@article {alattar2008,
author = {Al-Attar, David and Woodhouse, John H.},
title = {Calculation of seismic displacement fields in self-gravitating earth models—applications of minors vectors and symplectic structure},
journal = {Geophysical Journal International},
volume = {175},
number = {3},
publisher = {Blackwell Publishing Ltd},
issn = {1365-246X},
url = {http://dx.doi.org/10.1111/j.1365-246X.2008.03961.x},
doi = {10.1111/j.1365-246X.2008.03961.x},
pages = {1176--1208},
keywords = {Numerical solutions, Surface waves and free oscillations, Theoretical seismology},
year = {2008},
}
@article{ammon2005,
author = {Ammon, Charles J. and Ji, Chen and Thio, Hong-Kie and Robinson, David and Ni, Sidao and Hjorleifsdottir, Vala and Kanamori, Hiroo and Lay, Thorne and Das, Shamita and Helmberger, Don and Ichinose, Gene and Polet, Jascha and Wald, David},
title = {Rupture Process of the 2004 Sumatra-Andaman Earthquake},
volume = {308},
number = {5725},
pages = {1133-1139},
year = {2005},
doi = {10.1126/science.1112260},
abstract ={The 26 December 2004 Sumatra-Andaman earthquake initiated slowly, with small slip and a slow rupture speed for the first 40 to 60 seconds. Then the rupture expanded at a speed of about 2.5 kilometers per second toward the north northwest, extending 1200 to 1300 kilometers along the Andaman trough. Peak displacements reached ?15 meters along a 600-kilometer segment of the plate boundary offshore of northwestern Sumatra and the southern Nicobar islands. Slip was less in the northern 400 to 500 kilometers of the aftershock zone, and at least some slip in that region may have occurred on a time scale beyond the seismic band.},
URL = {http://www.sciencemag.org/content/308/5725/1133.abstract},
eprint = {http://www.sciencemag.org/content/308/5725/1133.full.pdf},
journal = {Science}
}
#1
@article{becker2002,
author = {Becker, T. W. and Boschi, L.},
title = {A comparison of tomographic and geodynamic mantle models},
journal = {Geochemistry Geophysics Geosystems},
volume = {3},
abstract = {We conduct a comprehensive and quantitative analysis of similarities and differences between recent seismic tomography models of the Earth's mantle in an attempt to determine a benchmark for geodynamic interpretation. After a spherical harmonic expansion, we find the spectral power and radial correlation of each tomographic model as a function of depth and harmonic degree. We then cal{{GPS}}culate the correlation, at the same depths and degrees, between all possible pairs of models, to identify stable and model-dependent features ( the former being usually of longer spatial wavelength than the latter). We can therefore evaluate the degree of robust structure that seismologists have mapped so far and proceed to calculate ad hoc mean reference models. Tomographic models are furthermore compared with two geodynamic subduction models that are based on plate motion reconstructions. We find systematically low intermediate-wavelength correlation between tomography and convective reconstruction models and suggest that the inadequate treatment of the details of slab advection is responsible. However, we confirm the presence of stable, slab-like fast anomalies in the mid-mantle whose geographic pattern naturally associates them with subduction. This finding, in addition to our analysis of heterogeneity spectra and the absence of strong minima in the radial correlation functions besides the one at similar to 700 km, supports the idea of whole mantle convection with slab penetration through the 660 km phase transition, possibly accompanied by a reorganization of flow.},
ISSN = {1525-2027},
DOI = {1003
10.1029/2001gc000168},
url = {<Go to ISI>://WOS:000173170800001 },
year = {2002},
type = {Journal Article}
}
@article{avallone2011,
year=2011,
author={Avallone, A. and Marzario, M. and Cirella, A. and Piatanesi, A. and Rovelli, A. and Di Alessandro, C. and D'Anastasio, E. and D'Agostino, N. and Giuliani, R. and Mattone, M.},
title={{Very high rate (10 Hz) GPS seismology for moderate-magnitude earthquakes: The case of the M-w 6.3 L'Aquila (central Italy) event}},
doi={10.1029/2010JB007834},
journal={J. Geophys. Res.},
number={B02305},
volume=116,
}
@article{bassin2000,
author = {Bassin, C. and Laske, G. and Masters, G.},
title = {The Current Limits of Resolution for Surface Wave Tomography in North America},
journal = {Eos Trans. AGU,},
volume = {81},
number = {F897},
year = {2000},
type = {Journal Article}
}
@article {chao2005,
author = {Chao, B. F. and Gross, R. S.},
title = {Did the 26 December 2004 Sumatra, Indonesia, Earthquake disrupt the Earth's rotation as the mass media have said?},
journal = {Eos, Transactions American Geophysical Union},
volume = {86},
number = {1},
issn = {2324-9250},
url = {http://dx.doi.org/10.1029/2005EO010003},
doi = {10.1029/2005EO010003},
pages = {1--2},
year = {2005},
}
@article{psimoulis2014,
year=2014,
title={{Long-period surface motion of the multipatch M(w)9.0 Tohoku-Oki}},
author={Psimoulis, P. and Houli\'e, N. and Michel, C. and Meindl, M. and Rothacher, M.},
journal={Geophysical Journal International},
doi={10.1093/gji/ggu302},
volume=199,
number=2,
}
@article{psimoulis2015,
author={Psimoulis, P., Houli\'e, N., Meindl, M. and Rothacher, M.},
year= 2015,
title={{Consistency of GPS and strong-motion records: case study of Mw9.0 Tohoku-Oki 2011
earthquake}},
journal={Smart Struct. Syst.},
volume={26},
}
#2
@article{blewitt2008,
author = {Blewitt, G.},
title = {Fixed point theorems of {{GPS}} carrier phase ambiguity resolution and their application to massive network processing: Ambizap},
journal = {Journal of Geophysical Research},
volume = {113},
number = {B12},
ISSN = {0148-0227},
DOI = {10.1029/2008jb005736},
year = {2008},
type = {Journal Article}
}
#3
@article{blewitt2008b,
author = {Blewitt, G. and Hammond, W. and Kreemer, C. and Plag, H. P. and Stein, S. and Okal, E.},
title = {{GPS} for real-time earthquake source determination and tsunami warning systems},
journal = {Journal of Geodesy},
volume = {83},
number = {3},
abstract = {We identify the key design aspects of a {GPS}-based system (and in the future, GNSS-based systems) that could contribute to real-time earthquake source determination and tsunami warning systems. Our approach is based on models of both transient and permanent displacement of {GPS} stations caused by large earthquakes, while considering the effect of {GPS} errors on inverted earthquake source parameters. Our main conclusions are that (1) the spatial pattern, magnitude, and timing of permanent displacement of {GPS} stations can be inverted for the earthquake source and so predict the 3D displacement field of the ocean bottom, thus providing the initial conditions for tsunami models, and (2) there are no inherently limiting factors arising from real-time orbit and positioning errors, provided sufficient near-field {GPS} stations are deployed. This signal could be readily exploited by {GPS} networks currently in place, and will be facilitated by the IGS Real-Time Project as it comes to fruition.},
ISSN = {0949-7714},
DOI = {10.1007/s00190-008-0262-5},
url = {<Go to ISI>://INSPEC:10912471 },
year = {2008},
type = {Journal Article}
}
#4
@article{bock2011,
author = {Bock, Y. and Melgar, D. and Crowell, B. W.},
title = {Real-Time Strong-Motion Broadband Displacements from Collocated {GPS} and Accelerometers},
journal = {Bulletin of the Seismological Society of America},
volume = {101},
number = {6},
pages = {2904-2925},
ISSN = {0037-1106},
DOI = {10.1785/0120110007},
year = {2011},
type = {Journal Article}
}
#5
@article{bock2004,
author = {Bock, Y. and Prawirodirdjo, L. and Melbourne, T. I.},
title = {Detection of arbitrarily large dynamic ground motions with a dense high-rate {GPS} network},
journal = {Geophysical Research Letters},
volume = {31},
number = {6},
abstract = {[1] We describe the detection of teleseismic surface waves from the 3 November 2002 Mw 7.9 Denali fault earthquake in Alaska with a dense network of {1 Hz} {GPS} stations in southern California, about 3900 km from the event. Relative horizontal displacements with amplitudes in excess of 15 mm and duration of 700 seconds agree with integrated velocities recorded by nearby broadband seismometers with an rms difference of 2-3 mm. The displacements are derived from independent {1 Hz} instantaneous positions demonstrating that a {GPS} network can provide direct measurements of arbitrarily large dynamic and static ground horizontal displacements at periods longer than 1 s and amplitudes above 2 mm, with an inherent precision (signal to noise) that improves indefinitely with amplitude without clipping and in real time. High-rate, real-time {GPS} networks can enhance earthquake detection and seismic risk mitigation and support other applications such as intelligent transportation and civil infrastructure monitoring.},
ISSN = {0094-8276},
DOI = {L06604
10.1029/2003gl019150},
url = {<Go to ISI>://WOS:000220436600005 },
year = {2004},
type = {Journal Article}
}
#6
@article{bufe2006,
author = {Bufe, C. G.},
title = {Coulomb stress transfer and tectonic loading preceding the 2002 Denali fault earthquake},
journal = {Bulletin of the Seismological Society of America},
volume = {96},
number = {5},
pages = {1662-1674},
abstract = {Pre-2002 tectonic loading and Coulomb stress transfer are modeled along the rupture zone of the M 7.9 Denali fault earthquake (DFE) and on adjacent segments of the right-lateral Denali-Totschunda fault system in central Alaska, using a three-dimensional boundary-element program. The segments modeled closely follow, for about 95 degrees, the arc of a circle of radius 375 km centered on an inferred asperity near the northeastern end of the intersection of the Patton Bay fault with the Alaskan megathrust under Prince William Sound. The loading model includes slip of 6 mm/yr below 12 km along the fault system, consistent with rotation of the Wrangell block about the asperity at a rate of about 1 degrees/m.y. as well as slip of the Pacific plate at 5 cm/yr at depth along the Fairweather-Queen Charlotte transform fault system and on the Alaska megathrust. The model is consistent with most available pre-2002 Global Positioning System ({GPS}) displacement rate data. Coulomb stresses induced on the Denali-Totschunda fault system (locked above 12 km) by slip at depth and by transfer from the M 9.2 Prince William Sound earthquake of 1964 dominated the changing Coulomb stress distribution along the fault. The combination of loading (similar to 70-85$\%$) and coseismic stress transfer from the great 1964 earthquake (similar to 15-30$\%$) were the principal post-1900 stress factors building toward strike-slip failure of the northern Denali and Totschunda segments in the M 7.9 earthquake of November 2002. Postseismic stresses transferred from the 1964 earthquake may also have been a significant factor. The M 7.2-7.4 Delta River earthquake of 1912 (Carver et al., 2004) may have delayed or advanced the timing of the DFE, depending on the details and location of its rupture. The initial subevent of the 2002 DFE earthquake was on the 40-km Susitna Glacier thrust fault at the western end of the Denali fault rupture. The Coulomb stress transferred from the 1964 earthquake moved the Susitna Glacier thrust fault uniformly away from thrust failure by about 100 kPa. The initiation of the Denali fault earthquake was advanced by transfer of 30-50 kPa of positive Coulomb stress to the Susitna Glacier fault (Anderson and Ji, 2003) by the nearby M 6.7 Nenana Mountain foreshock of 23 October 2002. The regional tectonic loading model used here suggests that the Semidi (Alaska Peninsula) segment of the megathrust that ruptured in 1938 (M 8.2) may be reloaded and approaching failure.},
ISSN = {0037-1106},
DOI = {10.1785/0120050007},
year = {2006},
type = {Journal Article}
}
#7
@article{butterworth1930,
author = {Butterworth, S.},
title = {On the theory of Filter Amplifiers},
journal = {Experimental Wireless and the Wireless Engineer 7},
pages = {536-541},
year = {1930},
type = {Journal Article}
}
@phdthesis{clinton2004,
author = {Clinton, J.},
title = {Modern Digital Seismology $-$ Instrumentation, and Small Amplitude Studies in the Engineering World},
year = {2004},
school={Caltech},
}
#9
@article{delouis2010,
author = {Delouis, Bertrand and Nocquet, Jean-Mathieu and Vallee, Martin},
title = {{Slip distribution of the February 27, 2010 Mw=8.8 Maule Earthquake, central Chile, from static and high-rate {GPS}, InSAR, and broadband teleseismic data}},
journal = {Geophysical Research Letters},
volume = {37},
abstract = {The shallow depth underthrust earthquake of February 27, 2010 (Mw 8.8) ruptured the subduction plate interface in central Chile between 34 S and 38 S. We retrieve the spatial and temporal distribution of slip during this mega-earthquake through a joint inversion of teleseismic records, InSAR and High Rate {GPS} (HR{GPS}) data. Additionally, our model is shown to agree with broadband surface waves. Rupture initiated at about 32 km depth and propagated bilaterally resulting in two main slip zones located SSW and NNE of the hypocenter. Nucleation did not take place within or at the edge of one of these main asperities, but in between. During the first 30s, slip propagated predominantly southwards. Later on, the rupture evolved more slowly and more symmetrically. Eventually, the northern asperity became predominant with maximum slip reaching about 20 m. Most of the seismic moment was released within 110s, a relatively short time, explained by the bilateral propagation. The overall average rupture velocity is 2.6 km/s but propagation occurred initially faster towards the south (3.2 km/s). Large slip did not reach the trench, a result consistent with the moderate size of the tsunami. Down-dip, rupture stopped at about 50 km depth, in agreement with the lower limit of the locked zone inferred by Ruegg et al. (2009) from pre-seismic {GPS} data. Citation: Delouis, B., J.-M. Nocquet, and M. Vallee (2010), Slip distribution of the February 27, 2010 Mw = 8.8 Maule Earthquake, central Chile, from static and high-rate {GPS}, InSAR, and broadband teleseismic data, Geophys. Res. Lett., 37, L17305, doi: 10.1029/2010GL043899.},
ISSN = {0094-8276},
DOI = {L17305
10.1029/2010gl043899},
url = {<Go to ISI>://WOS:000281754800002 },
year={2010},
type = {Journal Article}
}
@article{deuss2013,
author = {Deuss, Arwen and Ritsema, Jeroen and van Heijst, Hendrik},
title = {A new catalogue of normal-mode splitting function measurements up to 10 mHz},
volume = {193},
number = {2},
pages = {920-937},
year = {2013},
doi = {10.1093/gji/ggt010},
URL = {http://gji.oxfordjournals.org/content/193/2/920.abstract},
eprint = {http://gji.oxfordjournals.org/content/193/2/920.full.pdf+html},
journal = {Geophysical Journal International}
}
@article{dziewonski1981,
title = "Preliminary reference Earth model",
journal = "Physics of the Earth and Planetary Interiors",
volume = "25",
number = "4",
pages = "297 - 356",
year = "1981",
note = "",
issn = "0031-9201",
doi = "http://dx.doi.org/10.1016/0031-9201(81)90046-7",
url = "http://www.sciencedirect.com/science/article/pii/0031920181900467",
author = "Adam M. Dziewonski and Don L. Anderson",
}
@article{ekstrom2011,
author = {Ekstr\"{o}m, G.},
title = {A global model of Love and Rayleigh surface wave dispersion and anisotropy 25-250 s},
journal = {Geophys. J. Int.},
volume = {187},
number = {3},
pages = {1668-1686},
DOI = {10.1111/j.1365-246X.2011.05225.x},
year = {2011},
type = {Journal Article}
}
#10
@article{elosegui2006,
author = {Elosegui, P. and Davis, J. L. and Oberlander, D. and Baena, R. and Ekstrom, G.},
title = {Accuracy of high-rate {GPS} for seismology},
journal = {Geophysical Research Letters},
volume = {33},
number = {11},
ISSN = {0094-8276},
DOI = {L11308
10.1029/2006gl026065},
url = {<Go to ISI>://WOS:000238569700002 },
year = {2006},
type = {Journal Article}
}
#11
@article{emore2007,
author = {Emore, G. L. and Haase, J. S. and Choi, K. and Larson, K. A. and Yamagiwa, A.},
title = {Recovering seismic displacements through combined use of 1-Hz {GPS} and strong-motion accelerometers},
journal = {Bulletin of the Seismological Society of America},
volume = {97},
number = {2},
pages = {357-378},
ISSN = {0037-1106},
DOI = {10.1785/0120060153},
url = {<Go to ISI>://WOS:000245490500001 },
year = {2007},
type = {Journal Article}
}
@article {friedrich1995,
author = {Friederich, Wolfgang and Dalkolmo, J***INVALID BYTE SEQUENCE HERE***rg},
title = {Complete synthetic seismograms for a spherically symmetric earth by a numerical computation of the Green's function in the frequency domain},
journal = {Geophysical Journal International},
volume = {122},
number = {2},
publisher = {Blackwell Publishing Ltd},
issn = {1365-246X},
url = {http://dx.doi.org/10.1111/j.1365-246X.1995.tb07012.x},
doi = {10.1111/j.1365-246X.1995.tb07012.x},
pages = {537--550},
keywords = {Key words: Green's function, long-period body waves, synthetic seismograms},
year = {1995},
}
#12
@article{garcia2005,
author = {Garcia, R. and Crespon, F. and Ducic, V. and Lognonne, P.},
title = {Three-dimensional ionospheric tomography of post-seismic perturbations produced by the Denali earthquake from {GPS} data},
journal = {Geophysical Journal International},
volume = {163},
number = {3},
pages = {1049-1064},
ISSN = {0956-540X},
DOI = {10.1111/j.1365-246X.2005.02775.x},
url = {<Go to ISI>://WOS:000233435000016 },
year = {2005},
type = {Journal Article}
}
@article{Hayes2011,
author = {Hayes, G. P.},
title = "{Rapid source characterization of the 2011 M $_{w}$ 9.0 off the Pacific coast of Tohoku Earthquake}",
journal = {Earth, Planets, and Space},
keywords = {Great earthquake, earthquake rupture processes, 2011 off the Pacific coast of Tohoku Earthquake, source inversion},
year = 2011,
month = jul,
volume = 63,
pages = {529-534},
doi = {10.5047/eps.2011.05.012},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
#13
@article{houlie2014,
author = {Houli\'{e}, N. and Dreger, D. and Kim, A.},
title = {{GPS} source solution of the 2004 Parkfield earthquake},
journal = {Sci. Rep.},
volume = {4},
pages = {3646},
DOI = {10.1038/srep03646},
year = {2014},
type = {Journal Article}
}
@article {houlie2005,
author = {Houli\'{e}, N. and Briole, P. and Nercessian, A. and Murakami, M.},
title = {Volcanic plume above Mount St. Helens detected with GPS},
journal = {Eos, Transactions American Geophysical Union},
volume = {86},
number = {30},
issn = {2324-9250},
url = {http://dx.doi.org/10.1029/2005EO300001},
doi = {10.1029/2005EO300001},
pages = {277--281},
keywords = {Fluid flow, Instruments and techniques, Explosive volcanism},
year = {2005},
}
#14
@article{houlie2011,
author = {Houli\'{e}, N. and Occhipinti, G. and Blanchard, T. and Shapiro, N. and Lognonne, P. and Murakami, M.},
title = {New approach to detect seismic surface waves in {1Hz}-sampled {GPS} time series},
journal = {Sci Rep},
volume = {1},
pages = {44},
ISSN = {2045-2322 (Electronic)
2045-2322 (Linking)},
DOI = {10.1038/srep00044},
url = {http://www.ncbi.nlm.nih.gov/pubmed/22355563},
year = {2011},
type = {Journal Article}
}
#15
@article{chen2004,
author = {Ji, Chen},
title = {Slip history of the 2003 San Simeon earthquake constrained by combining 1-Hz {GPS}, strong motion, and teleseismic data},
journal = {Geophysical Research Letters},
volume = {31},
number = {17},
ISSN = {0094-8276},
DOI = {10.1029/2004gl020448},
year = {2004},
type = {Journal Article}
}
#16
@unpublished{king2011,
author = {King, B. and Bock, Y.},
title = {GAMIT manual},
year = {2011},
type = {Unpublished Work},
note={}
}
#17
@article{kobayashi2006,
author = {Kobayashi, R. and Miyazaki, S. and Koketsu, K.},
title = {{Source processes of the 2005 West Off Fukuoka Prefecture earthquake and its largest aftershock inferred from strong motion and 1-Hz {GPS} data}},
journal = {Earth Planets and Space},
volume = {58},
number = {1},
pages = {57-62},
ISSN = {1343-8832},
year = {2006},
type = {Journal Article}
}
#18
@article{komatitsch2002,
author = {Komatitsch, D. and Tromp, J.},
title = {{Spectral-element simulations of global seismic wave propagation - II. Three-dimensional models, oceans, rotation and self-gravitation}},
journal = {Geophysical Journal International},
volume = {150},
number = {1},
pages = {303-318},
ISSN = {0956-540X},
DOI = {10.1046/j.1365-246X.2002.01716.x},
url = {<Go to ISI>://WOS:000176445900023 },
year = {2002},
type = {Journal Article}
}
@article {Kustowski2008,
author = {Kustowski, B. and Ekstr\^{o}m, G. and Dziewo\v{n}ski, A. M.},
title = {Anisotropic shear-wave velocity structure of the Earth's mantle: A global model},
journal = {Journal of Geophysical Research: Solid Earth},
volume = {113},
number = {B6},
issn = {2156-2202},
url = {http://dx.doi.org/10.1029/2007JB005169},
doi = {10.1029/2007JB005169},
pages = {n/a--n/a},
keywords = {mantle, tomography, anisotrophy},
year = {2008},
}
#20
@article{larson2003,
author = {Larson, K. and Bodin, P. and Gomsberg, J.},
title = {Using 1-Hz {GPS} Data to Measure Deformations Caused by the Denali Fault Earthquake},
journal = {Science},
volume = {300},
pages = {1421-1424},
year = {2003},
type = {Journal Article}
}
@article{maercklin2012,
author = {Maercklin, N. and Festa, G. and Colombelli, S. and Zollo, A.},
title = {Twin ruptures grew to build up the giant 2011 Tohoku, Japan, earthquake},
journal = {Sci. Rep.},
volume = {2},
number = {709},
DOI = {10.1038/srep00709},
year = {2012},
type = {Journal Article}
}
@article{masson2013,
title={On the numerical implementation of time-reversal mirrors for tomographic imaging},
author={Masson, Y. and Cupillard, P. and Capdeville, Y. and Romanowicz, B.},
journal={Geophysical Journal International},
pages={ggt459},
year={2013},
publisher={Oxford University Press}
}
#21
@article{meng2013,
author = {Meng, Guojie and Ren, Jinwei and Su, Xiaoning and Yang, Yonglin and Zhu, Ze and Ge, Linlin and Li, Xiaojing},
title = {{Coseismic Deformation of the 2010 Mw6.9 Yushu Earthquake Derived from {GPS} Data}},
journal = {Seismological Research Letters},
volume = {84},
number = {1},
pages = {57-64},
DOI = {10.1785/0220120018},
url = {http://srl.geoscienceworld.org/content/84/1/57.short},
year = {2013},
type = {Journal Article}
}
@article{mitsui2012,
author = {Mitsui, Yuta and Heki, Kosuke},
title = {Observation of Earth's free oscillation by dense GPS array: After the 2011 Tohoku megathrust earthquake},
journal = {Sci. Rep.},
volume = {2},
note = {10.1038/srep00931},
url = {http://dx.doi.org/10.1038/srep00931},
year = {2012},
type = {Journal Article}
}
#22
@article{miyazaki2004,
author = {Miyazaki, S. and Larson, K. M. and Choi, K. and Kazuhito Hikima, K. and Koketsu, K. and Bodin, P. and Haase, J. and Emore, G. and Yamagiwa, A.},
title = {{Modeling the rupture process of the 2003 September 25 Tokachi-Oki (Hokkaido) earthquake using 1-Hz {GPS} data}},
journal = {Geophys. Res. Lett.},
volume = {31},
number = {L21603},
year = {2004},
type = {Journal Article}
}
#23
@article{nissenmeyer2014,
author = {Nissen-Meyer, T. and van Driel, M. and Stähler, S. C. and Hosseini, K. and Hempel, S. and Auer, L. and Colombi, A. and Fournier, A.},
title = {{AxiSEM: broadband 3-D seismic wavefields in axisymmetric media}},
journal = {Solid Earth},
volume = {5},
number = {1},
pages = {425-445},
note = {SE},
ISSN = {1869-9529},
DOI = {10.5194/se-5-425-2014},
url = {http://www.solid-earth.net/5/425/2014/},
year = {2014},
type = {Journal Article}
}
@article{okada2004,
author="Okada, Yoshimitsu
and Kasahara, Keiji
and Hori, Sadaki
and Obara, Kazushige
and Sekiguchi, Shoji
and Fujiwara, Hiroyuki
and Yamamoto, Akira",
title="Recent progress of seismic observation networks in Japan ---Hi-net, F-net, K-NET and KiK-net---",
journal="Earth, Planets and Space",
year="2014",
volume="56",
number="8",
pages="xv--xxviii",
issn="1880-5981",
doi="10.1186/BF03353076",
url="http://dx.doi.org/10.1186/BF03353076"
}
#24
@article{ritsema2011,
author = {Ritsema, J. and Deuss, A. and van Heijst, H. J. and Woodhouse, J. H.},
title = {{S40RTS: a degree-40 shear-velocity model for the mantle from new Rayleigh wave dispersion, teleseismic traveltime and normal-mode splitting function measurements}},
journal = {Geophysical Journal International},
volume = {184},
number = {3},
pages = {1223-1236},
ISSN = {0956-540X},
DOI = {10.1111/j.1365-246X.2010.04884.x},
url = {<Go to ISI>://WOS:000287362500016 },
year = {2011},
type = {Journal Article}
}
#26
@article{wright2012,
author = {Wright, T.J. and Houli\'{e}, N. and Hildyard, M. and Iwabuchi, T.},
title = {{Real-time, reliable magnitudes for large earthquakes from {1 Hz} {GPS} Precise Point Positioning: the 2011 Tohoku-Oki (Japan) earthquake}},
journal = {Geophys. Res. Lett.},
DOI = {10.1029/2012GL051894},
year = {2012},
type = {Journal Article}
}
#27
@article{yokota2009,
author = {Yokota, Y. and Koketsu, K. and Hikima, K. and Miyazaki, S.},
title = {{Ability of 1-Hz {GPS} data to infer the source process of a medium-sized earthquake: The case of the 2008 Iwate-Miyagi Nairiku, Japan, earthquake}},
journal = {Geophysical Research Letters},
volume = {36},
ISSN = {0094-8276},
DOI = {10.1029/2009gl037799},
url = {<Go to ISI>://WOS:000267185800002 },
year = {2009},
type = {Journal Article}
}
#28
@article{bock1993,
author = {Bock, Y. and Agnew, D. C. and Fang, P. and Genrich, J. F. and Hager, B. H. and Herring, T. A. and Hudnut, K. W. and King, R. W. and Larsen, S. and Minster, J. B. and Stark, K. and Wdowinski, S. and Wyatt, F. K.},
title = {Detection of Crustal Deformation from the Landers Earthquake Sequence Using Continuous Geodetic Measurements},
journal = {Nature},
volume = {361},
number = {6410},
pages = {337-340},
ISSN = {0028-0836},
DOI = {10.1038/361337a0},
url = {<Go to ISI>://WOS:A1993KJ59000051 },
year = {1993},
type = {Journal Article}
}
#29
@article{bilich2008,
author = {Bilich, A. and Cassidy, J. F. and Larson, K. M.},
title = {{GPS} seismology: Application to the 2002 M-w 7.9 Denali fault earthquake},
journal = {Bulletin of the Seismological Society of America},
volume = {98},
number = {2},
pages = {593-606},
ISSN = {0037-1106},
DOI = {10.1785/0120070096},
url = {<Go to ISI>://WOS:000254528000006 },
year = {2008},
type = {Journal Article}
}
@article{panning2006,
author = {Panning, Mark and Romanowicz, Barbara},
title = {A three-dimensional radially anisotropic model of shear velocity in the whole mantle},
journal = {Geophysical Journal International},
volume = {167},
number = {1},
pages = {361-379},
abstract = {We present a 3-D radially anisotropic S velocity model of the whole mantle (SAW642AN), obtained using a large three component surface and body waveform data set and an iterative inversion for structure and source parameters based on Non-linear Asymptotic Coupling Theory (NACT). The model is parametrized in level 4 spherical splines, which have a spacing of similar to 8 degrees. The model shows a link between mantle flow and anisotropy in a variety of depth ranges. In the uppermost mantle, we confirm observations of regions with V(SH) > V(SV) starting at similar to 80 km under oceanic regions and similar to 200 km under stable continental lithosphere, suggesting horizontal flow beneath the lithosphere. We also observe a V(SV) > V(SH) signature at similar to 150-300 km depth beneath major ridge systems with amplitude correlated with spreading rate for fast-spreading segments. In the transition zone (400-700 km depth), regions of subducted slab material are associated with V(SV) > V(SH), while the ridge signal decreases. While the mid-mantle has lower amplitude anisotropy (< 1 per cent), we also confirm the observation of radially symmetric V(SH) > V(SV) in the lowermost 300 km, which appears to be a robust conclusion, despite an error in our previous paper which has been corrected here. The 3-D deviations from this signature are associated with the large-scale low-velocity superplumes under the central Pacific and Africa, suggesting that V(SH) > V(SV) is generated in the predominant horizontal flow of a mechanical boundary layer, with a change in signature related to transition to upwelling at the superplumes.},
ISSN = {0956-540X},
DOI = {10.1111/j.1365-246X.2006.03100.x},
url = {<Go to ISI>://WOS:000240919900026 },
year = {2006},
type = {Journal Article}
}
@article{park2005,
author = {Park, J. and Song, T. R. A. and Tromp, J. and Okal, E. and Stein, S. and Roult, G. and Clevede, E. and Laske, G. and Kanamori, H. and Davis, P. and Berger, J. and Braitenberg, C. and Van Camp, M. and Lei, X. and Sun, H. P. and Xu, H. Z. and Rosat, S.},
title = {Earth's free oscillations excited by the 26 December 2004 Sumatra-Andaman earthquake},
journal = {Science},
volume = {308},
number = {5725},
pages = {1139-1144},
abstract = {At periods greater than 1000 seconds, Earth's seismic free oscillations have anomalously large amplitude when referenced to the Harvard Centroid Moment Tensor fault mechanism, which is estimated from 300- to 500-second surface waves. By using more realistic rupture models on a steeper fault derived from seismic body and surface waves, we approximated free oscillation amplitudes with a seismic moment (6.5 x 10(22) Newton-meters) that corresponds to a moment magnitude of 9.15. With a rupture duration of 600 seconds, the fault-rupture models represent seismic observations adequately but underpredict geodetic displacements that argue for slow fault motion beneath the Nicobar and Andaman islands.},
ISSN = {0036-8075},
DOI = {10.1126/science.1112305},
url = {<Go to ISI>://WOS:000229293400035 },
year = {2005},
type = {Journal Article}
}
@article{geoscope,
author = {Romanowicz, B. and Cara, M. and Fel, J. F. and Rouland, D.},
title = {GEOSCOPE: A French initiative in long-period three-component global seismic networks},
journal = {Eos, Transactions American Geophysical Union},
volume = {65},
number = {42},
pages = {753-753},
ISSN = {2324-9250},
DOI = {10.1029/EO065i042p00753-01},
url = {http://dx.doi.org/10.1029/EO065i042p00753-01},
year = {1984},
type = {Journal Article}
}
@article{romanowicz2001,
author = {Romanowicz, B. and Giardini, D.},
title = {Geophysics - The future of permanent seismic networks},
journal = {Science},
volume = {293},
number = {5537},
pages = {2000-2001},
ISSN = {0036-8075},
DOI = {10.1126/science.1061771},
url = {<Go to ISI>://WOS:000171028700036 },
year = {2001},
type = {Journal Article}
}
#30
@article{romanowicz2003,
author = {Romanowicz, B.},
title = {Global mantle tomography: Progress status in the past 10 years},
journal = {Annual Review of Earth and Planetary Sciences},
volume = {31},
pages = {303-328},
abstract = {We review the present status of global mantle tomography and discuss two main classes of models that have been developed in the past 10 years: P velocity models based on large datasets of travel times from the International Seismological Centre bulletins, often referred to as "high resolution" models, and S velocity models based on a combination of surface wave and hand picked body wave travel times, or waveforms, referred to as "long wavelength" models. We discuss their respective strengths and weaknesses, as well as progress in the resolution of other physical parameters, such as anisotropy, anelasticity, density, and bulk sound velocity using tomographic approaches. We present the view that future improvements in global seismic tomography require the utilization of the rich information contained in complete broadband seismic waveforms. This is presently within our reach owing to theoretical progress as well as the increase in computational power in recent years.},
ISSN = {0084-6597},
DOI = {10.1146/annurev.earth.31.091602.113555},
url = {<Go to ISI>://WOS:000185093700009 },
year = {2003},
type = {Journal Article}
}
@article{rosat2004,
title = {Performance of superconducting gravimeters from long-period seismology to tides},
journal = {Journal of Geodynamics},
volume = {38},
number = {3***INVALID BYTE SEQUENCE HERE***-5},
pages = {461-476},
year = {2004},
issn = {0264-3707},
doi = {http://dx.doi.org/10.1016/j.jog.2004.07.005},
url = {http://www.sciencedirect.com/science/article/pii/S026437070400081X},
author = {S. Rosat and J. Hinderer and D. Crossley and J.P. Boy}
}
@article{rosat2009,
author = {Rosat, S. and Lambert, S. B.},
title = {Free core nutation resonance parameters from VLBI and superconducting gravimeter data},
DOI= {10.1051/0004-6361/200811489},
url= {http://dx.doi.org/10.1051/0004-6361/200811489},
journal = {A&A},
year = {2009},
volume = {503},
number = {1},
pages = {287-291},
}
@article{roult2006,
author = {Roult, Genevi***INVALID BYTE SEQUENCE HERE***ve and Rosat, S***INVALID BYTE SEQUENCE HERE***verine and Cl***INVALID BYTE SEQUENCE HERE***v***INVALID BYTE SEQUENCE HERE***d***INVALID BYTE SEQUENCE HERE***, Eric and Millot-Langet, Rapha***INVALID BYTE SEQUENCE HERE***le and Hinderer, Jacques},
title = {New determinations of Q quality factors and eigenfrequencies for the whole set of singlets of the Earth's normal modes 0S0, 0S2, 0S3 and 2S1 using superconducting gravimeter data from the GGP network},
journal = {Journal of Geodynamics},
volume = {41},
number = {1-3},
pages = {345-357},
ISSN = {02643707},
DOI = {10.1016/j.jog.2005.08.020},
year = {2006},
type = {Journal Article}
}
# 31
@article{kennett1991,
author = {Kennett, B. L. N. and Engdahl, E. R.},
title = {Traveltimes for global earthquakes location and phase identification},
journal = {Geophys. J. Int.},
volume = {105},
pages = {429-465},
year = {1991},
type = {Journal Article}
}
# 32
@article{woodhouse1984,
author = {Woodhouse, John H. and Dziewonski, Adam M.},
title = {Mapping the upper mantle: Three-dimensional modeling of earth structure by inversion of seismic waveforms},
journal = {Journal of Geophysical Research: Solid Earth},
volume = {89},
number = {B7},
pages = {5953-5986},
keywords = {7206 Seismology: Structure of the crust and upper mantle
7255 Seismology: Surface waves
8121 Tectonophysics: Convection currents},
ISSN = {2156-2202},
DOI = {10.1029/JB089iB07p05953},
url = {http://dx.doi.org/10.1029/JB089iB07p05953},
year = {1984},
type = {Journal Article}
}
#33
@article{ekstrom1997,
author = {Ekstrom, G. and Tromp, J. and Larson, E. W. F.},
title = {Measurements and global models of surface wave propagation},
journal = {Journal of Geophysical Research-Solid Earth},
volume = {102},
number = {B4},
pages = {8137-8157},
abstract = {A new technique for making single-station phase velocity measurements is developed and applied to a large number of globally recorded Rayleigh and Love waves in the period range 35-150 s. The method is based on phase-matched filter theory and iteratively suppresses the effect of interfering overtones by minimizing residual dispersion. The model surface wave signal is described by its amplitude and apparent phase velocity, both of which are parameterized in terms of smooth B-spline functions of frequency. A misfit function is constructed which represents the difference between the model and observed waveforms, and the optimal spline coefficients are estimated in an iterative misfit minimization algorithm. In order to eliminate cycle skips in the measurements of phase at short periods, the waveforms are first matched at long periods, and the frequency range is gradually extended to include higher frequencies. The application of the algorithm to records from the Global Seismographic Network, using earthquakes in the Harvard centroid-moment tensor catalog, results in the determination of more than 50,000 high-quality dispersion curves. The observed variations in measured dispersion for pairwise similar paths are used to estimate realistic uncertainties in the data. Phase delays at discrete periods are inverted for global maps of variations in phase velocity expanded in spherical harmonics up to degree 40. A realistic resolution test indicates that structures are well recovered up to at least degree 20. The new phase velocity maps explain 70-96% of the observed variance in phase residuals, reflecting the high internal consistency of the dispersion measurements.},
ISSN = {0148-0227},
DOI = {10.1029/96jb03729},
url = {<Go to ISI>://WOS:A1997WU87600037 },
year = {1997},
type = {Journal Article}
}
@book{udias2014,
title = {Source Mechanisms of Earthquakes: Theory and Practice},
author={Udias, A. and Madariaga, R. and Buforn E.},
year = {2014},
publisher = {Cambridge University Press},
ISBN = {9781107040274},
type = {Book}
}
@article{montagner2008,
author={Montagner, J.-P. and Roult, G.},
title={Normal modes of the Earth},
journal={Journal of Physics: Conference Series},
volume={118},
number={1},
pages={012004},
url={http://stacks.iop.org/1742-6596/118/i=1/a=012004},
year={2008},
abstract={The free oscillations of the Earth were observed for the first time in the 1960s. They can be divided into spheroidal modes and toroidal modes, which are characterized by three quantum numbers n,l , and m. In a spherically symmetric Earth, the modes are degenerate in m , but the influence of rotation and lateral heterogeneities within the Earth splits the modes and lifts this degeneracy. The occurrence of the Great Sumatra-Andaman earthquake on 24 December 2004 provided unprecedented high-quality seismic data recorded by the broadband stations of the FDSN (Federation of Digital Seismograph Networks). For the first time, it has been possible to observe a very large collection of split modes, not only spheroidal modes but also toroidal modes.}
}
@article{vandriel2014,
author = {van Driel, M. and Nissen-Meyer, T.},
title = {Seismic wave propagation in fully anisotropic axisymmetric media},
volume = {199},
number = {2},
pages = {880-893},
year = {2014},
doi = {10.1093/gji/ggu269},
abstract ={We present a numerical method to compute 3-D elastic waves in fully anisotropic axisymmetric media. This method is based on a decomposition of the wave equation into a series of uncoupled 2-D equations for which the dependence of the wavefield on the azimuth can be solved analytically. Four independent equations up to quadrupole order appear as solutions for moment-tensor sources located on the symmetry axis while single forces can be accommodated by two separate solutions up to dipole order. This decomposition gives rise to an efficient solution of the 3-D wave equation in a 2-D axisymmetric medium. First, we prove the validity of the decomposition of the wavefield in the presence of general anisotropy. Then we use it to derive the reduced 2-D equations of motions and discretize them using the spectral element method. Finally, we benchmark the numerical implementation for global wave propagation at 1?Hz and consider inner core anisotropy as an application for high-frequency wave propagation in anisotropic media at frequencies up to 2?Hz.},
URL = {http://gji.oxfordjournals.org/content/199/2/880.abstract},
eprint = {http://gji.oxfordjournals.org/content/199/2/880.full.pdf+html},
journal = {Geophysical Journal International}
}
@article{wielandt1982,
author = {Wielandt, E. and Streckeisen, G.},
title = {The leaf-spring seismometer; design and performance},
journal = {Bulletin of Seismological Society of America},
volume = {72},
number = {A},
pages = {2349-2367},
year = {1982},
type = {Journal Article}
}
@techreport{peterson1989,
author = {Peterson, J. and Hutt, C. R.},
title = {{IRIS/USGS plans for upgrading the Global Seismograph Network}},
journal = {Open File Rep},
institution={USGS},
year={1989},
}
@article{usarray,
title = {USArray design implications for wavefield imaging in the lithosphere and upper mantle},
author={Levander, A.},
journal = {The Leading Edge},
volume = {22},
number = {3},
pages = {250-255},
year = {2003},
doi = {10.1190/1.1564530}
}
@article{sac,
title = {SAC Availability for the IRIS Community},
author={Goldstein, P. and Snoke, A.},
journal = {Data Services Newsletter},
volume = {7},
number = {1},
pages = {},
year = {2005},
doi = {}
}
@article{pasyanos2010,
title = "Lithospheric thickness modeled from long-period surface wave dispersion ",
journal = "Tectonophysics ",
volume = "481",
number = "1–4",
pages = "38 - 50",
year = "2010",
note = "Insights into the Earth's Deep Lithosphere ",
issn = "0040-1951",
doi = "http://dx.doi.org/10.1016/j.tecto.2009.02.023",
url = "http://www.sciencedirect.com/science/article/pii/S0040195109000997",
author = "Michael E. Pasyanos",
keywords = "Lithosphere",
keywords = "Lithospheric thickness",
keywords = "Upper mantle",
keywords = "Surface waves",
keywords = "Eurasia",
keywords = "Africa",
keywords = "Mantle lid "
}
@article{koketsu2004,
year={2004},
issn={1343-8832},
journal={Earth, Planets and Space},
volume={56},
number={3},
doi={10.1186/BF03353060},
title={Joint inversion of strong motion and geodetic data for the source process of the 2003 Tokachi-oki, Hokkaido, earthquake},
url={http://dx.doi.org/10.1186/BF03353060},
publisher={Springer-Verlag},
keywords={Source process; joint inversion; strong motion data; geodetic data},
author={Koketsu, Kazuki and Hikima, Kazuhito and Miyazaki, Shin’ichi and Ide, Satoshi},
pages={329-334},
language={English}
}
