Twentieth Century History
Seismology and Physics of the Earth's Interior at the
University of Colorado in the 20th Century
Carl Kisslinger, University of Colorado at Boulder, USA, May 1999
Please note that this reflects the status of geophysics at CU as of 1999; we're leaving it here as a reminder of how the program has evolved.
|Servicing CU portable seismic station in eastern Nepal.
Solid-earth geophysics was introduced into the Geology Department at the University of Colorado at Boulder (CU) in 1940
and a seismograph station was set up on campus soon after. A decision to create a program
in geophysics in the Department of Geological Sciences was made in 1960. The first
research efforts were in paleomagnetism and crustal deformation instrumentation and
observations. In 1967, a major development was the creation of the Cooperative Institute for Research in the
Environmental Sciences (CIRES), a joint institute of the University and the National Oceanic and Atmospheric Administration (NOAA) .The
program in seismology was launched in 1972. The research plans have emphasized coordinated
efforts in field observations, laboratory studies, computer simulations, and theoretical
investigations, The principal subjects in the seismology program have been earthquake and
explosion source physics, seismotectonics, earthquake prediction, and studies of structure
and dynamics of the Earth's crust, mantle, and deep interior. Application to earthquake
hazard assessment, prediction, and nuclear test monitoring has been the motivation for
some research. Research and education in other topics within the scope of IASPEI are
carried out through a number of other academic departments and research institutes on the
Table of Contents
1. The beginnings of geophysics at the University of Colorado at
2. The creation of CIRES and the development of the seismology program
3. Research on source physics and seismotectonics, earthquakes and
4. Earthquake prediction research
5. Investigations of the Earth's interior.
**Manuscript submission date: May 18,1999
Professor Carl Kisslinger, University of Colorado, CIRES, Campus Box 216, Boulder, CO
Phone: 1-303-492-6089; FAX 1-303-492-1149; E-mail: email@example.com
1. The beginnings of geophysics at the University of Colorado at
As a result of historical developments driven by a few enterprising individuals,
research programs and advanced study in seismology and the physics of the Earth's interior
in the University of Colorado at Boulder are scattered among a number of academic
departments and research institutes. An interdepartmental Ph.D. Program in Geophysics and
the interdisciplinary emphasis in the Cooperative Institute for Research in Environmental
Sciences (CIRES) have served to encourage integration of these components. In this report,
this history will be traced briefly and the end-of-century activities in these
programs summarized. The history begins quite recently, compared to other major
geophysical organizations around the world.
In 1940, Warren W. Longley (Minnesota*) was appointed to the faculty of the Department
of Geology (later renamed Geological Sciences). His background in mathematics and physics
and his experience in exploration for mineral deposits provided a basis for bringing
geophysics into the department offerings. The first effort in seismology came soon after
with the installation of a seismographic station, consisting of three short-period
instruments recording on film, in the basement of the Geology Building. Longeley
accomplished this in cooperation with the U.S. Coast and Geodetic Survey. The station was
operated by Longley through 1959. It was reactivated by J. C."Chris" Harrison
(Cambridge ) in late 1965 and was in service through 1968 as part of the monitoring of the
earthquakes associated with fluid injection at the Rocky Mountain Arsenal, near Denver.
The department made a decision in 1960 to initiate a distinct program in geophysics.
David Strangway (Toronto) was recruited and brought his expertise in paleomagnetism to
that program in 1961. He left in 1964, but the work in paleomagnetism was continued for
the next 30 years by Edwin Larson (Colorado), Department of Geological Sciences and former
Fellow of CIRES. Strangway's replacement on the faculty was Chris Harrison, whose broad
interests in the geophysical sciences were centered on gravity and geodesy. He is
recognized as the person most responsible for the birth and early nurturing of a prominent
program in geophysics at CU, including the creation of CIRES and of the interdepartmental
Ph.D. program.. The research on crustal deformation begun by Harrison has remained an
important component of the global CU effort. He installed tiltmeters in the Poorman Mine,
near Boulder, (1966), which led to his demonstration that, contrary to widespread practice
of that time, mines are not good sites for tilt measurements because of cavity and
topographic effects. In 1976 he proceeded to develop and deploy borehole tiltmeters.
Concurrently, Judah Levine (NewYork U.)of the Joint Institute for Laboratory Astrophysics
(JILA), was developing a laserstrainmeter, which he also deployed in the Poorman Mine.
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2. The creation of CIRES and the development of the seismology program.
The pivotal step in this history was the creation of CIRES in 1967, under the
leadership of Harrison, who worked closely with the leadership of the Department of
Commerce laboratories in Boulder. CIRES was formed as a joint enterprise of the University
and the Environmental Sciences Service Administration, soon renamed the National Oceanic
and Atmospheric Administration (NOAA), of the U.S. Department of Commerce. CIRES was
conceived as, and remains, an interdisciplinary organization that bridges all aspects of
the sciences of the solid, liquid, and gaseous components of the Earth. The Fellows and
their research programs support and coordinate the interests of a number of academic
departments of the University and a number of the research units of NOAA. A program in
seismology as an area of instruction and research concentration in the University began
with the development of CIRES.
In the late 1960's, one of the NOAA laboratories was the Earth Sciences Laboratory
(ESL), which had absorbed many of the scientists from the U.S. Coast and Geodetic Survey
when that organization, the oldest Federal scientific unit, was made a part of NOAA. The
ESL was doing an excellent job of fulfilling its responsibilities for earthquake
monitoring (it produced the Preliminary Determination of Epicenters reports, other data
products, and had managed the installation and operation of the World Wide Standardized
Seismograph Network (WWSSN)). NOAA was committed to strengthening the research
capabilities of the ESL and saw the cooperative arrangement with the University as a
mechanism for accomplishing this. Therefore, a decision was made to recruit a solid-earth
geophysicist specializing in seismology as the first Director of CIRES. Meanwhile,
Harrison was managing the launch of the new institute as its Acting Director.
Carl Kisslinger (St. Louis U. ) was appointed Director in 1972, a position he held
until mid-1979 (he served a second term, 1993-1994). He promptly began the process of
recruiting Max Wyss (Caltech) and Hartmut Spetzler
(Caltech) as Fellows of CIRES and faculty members in Geological Sciences, and arranged for
E. R. "Bob" Engdahl (St. Louis U.), then with NOAA, to be assigned fulltime to
CIRES as a Fellow. Charles Archambeau (Caltech) joined the group soon after, providing
strength in theoretical seismology to go with the laboratory expertise of Spetzler and the
field observational interests of the others. Subhendu Datta (U. Jadhavpur), professor of
Mechanical Engineering and later a Fellow of CIRES for several years, brought his
expertise in theoretical wave propagation research to the group. Links were formed with
other CU geophysicists whose work in non-seismological studies pre-dated, but
complemented, the CIRES efforts: Jim Wait (Toronto), NOAA and a founding Fellow of CIRES,
expert in electromagnetic wave propagation in the solid Earth and the atmosphere; Edward
A. "Ned" Benton (Harvard), Astro-Geophysics and Fellow of CIRES, geodynamo
theory and geophysical fluid dynamics; Jim Faller (Princeton), JILA, absolute gravity
measurements; Peter Bender (Princeton), JILA, geodesy.
A significant change in circumstances occurred in January, 1973, when the Federal
Office of Management and Budget, Executive Office of the President, decided to remove all
research in solid-earth geophysics, except geodesy, from NOAA and consolidate it with the
programs of the U.S.Geological Survey (U.S.G.S.). The ESL was terminated and many of its
scientists transferred to the U.S.G.S.. In addition to the research functions, all of the
seismological work, including the preparation of the PDE reports, except for the archiving
and distribution of geophysical data bases, was transferred. Some key personnel became
part of the National Geophysical Data Center of NOAA. The administration of NOAA and the
Environmental Research Laboratories encouraged the CIRES leadership to continue the
development of a broad research program in Earth-system science, but the funding for
seismological and other solid-earth studies had to come from sources other than NOAA.
During the following quarter century the principal thrusts of CIRES have shifted to the
atmosphere, climate, and the oceans, with the solid-earth program rounding out a
comprehensive Earth-system sciences effort.
From its beginning, CIRES has enjoyed excellent working relations with Federal
Government agencies beyond its formal relation to NOAA. Collaboration with and research
funding from many agencies engaged in solid-earth research has been fruitful. The National
Science Foundation, U.S.G.S, NASA, and the Department of Energy have been especially
supportive. The research efforts on topics within the scope of IASPEI that evolved from
this beginning can be categorized broadly as seismic source physics and seismotectonics,
investigation of potential techniques for earthquake prediction, and studies of the
internal structure, composition, and processes of the Earth.
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3. Research on seismic source physics, earthquakes and explosions.
The research on seismic sources has been based on a combination of field and
instrumental studies of earthquake generation, laboratory studies of fault formation in
rock specimens using holographic techniques, the theory of fault rupture and wave
generation, and computer simulations of earthquake processes. Engdahl's experience in
designing and operating a seismic network at Amchitka Island before he came to CIRES
provided a good basis for creating the Central Aleutians Seismic Network in 1974, when the
U.S. Geological Survey began to support prediction-related research. This network, which
operated from Adak Island until 1992 under the National Earthquake Hazards Reduction
Program, was expanded and upgraded as time passed. It provided quality data from thousands
of earthquakes in a part of the most prominent subduction zone in the territory of the
United States. When Engdahl left CIRES to join the National Earthquake Information Center
of the U.S.G.S., Kisslinger took over the direction of the network, with major operational
management responsibilities going to Selena Billington (Cornell U.). S.T. Morrissey, on
the staff at St. Louis University, provided the technical expertise for instrumentation
installation and upgrades, and the maintenance of the network under very difficult field
conditions. Several research assistants, including Sharon Kubichek, Robin Wright, Cyndi
McDonald, Susanne Bell, Tom Toth, and Bruce Kindel provided the key staff support for the
data analysis and catalog preparation, The data were the basis for many research papers
and dissertations on the fundamentals of subduction zone seismology, as well as prediction
research described below. The network was dismantled in 1992, when funding was ended.
The research on earthquake sources was not been confined to the Aleutians by any means.
Studies spanned the globe, from east Asia, through central Asia and the eastern
Mediterranean, to Hawaii, the mid-continent of the U.S. and, especially, California.
A series of aftershock studies was originally motivated by the thousands of aftershocks
of the magnitude 8 earthquake of May 7, 1986, within the Central Aleutians Seismic
Network. In addition to the Aleutians, the spatial and temporal distributions of
aftershock sequences in California, Japan, and the Vrancea zone of Romania have been
studied. One goal of these studies has been the clarification of fault-zone properties on
the basis of aftershock behavior. Work on improved mathematical models of earthquake decay
rate has been done by Kisslinger and, especially, Susanna
Gross (U. Colorado).
Early laboratory investigations, under Spetzler and Ivan Getting, used laser holography
to monitor the deformation of a rock mass as fault formation and failure proceeded. They
were joined in this work by many co-workers over the years, including Randolph Martin
(MIT), who became a Fellow of CIRES, and Carl Sondergeld (Cornell). The scope of this
effort broadened and became thoroughly international, as specialists from a number of
countries, listed at the end of this text, joined as Research Associates and visiting
scientists. Processes associated with the preparation of a rock mass for fault slip were
demonstrated and some effects could be correlated with field observations. More recent
work in this laboratory, discussed below, has been concentrated on rock properties at high
pressures, including wave attenuation, subjects more related to the interpretation of data
on deep-earth processes than source studies.
Theoretical work on the production and propagation of earthquake- and
explosion-generated seismic signals has been carried out by Archambeau, as a contribution
to the national program of research on monitoring clandestine nuclear tests. He succeeded
in developing useful criteria for discriminating between natural earthquakes and buried
explosions. His work stimulated and was joined with observational studies of central Asian
events under the Joint Seismic Program, led by Danny Harvey (U. Colorado) and Michael Ritzwoller (U.
California, San Diego) of the Department of Physics. The University was the site of the
IRIS Joint Seismic Program Center for about six years, 1991-1997. Anatoli Levshin (Inst.
Earth Physics, Acad. Sci. USSR), former chief of the Laboratory of Wave Fields
Interpretation, International Institute of Earthquake Prediction Theory and Mathematical
Geophysics of the Russian Academy of Science, joined the group in 1992.
Work on seismic sources was led by John Rundle (U. California, Los
Angeles). He concentrated on the development of computational and analytical
techniques to model, simulate, interpret, and, ultimately, to understand the physics of
earthquakes. In particular, he developed the application of the methods of statistical
physics to the modeling and analysis of earthquake source mechanisms. Many of the
techniques he developed may also have applications to other kinds of non-equilibrium
driven systems, including complex non-linear earth systems. Rundle took the lead in
the formulation and development of a new General Earthquake Model (GEM) simulation
program. This collaboration of many scientists is based at the Southern California
Studies of crustal deformation on local and regional scales have continued as an
important part of the tectonophysics program, much of which is directly linked to
understanding earthquake source processes and crustal movements associated with volcanoes.
Starting with the pioneering work of Harrison, mentioned above, this effort has employed
point measurements using strain and tilt meters, creep meters, gravity measurements,
electronic distance measuring devices (EDM) in fault zones, and now, Synthetic Aperture
Radar (SAR) and Global Positioning System (GPS) surveys. The EDM work, concentrated on the
San Andreas fault, was the primary contribution of Larry Slater, a former Fellow of CIRES.
A major contribution to the interpretation of measurements of changes in surface elevation
and ground tilt was provided by William Farrell (U.California, San Diego), who studied in
detail the influence of ocean loading variations on crustal deformation observations. John
Wahr (Colorado), Fellow of CIRES and Professor of Physics, contributed to theory and
modeling of post-seismic deformation as one part of his analysis of surface elevation
variations, described below.
In 1986, Roger Bilham
(Cambridge U.) and Randolph Ware (Colorado) created the nucleus of UNAVCO, a consortium of universities (now
more than 100) applying GPS methods to the study of global tectonics. CIRES currently owns
22 GPS receivers that are operating in permanent or mobile arrays in th e Himalayas,
Tibet, China, Venezuela, Mexico, and Ethiopia.. The work continues to contribute to
understanding regional or continental scale deformations, as well as local changes related
to earthquake generation. The GPS work is currently led by Bilham and Kristine Larson (U.
California, San Diego).Numerical modeling has been an important tool in the interpretation
of the field data.
A recent innovative application of strain measurements is the monitoring of strains in
the soft soil under Mexico City associated with strong motions following large
subduction-zone earthquakes along Mexico's southern coast.
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4. Earthquake prediction research.
Much of the innovative research on prediction of earthquakes at CIRES was led by Max
Wyss, who left CU in 1991. Variations in numerous geophysical parameters were examined for
precursory patterns using global and regional (Hawaii, California, Turkey, Alaska)
observations. In particular, Wyss and R. E. "Ted" Habermann
(Colorado), (currently a NOAA Fellow of CIRES) focused attention on seismicity rate
decreases (quiescence) prior to large earthquakes. As an integral part of these studies,
they developed quantitative tools for recognizing and understanding apparent seismicity
variations caused by changes in seismic networks and data processing procedures. They
demonstrated that many seismicity rate variations proposed as precursors are artificial
and can be explained by common network changes. Wyss also investigated crustal uplift and
subsidence as revealed by tide-gauge data and systematic variations in b-value as
Kisslinger and Engdahl carried out prediction studies based mostly on observations with
the Central Aleutians Seismic Network. A number of phenomena that have been suggested as
precursory to an imminent earthquake were investigated. These included systematic rotation
of focal mechanisms of local events before a stronger event, the isolation of possible
asperities on the subduction thrust surface on the basis of the distribution of background
seismicity and stress drops, variations in attenuation based on measurements of coda-Q,
investigations of localized changes in seismic body-wave velocities prior to a strong
event, and seismic quiescence. Of these, quiescence as detected with the data from an
adequate local network emerged as most promising, but no consistently successful precursor
has been identified
Recent work by Rundle and others in the areas of non-linear continuum mechanics,
chaotic behavior and the physics of complex systems may lead to advances in prediction
technology, or, at least to a better understanding of approaches to overcoming the
difficulties. Rundle is approaching earthquake forecasting through the analysis of neural
networks. Projects done by his group have emphasized the development of techniques for
understanding the space-time patterns and correlations that appear in many
high-dimensional complex non-linear systems, including patterns of seismicity. The
patterns are quantified in terms of eigenvectors of defined autocorrelation operators.
Measurements of tilt in the Long Valley Caldera, California, and of creep on the
Hayward fault in the San Francisco Bay region, both directed by Bilham, are now part of
early warning systems in these active zones. Data from these monitoring arrays are updated
every 10 minutes on the following Web sites:
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5. Investigations of the Earth's interior.
Studies of the structure, composition, and processes in the interior of the Earth
have included investigations from the crust and upper mantle to the deep mantle and the
core. The tools have included the deployment of portable broadband PASSCAL instruments in
both passive and active field experiments, and studies of body waves, surface waves, and
free oscillations using data from the global seismographic observing system.
Crust and Upper Mantle. The recent work on the structure and dynamics of the crust and
upper mantle has been led by Anne
Sheehan (MIT) and Craig Jones
(MIT), both in the Department of Geological Sciences and Fellows of CIRES. Their
geophysical studies are strongly supplemented by the geochemical research of G. Lang Farmer (U.
California, Los Angeles), also affiliated with Geology and a Fellow of CIRES, who applies
radiogenic isotope systematics to problems of the origin and evolution of continental
crust and tectonic modification of continental mantle lithosphere.
Experiments in which Sheehan and Jones have participated include the
Rocky Mountain Front experiment, Colorado Plateau/Great Basin seismic
experiment, Sierran Paradox I and II, Snake River plain experiment,
and the Continental Dynamics of the Rocky Mountains experiment. Sheehan
and CIRES Research Associate Ken Dueker
have developed high-resolution imaging techniques using phases converted at subsurface
seismic discontinuities and have applied these to dense PASSCAL deployments. Other
studies include seismic anisotropy and applications of seismic tomography.
The efforts of this group also extend to the sea floor, with participation in the MELT
ocean bottom seismograph experiment on the East Pacific Rise, which explored the structure
and dynamics of this mid-ocean ridge, and the Lau Basin experiment in the western Pacific.
The Deep Interior. The late Ned Benton carried out some of the earliest work at CU on
the deep interior. His primary interest was the physics of the geodynamo and other
problems in fluid dynamics related to core processes and the generation of the geomagnetic
field. He was one of the creators of the IUGG program Study of the Earth's Deep Interior
Seismic array analysis by Bob Engdahl and co-workers permitted the recovery of clear
observations of previously undetected or unexplained seismic phases. The source of these
phases was convincingly associated with major boundaries in the Earth. Reflected core
phases were used to fix accurately the radii of the inner and outer core and to describe
the nature of these boundaries. These data are still used as a standard to test Earth
Some of the first CIRES work on the analysis of surface waves and normal modes was
performed by Martin Smith (Princeton), a former Fellow of CIRES also associated with the
Department of Physics.
John Wahr and his
co-workers have made significant contributions to studies of the interior, with emphasis
on the applications of geodetic information (Earth rotation, gravity), in addition to the
analysis of seismic wave travel-times. He and graduate student Artie Rodgers tried to use
ISC travel- times to infer core-mantle boundary (CMB) topography and concluded that the
data were inadequate for providing accurate maps. He and Juergen Neuberg examined PcP
reflections from a small portion of the CMB to derive topography and in the process noted
a reflection that is presumably from the top of D".
This group also examined the possibility of laterally-varying structure in the core
caused by density anomalies in the mantle. They were able to quantify the possible size of
this variability and compute its effects on various observable quantities. With co-workers
from Belgium, Wahr examined how internal density anomalies would perturb the geoid and the
shapes of all boundaries, whether at the surface or internal.
Wahr's work on post-glacial rebound encompassed extension of the computational
formalism and quantification of the sources of error in inferring mantle viscosity from
rebound observations. His group carried out numerous studies of the use of new types of
geodetic observations in rebound investigations and estimated the deformation of the outer
surface and internal boundaries caused by the rebound. His work on earth tides and
nutations led to an effective formalism for studying the shape of the CMB, as well as a
method for using earth tides to infer mantle Q at tidal periods.
Work on the deep interior is also led by Michael Ritzwoller, Department of Physics and
affiliate of CIRES. In addition to his Earth-oriented research, he contributes to efforts
to understand how large-scale convection in the solar convection zone affects helioseismic
oscillations. Some of his work with numerous colleagues, including J. Resovsky and E.
Lavely, has focused on the theory and applications of normal mode analysis. They have
developed three-dimensional models of mantle structure, including a recent (1999) model of
mantle shear wave velocity structure. They are now working on the density structure of the
mantle from normal modes. Ritzwoller contributed some of the earliest work leading to
discovery of inner core anisotropy.
This group, with major contributions from A. Levshin, have completed group velocity
tomography, in the period range 20-200 sec., to estimate continental crustal and uppermost
mantle structure in Antarctica, Eurasia, South America and the Arctic. Levshin has
contributed to the development of a new technique for measurement of surface wave
characteristics (dispersion, polarization, spectral amplitudes) that is efficient and
convenient for analyzing large volumes of data. Ritzwoller and co-authors were among the
first to invert globally orbiting long-period surface waves for lateral attenuation models
of the upper mantle.
The laboratory studies of mineral physics of the kind done by Spetzler and Getting, as
well as Joseph Smyth of
Geological Sciences, provide essential background for the interpretation of seismic
observations in terms of internal composition and processes. Currently Spetzler is working
on the chemical and physical effects of fluid flow in undersaturated porous rocks, with
emphasis on seismic wave attenuation, and studies of mantle rheology through experimental
determinations of shear anelasticity in candidate mantle minerals. He has also been
carrying out geophysically important high-pressure, high-temperature equation-of-state
measurements in a diamond anvil cell, using ultrasonic (GHz) interferometry and x-rays.
Getting has developed a unique apparatus for measuring attenuation and dispersion in
mantle minerals at seismic frequencies and small strains. The attenuation observed in
these and other experiments is much more frequency-dependent than indicated by field
observations and this raises some crucial questions for the science. Getting has also
developed a number of devices for high-pressure experiments that have been installed in
several of the premier laboratories in the United States.
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* The place or university names indicate the institution from which the person received
his or her highest degree. Additional information about many of the individuals mentioned
here and the programs offered in the various institutes and academic departments mentioned
here may be found at the following Internet addresses:
Fellows, Visiting Fellows, Research Associates, and other scientists who have
contributed to the solid-earth geophysics program while in residence at CIRES who are not
referred to in the above text.
Tomas L. Chelidze
F. A. Dahlen
Leonard E. Johnson
H. Paul Johnson
Charles M. Meertens
James H. Whitcomb
Representative sample of publications in IASPEI-related sciences by University of
Colorado geophysicists and their co-authors (CIRES and others). This partial list is
intended only to show the breadth and scope of research efforts.
Agnew, D., Nonlinearity in rocks: Evidence from earth tides, J. Geophys. Res. 86:
Ando, M.,Y. Ishikawa, F. Yamazaki, Shear wave polarization anisotropy in the upper
mantle beneath Honshu, Japan, J.Geophys. Res. 88: 5750-5864,1983.
Archambeau, C.B., J.B. Minster, Dynamics in prestressed media with moving phase
boundaries: A continuum theory of failure in solids, Geophys. J. Roy. Astro. Soc. 52:
Bilham, R., Surface slip subsequent to the 24 November 1987 Superstition Hills,
California, earthquake monitored by digital creepmeters, Bull. Seism. Soc. Amer. 79:
Bilham, R., The 1737 Calcutta earthquake and cyclone evaluated, Bull. Seism. Soc. Amer.
84: 1650-1657, 1994.
Bilham, R., K. Larson, J. Freymueller, Project Idyihim members, GPS measurements of
present-day convergence across the Nepal Himalaya, Letter to Nature 386: 61-64, 1997.
Billington, S., E.R. Engdahl, S. Price, Changes in seismicity and focal mechanisms of
small earthquakes prior to an Ms 6.7 earthquake in the central Aleutian island arc,
Earthquake prediction-An Int'l Rev., Maurice Ewing Series 4:348-356, 1981.
Billington, S., C. Frohlich, E.R. Engdahl, A. Malahoff, Detection and location of
earthquakes in the central Aleutian subduction zone using island and ocean bottom
seismograph stations, J. Geophys. Res. 87: 6853-6864, 1982.
Bowman, J. R., C. Kisslinger, Seismicity associated with a cluster of earthquakes of
mb>4.5 near Adak, Alaska: Evidence for an asperity?, Bull. Seism. Soc. Amer. 75:
Brodsky, N., I. C. Getting, H. Spetzler, an experimental and theoretical approach to
rock deformation at elevated temperature and pressure, Sp. Tech. Pub. 869, Amer. Soc.
Testing and Materials: 37-54, 1985.
Burnley, P. C., The fate of olivine in subducting slabs: a reconnaissance study, Amer.
Mineralog. 80: 1293-1301, 1995.
Chen, G., H. Spetzler, Complexities of rock fracture and rock friction from deformation
of Westerly granite, Pure & Appl. Geophys. 140: 123-135, 1993.
Cormier, V. F., The synthesis of complete seismograms in an earth model specified by
radially inhomogeneous layers, Bull. Seism. Soc. Amer. 70: 691-716, 1980.
Datta, S.K., A.H. Shah, W. Karunasena, Wave propagation in composite media and material
characterization, in Elastic Waves and Ultrasonic Nondestructive Evaluation: 135-141, S.
K. Datta, J.D. Achenbach, Y.S. Rajapakse,
Elsevier Sci. Publs, 1990.
Dahlen, F.H., M.L. Smith, The influence of rotation on the free oscillations of the
Earth, Phil. Trans. Roy. Soc. London A 279: 583-629, 1975.
Douglas, B. J., S. L. Saul, C. R. Stern, Rheology of the upper mantle beneath
southernmost South America inferred from peridotite xenoliths, J. Geol. 95: 241-253, 1987.
Dueker, K., A.F. Sheehan, Mantle discontinuity structure from midpoint stacks of
converted P to S waves across the Yellowstone hotspot track, J. Geophys. Res. 102 :
Dueker, K., A.F. Sheehan, Mantle discontinuity structure beneath the Colorado Rocky
Mountains and High Plains, J. Geophys. Res. 103: 7153-7169, 1998.
Engdahl, E.R., L.E. Johnson, Differential PcP travel times and the radius of the core,
Geophysical J., 39: 435-456, 1974
Engdahl, E.R., E.A. Flinn, R.P. Mass, Differential PkiKP times and the radius of the
inner core, Geophysical J. 30: 457-463, 1974
Engdahl, E. R., W. H. K. Lee, Relocation of local earthquakes by seismic ray tracing,
J. Geophys. Res. 81: 4400-4066, 1976
Engdahl, E.R., S. Billington, Focal depth determination of central Aleutian
earthquakes, Bull. Seis. Soc. Amer. 76: 77-93, 1986.
Engdahl, E.R., S. Billington, C. Kisslinger, Teleseismically recorded seismicity before
and after the May 7, 1986, Andreanof Islands, Alaska, earthquake, J. Geophys. Res. 94:
Evernden, J., C.B. Archambeau, E. Cranswick, An evaluation of seismic decoupling and
underground nuclear test monitoring using high-frequency seismic data, Rev. Geophys. 24:
Farmer, G.L., F.V. Perry, S. Semken, B. Crowe, D. Curtis, D. J. DePaolo, Isotopic
evidence on the structure and origin of subcontinental lithospheric mantle in southern
Nevada, J. Geophys. Res. 94: 7885-7898, 1989.
Farrell, W.E., Deformation of the Earth by surface loads, Rev. Geophys. Space Phys. 10:
Farrell, W.E., Earth tides, ocean tides and tidal loading, Phil. Trans. Roy. Soc.
London, A 274: 253-259, 1973.
Francis, T.J.G., The ratio of compressional to shear wave velocity and rock porosity on
the axis of the mid-Atlantic ridge, J. Geophys. Res. 81: 4361-4364, 1976.
Getting, I.C., J. Paffenholz, H.A. Spetzler, Measuring attenuation in geologic
materials at seismic frequencies and amplitudes, in The brittle-ductile transition in
rocks, AGU Geophys. Monograph 56: 239-243, 1990.
Getting, I.C., S.J. Dutton, P.C. Burnley, S-I. Karato, H.A. Spetzler, Shear attenuation
and dispersion in MgO, Phys. Earth and Planetary Interiors, 99: 249-257, 1997.
Gross, S.J., Magnitude distributions and slip scaling of heterogeneous seismic sources,
Bull. Seism. Soc. Amer.86: 498- 504, 1996.
Gross, S.J. C. Kisslinger, Tests of Models of aftershock decay, Bull. Seism.Soc. Amer.
84: 1571-1579, 1994.
Gross, S.J., C. Kisslinger, Estimating tectonic stress rate and state with Landers
aftershocks, J. Geophys. Res. 102: 7603-7612, 1997.
Gross, S.J., J.B. Rundle, A systematic test of time-to-failure analysis, Geophys. J.
Int'l 133: 57-64, 1998.
Habermann, R.E., Consistency of teleseismic reporting since 1963, Bull. Seism. Soc.
Amer. 72:93-111, 1982.
Habermann, R.E., M.S. Craig, Comparison of Berkeley and CALNET magnitude estimates as a
means of evaluating temporal consistency of magnitudes in California, Bull. Seism. Soc.
Amer. 78: 1255-1267, 1988.
Habermann, R.E., Seismicity rate variations and systematic changes in magnitudes in
teleseismic catalogs, Tectonophysics 193:277-289, 1991.
Harrison, J.C., Cavity and topographic effects in tilt and strain measurement, J.
Geophys. Res. 81: 319-328, 1976.
Harrison, J.C., Tilt observations in the Poorman mine, near Boulder, Colorado,
J.Geophys. Res. 81: 329-336, 1976.
Harrison, J.C., J. Levine, C.M. Meertens, Design of a deep borehole tiltmeter, Proc.
Ninth Intn'l Symp. on Earth Tides: 273-281, 1983.
Harvey, D.J., Seismogram synthesis using normal mode superposition: the locked mode
approximation, Geophys. J. Roy. Astro Soc. 66: 37-69, 1981.
Harvey, D.J., M. Wyss, Comparison of a complex rupture model with the precursor
asperities of the 1975 Hawaii Ms 7.2 earthquake, Pure & Appl. Geophys, 124: 957-973,
Hebenstreit, G.T., E.N. Bernard, Azimuthal variations in tsunami interaction with
multiple-island systems, J. Geophys. Res. 90: 3353-3360, 1985.
Herrmann, R.B. The use of duration as a measure of seismic moment and magnitude, Bull.
Seism. Soc. Amer. 65: 899- 913, 1975.
Johnson, L.E., A new datum for use in the body wave travel time inverse problem,
Geophys. J. Roy. Astor. Soc.30: 1972.
Jones, C.H., H. Kanamori, S.W. Roecker, Missing roots and mantle "drips":
regional Pn and teleseismic arrival times in the southern Sierra Nevada and vicinity,
California, J. Geophys. Res. 99: 4567-4601, 1994.
Jones, C.H., R. Phinney, Seismic structure of the lithosphere from teleseismic
converted arrivals observed at small arrays in the southern Sierra Nevada and vicinity,
California, J. Geophys. Res. 103: 10,065-10090, 1998.
Khattri, K., M. Wyss, Precursory variation in seismicity rate in the Assam area, India,
Geology, 6: 685-688, 1978.
Kisslinger, C., Processes during the Matsushiro, Japan earthquake swarm as revealed by
leveling, gravity, and spring- flow observations, Geology : 57-62, Feb. 1975.
Kisslinger, C., An experiment in earthquake prediction and the 7 May 1986 Andreanof
Islands earthquake, Bull. Seism. Soc. Amer. 78: 218-2229, 1988.
Kisslinger, C., L.M. Jones, Properties of aftershock sequences in southern California,
J. Geophys. Ree. 96: 11,947- 11,958, 1991.
Kisslinger, C., Aftershocks and fault-zone properties, Advances in Geophysics 30: 1-36,
Liang, B., C. Kisslinger, C. Bryan, Estimates of the stress field in Kilauea's south
flank, Hawaii, Geophys. J. Int'l 123: 213-231, 1995.
Martin, R.J. III, M. Wyss, Magnetism of rocks and volumetric strain in uniaxial failure
tests, Pure & Appl. Geophys. 113: 51-61, 1975.
Martin, R.J. III, R.E. Habermann, M. Wyss, The effect of stress cycling and inelastic
volumetric strain on remanent magnetization, J. Geophys. Res. 83: 3485-3496, 1978.
Meertens, C.M., R.B. Smith, Crustal deformation of the Yellowstone caldera from first
GPS measurements: 1987- 1989, Geophys. Res. Letters 18: 1763-1766, 1991.
Mizutani, H., H. Spetzler, H. Murakami, Brittle behavior of rocks at high pressure,
High Pressure Research in Geophysics, Advances in Earth and Planetary Sciences 12:
Paffenholz, J., H. Burkhardt, Absorption and modulus measurements in the seismic
frequency and strain range on partially saturated sedimentary rocks, J. Geophys. Res. 94:
Peltier, W.R., Penetrative convection in the planetary mantle, Geophys. Fluid Dynamics
5: 47-88, 1972.
Qamar, A., Revised velocities in the Earth's core, Bull. Seism. Soc. Amer., 63 :
Qamar, A., A. Eisenberg, The damping of core waves, J. Geophys. Res. 79: 758-765, 1974.
Resovsky, J.S., M.H. Ritzwoller, A degree 8 mantle shear velocity model from normal
mode observations below 3 mHz, J. Geophys. Res.104: 993-1014, 1999.
Riad, S., H. Meyers, Earthquake catalog for the Middle East countries, 1900-1983, World
Data Center A for Solid Earth Geophysics, Rpt SE-40: 1-127, NOAA, Boulder, CO, 1985.
Rikitake, T., Statistics of ultimate strain of the earth's crust and probability of
earthquake occurrence, Tectonophysics 26: 1-21, 1975.
Ritzwoller, M.H., E.M. Lavely, Three-dimensional seismic models of the Earth's mantle,
Rev. Geophys. 33: 1-66,
Ritzwoller, M.H., A.L. Levshin, Eurasian surface wave tomography: Group velocities, J.
Geophys. Res. 103: 4839- 4878, 1998.
Rundle, J.B., Magnitude-frequency relations using a statistical-mechanical approach, J.
Geophys. Res. 98: 21,943- 21,949, 1993.
Rundle, J.B., W. Klein, S. Gross, Dynamics of a traveling density wave model for
earthquakes, Phys. Rev. Lett., 76: 4285-4288, 1996.
Rundle, J.B., E. Preston, S. McGinnis, W. Klein, Why earthquakes stop: Growth and
arrest in stochastic fields, Phys. Rev. Lett. 80: 5698-5701, 1998.
Sasao, T., J. Wahr, An excitation mechanism for the free 'core nutation', Geophys. J.
Roy. Astro Spco. 64: 729-746, 1981.
Scherbaum, F., C. Kisslinger, Variations of apparent stresses and stress drops prior to
the earthquake of 6 May 1984 (mb=5.8) in the Adak seismic zone, Bull. Seism. Soc. Amer.74:
Scherbaum, F., Combined inversion for the three-dimensional Q structure and source
parameters using microearthquake spectra, J. Geophys. Res. 95: 12,423-12,438, 1990.
Sheehan, A.F., Abers, G.A.,Jones, C.H., Lerner-Lam, A.L., Crustal thickness variations
across the Colorado Rocky Mountains from teleseismic receiver functions, J. Geophys. Res.
Slater, L.E., Episodic block motion and convergence along the Calaveras fault in
central California, Tectonophysics 71: 87-94, 1981.
Slater, L.E., J.O. Langbein, M.F. Linker, A. McGarr, Observations of strain
accumulation across the San Andreas fault near Palmdale, CA, with a two-color geodimeter,
Science 218: 1217-1219, 1982.
Smith, M.L., F.A. Dahlen, The period and Q of the Chandler wobble, Geophys. J. Roy.
Astro, Soc. 64: 223-281, 1981.
Soga, N., H. Mizutani, H. Spetzler, R.J. Martin III, the effect of dilatancy on
velocity anisotropy in Westerly granite, J. Geophys. Res. 83: 4451-4458, 1978.
Sondergeld, C.H., L.A. Granryd, H.A. Spetzler, Compressional velocity measurements for
a highly fractured lunar anorthosite, 10th Proc. Lunar Planet. Sci. Conf.: 2147-2154,
Sondergeld, C.H., L.H. Estey, Acoustic emission study of microfracturing during the
cyclic loading of Westerly granite, J. Geophys. Res. 86: 2915-2924, 1981.
Spall, H., Paleomagnetic evidence for a Cretaceous disturbing event in the Precambrian
Johnny Lyon granodiorite, Cochise County, Arizona, J. Geol. 79: 118-122, 1970.
Spetzler, H.A., I.C. Getting, R.J. Martin III, Application of holographic
interferometry to high pressure experiments, High-Pressure Science & Technology 1:
Spetzler, H., C. Sondergeld, G. Sobolev, B. Salov, Seismic and strain studies on large
laboratory rock samples being stressed to failure, Tectonophysics 144: 55-68, 19987.
Spetzler, H., A. Yoneda, Performance of the complete travel-time equationof state at
high pressure and temperature, Pure & Appl. Geophys. 141: 379-392, 1993.
Tanaka, T., Effect of dilatancy on ocean load tides, Pure & Appl. Geophys. 114:
Toth, T., C. Kisslinger, Revised focal depths and velocity model for local earthquakes
in the Adak seismic zone, Bull. Seism. Soc. Amer. 74: 1349-1360, 1984.
Wahr, J., M. Wyss, Interpretation of post-seismic deformation with a viscoelastic
relaxation model, J. Geophys. Res. 85: 6471-6477, 1980.
Wahr, J.M., Normal modes of the coupled earth and ocean system, J. Geophys. Res. 89:
Wahr, J., D. de Vries, The possibility of lateral structure inside the core and its
implications for nutation and earth tide observations, Geophys. J. Int. 99: 511-519, 1989.
Wier, S., Surface wave dispersion and Earth structure in southeastern China, Geophys.
J. Roy. Astro. Soc. 69: 33-47, 1982.
Wyss, M., Towards a physical understanding of the earthquake frequency distribution,
Geophys. J. Roy. Astro. Soc. 31: 341-359, 1973.
Wyss, M., F.W. Klein, A. Johnston, Precursors to the Kalapana M=7.2 earthquake, J.
Geophys. Res.86: 3881-3900, 1981.
Wyss, M., R.E.Habermann, Precursory seismic quiescence, Pure & Appl. Geophys.126:
Wyss, M. (Ed), Evaluation of proposed earthquake precursors, 1989/1990 IASPEI
Sub-commission on Earthquake Prediction, AGU Monograph: 1-94, 1991.