locations reveals ongoing large scale fault reactivation in the field, and also suggests compaction of the gas reservoir as the major cause and water injection in the oil reservoir as the secondary cause for inducing seismicity in the field.Thirdly, event locations and interpretations are presented for a different set of induced seismicity data recorded by a deep-borehole network over an 11-month period at the same field. About 5400 events are located and analyzed, and detailed mapping of faults and fractures using the event hypocenters are presented.
(cont.) Patterns of seismicity also reveal faults and fracture systems previously unmapped by reflection seismic. While this dataset allows for much finer interpretation, the results between the two network data are found to be consistent and comparable.Finally, the double-difference relocation and tomography method is applied for event relocation and imaging of the reservoir. Better correlation of relocated events with faults is observed from application of this method to the surface-network events, and detailed velocity and structure images for the reservoir are obtained from application of tomography with the deep network events.
by Sudipta Sarkar.
Ph.D.
Books on the topic "Induced seismicity"
Gupta, Harsh K., and Rajender K. Chadha, eds. Induced Seismicity. Basel: Birkhäuser Basel, 1995. http://dx.doi.org/10.1007/978-3-0348-9238-4.
Full textArthur, McGarr, and Workshop on Induced Seismicity (1992 : Santa Fe, N.M.), eds. Induced seismicity. Basel: Birkhäuser Verlag, 1993.
Find full text1942-, Gupta Harsh K., and Chadha Rajender K. 1955-, eds. Induced seismicity. Basel: Birkhauser, 1995.
Find full textTrifu, Cezar I., ed. The Mechanism of Induced Seismicity. Basel: Birkhäuser Basel, 2002. http://dx.doi.org/10.1007/978-3-0348-8179-1.
Full textPeter, Knoll, and Kowalle Georg, eds. Induced seismic events. Basel: Birkhäuser, 1996.
Find full textRen, Jinwei. Cluster analysis of induced seismicity data. Dublin: University College Dublin, 1996.
Find full textOppenheimer, D. Seismicity near the Warm Springs Dam, Lake Sonoma, recorded by the Northern California Seismic Network. [Menlo Park, CA]: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.
Find full textBook chapters on the topic "Induced seismicity"
Gupta, Harsh K., and R. K. Chadha. "Introduction." In Induced Seismicity, 1–2. Basel: Birkhäuser Basel, 1995. http://dx.doi.org/10.1007/978-3-0348-9238-4_1.
Full textShen, Li-Ying, and Bao-Qi Chang. "Application of Stress-pore Pressure Coupling Theory for Porous Media to the Xinfengjiang Reservoir Earthquakes." In Induced Seismicity, 123–37. Basel: Birkhäuser Basel, 1995. http://dx.doi.org/10.1007/978-3-0348-9238-4_10.
Full textPanfilov, V. S., and G. A. Sobolev. "Unstable Steam-water Convection as Possible Trigger to Earthquakes." In Induced Seismicity, 139–47. Basel: Birkhäuser Basel, 1995. http://dx.doi.org/10.1007/978-3-0348-9238-4_11.
Full textFeng, Deyi, Xuejun Yu, and Jinqping Gu. "Assessment of Potential Strength of an Induced Earthquake by Using Fuzzy Multifactorial Evaluation." In Induced Seismicity, 149–53. Basel: Birkhäuser Basel, 1995. http://dx.doi.org/10.1007/978-3-0348-9238-4_12.
Full textChadha, R. K. "Role of Dykes in Induced Seismicity at Bhatsa Reservoir, Maharashtra, India." In Induced Seismicity, 155–65. Basel: Birkhäuser Basel, 1995. http://dx.doi.org/10.1007/978-3-0348-9238-4_13.
Full textTalwani, Pradeep. "Speculation on the Causes of Continuing Seismicity Near Koyna Reservoir, India." In Induced Seismicity, 167–74. Basel: Birkhäuser Basel, 1995. http://dx.doi.org/10.1007/978-3-0348-9238-4_14.
Full textRaval, U. "Seismicity of the Koyna Region and Regional Tectonomagmatism of the Western Margin (India)." In Induced Seismicity, 175–92. Basel: Birkhäuser Basel, 1995. http://dx.doi.org/10.1007/978-3-0348-9238-4_15.
Full textAwad, Mohamed, and Megume Mizoue. "Tomographic Inversion for the Three-dimensional Seismic Velocity Structure of the Aswan Region, Egypt." In Induced Seismicity, 193–207. Basel: Birkhäuser Basel, 1995. http://dx.doi.org/10.1007/978-3-0348-9238-4_16.
Full textSrivastava, H. N., S. N. Bhattacharya, K. C. Sinha Ray, S. M. Mahmoud, and S. Yunga. "Reservoir Associated Characteristics Using Deterministic Chaos in Aswan, Nurek and Koyna Reservoirs." In Induced Seismicity, 209–17. Basel: Birkhäuser Basel, 1995. http://dx.doi.org/10.1007/978-3-0348-9238-4_17.
Full textTrifu, Cezar-Ioan, Theodore I. Urbancic, and R. Paul Young. "Source Parameters of Mining-induced Seismic Events: An Evaluation of Homogeneous and Inhomogeneous Faulting Models for Assessing Damage Potential." In Induced Seismicity, 3–27. Basel: Birkhäuser Basel, 1995. http://dx.doi.org/10.1007/978-3-0348-9238-4_2.
Full textConference papers on the topic "Induced seismicity"
Spetzler, J. "Induced Seismicity in Groningen." In 79th EAGE Conference and Exhibition 2017. Netherlands: EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201700959.
Full textD. Goldbach, O. "Flooding-induced Seismicity in Mines." In 11th SAGA Biennial Technical Meeting and Exhibition. European Association of Geoscientists & Engineers, 2009. http://dx.doi.org/10.3997/2214-4609-pdb.241.goldbach_paper1.
Full textAbd, Najah, Hanan Mahdi, Haydar Al-Shukri, Aycan Catakli, Hussein Chlaib, and Mert Su. "Induced Seismicity of Central Arkansas." In Istanbul 2012 - International Geophysical Conference and Oil & Gas Exhibition. Society of Exploration Geophysicists and The Chamber of Geophysical Engineers of Turkey, 2012. http://dx.doi.org/10.1190/ist092012-001.139.
Full textDuncan, Peter M. "Induced Seismicity: Monitoring to Mitigation." In SEG Technical Program Expanded Abstracts 2012. Society of Exploration Geophysicists, 2012. http://dx.doi.org/10.1190/segam2012-0843.1.
Full textWalker, Robert L., and Fred Aminzadeh. "Dynamic Considerations for Induced Seismicity." In SPE Western Regional Meeting. Society of Petroleum Engineers, 2016. http://dx.doi.org/10.2118/180365-ms.
Full textSinha, Saurabh, Yunjie Wen, Rafael Pires De Lima, and Kurt Marfurt. "Statistical Controls on Induced Seismicity." In Unconventional Resources Technology Conference. Tulsa, OK, USA: American Association of Petroleum Geologists, 2018. http://dx.doi.org/10.15530/urtec-2018-2897507.
Full textRucci, A. R., A. F. Ferretti, and A. T. Tamburini. "InSAR for Induced Seismicity Monitoring." In 77th EAGE Conference and Exhibition - Workshops. Netherlands: EAGE Publications BV, 2015. http://dx.doi.org/10.3997/2214-4609.201413525.
Full textViegas, G., T. I. Urbancic, A. M. Baig, and E. von Lunen. "Rupture Behaviour of Induced Seismicity." In Sixth EAGE Workshop on Passive Seismic. Netherlands: EAGE Publications BV, 2016. http://dx.doi.org/10.3997/2214-4609.201600021.
Full textSundberg, Sarah A., Xiaowei Chen, Jake Walter, and Yan Qin. "HYDRAULIC FRACTURING INDUCED SEISMICITY IN OKLAHOMA." In Joint 53rd Annual South-Central/53rd North-Central/71st Rocky Mtn GSA Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019sc-327572.
Full textBuchanan, Rex C. "PUBLIC RESPONSE TO MIDCONTINENT INDUCED SEISMICITY." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-333061.
Full textReports on the topic "Induced seismicity"
Hasegawa, H. S. Mining induced seismicity. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/122734.
Full textSegall, P. Induced seismicity. Final report. Office of Scientific and Technical Information (OSTI), September 1997. http://dx.doi.org/10.2172/578467.
Full textChoens, Robert Charles, Anastasia Gennadyevna Ilgen, Carlos F. Jove-Colon, Jennifer Wilson, and Moo Y. Lee. ChemoMechanical Controls on Induced Seismicity. Office of Scientific and Technical Information (OSTI), September 2018. http://dx.doi.org/10.2172/1474256.
Full textDrummond, Barry. Review of Hydrofracturing and Induced Seismicity. Geoscience Australia, 2016. http://dx.doi.org/10.11636/record.2016.002.
Full textKao, H. Induced seismicity research project: an update. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2018. http://dx.doi.org/10.4095/308294.
Full textKao, H. Induced seismicity associated with shale gas development. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/299734.
Full textKao, H. Induced seismicity research project: accomplishments and looking forward. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/305005.
Full textGhassemi, Ahmad. Geomechanics-Based Stochastic Analysis of Injection- Induced Seismicity. Office of Scientific and Technical Information (OSTI), August 2017. http://dx.doi.org/10.2172/1375732.
Full textMatzel, Eric M. Real-time Microseismic Processing for Induced Seismicity Hazard Detection. Office of Scientific and Technical Information (OSTI), October 2016. http://dx.doi.org/10.2172/1332471.
Full textWoodbridge, Diane, and Randolph Brost. Geospatial-Temporal Semantic Graph Evaluation for Induced Seismicity Analysis. Office of Scientific and Technical Information (OSTI), September 2016. http://dx.doi.org/10.2172/1562818.
Full text