a new view of earthcais.gsi.go.jp/ujnr/ujnr4p/whitcomb-nsf.pdf · san andreas fault observatory at...
TRANSCRIPT
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A New Viewof Earth
IntegratedScience
InSAR
SAFOD
PBO
USArray
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The EarthScope Scientific Vision
To understand
the structure and
deformationof the North American continent
in four dimensions
x,y,z,t
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Four-dimensional imaging of tectonic North America requires all EarthScope component facilities
• USArray Images deformational structures at depth.
• PBO Observes surface deformation with high temporal and spatial resolution.
• InSAR Complementary geodetic tool provides deformation coverage over broad areas.
• SAFOD Directly samples the material properties of an actively deforming zone at depth.
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EarthScope Science Goals• Structure and evolution of the continent• Earthquake processes and seismic hazards• Magmatic processes and volcanic hazards• Active deformation and tectonics• Continental geodynamics• Fluids in the crust• Exploration and discovery
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Some Key Questions
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Some Key Questions• What are the underlying geologic processes governing
deformation of the North American continent?
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Some Key Questions• What are the underlying geologic processes governing
deformation of the North American continent?• On what geologic structures do these processes occur?
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Some Key Questions• What are the underlying geologic processes governing
deformation of the North American continent?• On what geologic structures do these processes occur?• What are the spatial and temporal scales of deformation
across the continent?
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Some Key Questions• What are the underlying geologic processes governing
deformation of the North American continent?• On what geologic structures do these processes occur?• What are the spatial and temporal scales of deformation
across the continent?• How are earthquakes, volcanoes, and mountain building
related to pre-existing geologic structures and patterns of ongoing deformation?
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Some Key Questions• What are the underlying geologic processes governing
deformation of the North American continent?• On what geologic structures do these processes occur?• What are the spatial and temporal scales of deformation
across the continent?• How are earthquakes, volcanoes, and mountain building
related to pre-existing geologic structures and patterns of ongoing deformation?
• How are features at Earth’s surface related to structures in Earth’s interior?
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Some Key Questions• What are the underlying geologic processes governing
deformation of the North American continent?• On what geologic structures do these processes occur?• What are the spatial and temporal scales of deformation
across the continent?• How are earthquakes, volcanoes, and mountain building
related to pre-existing geologic structures and patterns of ongoing deformation?
• How are features at Earth’s surface related to structures in Earth’s interior?
• How can the spatial and temporal patterns of deformation together with knowledge of their associated structures be used in predicting the behaviors of seismic, volcanic, and other geodynamic phenomena?
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EarthScope will increaseour resolution of theSubsurface Structure
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Topography of western U.S.filtered at 500 km wavelength
Topography of western U.S.filtered at 30 km wavelength
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EarthScope willenhance the
spatio-temporalcontrol on regional
Rates of Deformation
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GEOLOGY
PALEOSEISMOLOGY
GEODESYSEISMOLOGY
A Broad Band Approachto Measuring Deformation
Through Time
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EarthScope willadvance our understanding
ofActive Tectonics,
Earthquake and MagmaticProcesses,
andSeismic and Volcanic Hazard
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EarthScope will capitalizeon the notion of theNatural Laboratory*
* Where representative behaviors of a complex system can be investigated in appropriate context and detail, and with the appropriate complement of expertise and instrumentation (NRC BROES Report, 2001).
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North America as a Natural Laboratory
• Diverse array of continental processes and structures
• Multi-disciplinary investigations
• Multi-scale observations
• Existing data bases
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USArray – Components• Transportable Array
– fixed design broadband array - “Bigfoot”– flexible pool: broadband, short period,
high frequency instrumentation– magnetotelluric systems
• Permanent Reference Network– GSN/NSN quality seismometers– geodetic quality GPS receivers
• All data to community in near real time
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USArray – "Bigfoot"• 400 broadband
seismometers– 70 km spacing– Nominal 1400 x 1400
km grid• 50 magnetotelluric
field systems• Deployments for ~18
months at each site• Rolling deployment
over ~ 10 years
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Tectonic provinces of the U.S. with USArray footprint.70 km spacing between seismic stations (red dots).
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USArray can:• Provide increased resolution at depth through
comprehensive 3-D coverage of the continental U.S., with possible extensions into Mexico and Canada, and onto the continental margins.
• Tie together seemingly disparate tectonic provinces into a coherent model of the origin and evolution of the continental lithosphere.
• Tie the lithosphere to structures in the deeper mantle.
• Combine local and regional, and short and long term observations of subsurface imaging.
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USArray – Products• Crust and upper-mantle geologic structure
• Maps of the Moho, transition zones, and core-mantle boundary
• Three-dimensional seismic velocity models of the crust and upper mantle
• Maps of regional seismic attenuation
• Maps of crust and mantle anisotropy
• Earthquake mechanisms
All at high resolution
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Plate BoundaryObservatory
Imaging the Deformation of Tectonic North America
in Four Dimensions
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Plate BoundaryObservatory
Imaging the Deformation of Tectonic North America
in Four Dimensions
• Physics of earthquakes
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Plate BoundaryObservatory
Imaging the Deformation of Tectonic North America
in Four Dimensions
• Physics of earthquakes
• Physics of magmaticprocesses
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Plate BoundaryObservatory
Imaging the Deformation of Tectonic North America
in Four Dimensions
• Physics of earthquakes
• Physics of magmaticprocesses
• Plate boundary dynamics and evolution
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PBO – A Two-Tiered Deployment of Geodetic
Instrumentation
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PBO – A Two-Tiered Deployment of Geodetic
Instrumentation• A backbone of ~100 sparsely
distributed continuous GPS receivers to provide a synoptic view of the entire North American plate boundary deformation zone.
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PBO – A Two-Tiered Deployment of Geodetic
Instrumentation• A backbone of ~100 sparsely
distributed continuous GPS receivers to provide a synoptic view of the entire North American plate boundary deformation zone.
• Clusters of GPS receivers and strainmeters to be deployed in areas requiring greater spatial and temporal resolution, such as fault systems and magmatic centers (775 GPS units & 200 strainmeters).
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GPS Backbone;The Big Picture
The Backbone will:
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GPS Backbone;The Big Picture
The Backbone will:• Extend from west coast to
eastern edge of Rocky Mountains, and from Alaska to Mexico (with international collaboration).
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GPS Backbone;The Big Picture
The Backbone will:• Extend from west coast to
eastern edge of Rocky Mountains, and from Alaska to Mexico (with international collaboration).
• Consist of ~100 continuous GPS receivers at 200 km spacing.
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GPS Backbone;The Big Picture
The Backbone will:• Extend from west coast to
eastern edge of Rocky Mountains, and from Alaska to Mexico (with international collaboration).
• Consist of ~100 continuous GPS receivers at 200 km spacing.
• Provide a synoptic view of North American plate boundary deformation.
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PBO Deployment Plan for Magmatic Systems
• What are the dynamics and kinematics of magma rise, inrusion, and eruption?
• How do the temporal and spatial scales of deformation vary with eruptive style and magma type?
• Can the deformation that leads to an eruption be characterized?
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The San Andreas Fault System – A Natural Laboratory for Studying Earthquake Physics
• What determines the sequencing of seismic events?
• How do earthquakes nucleate?
GPS Strainmeters
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SAFODSan Andreas Fault Observatory at Depth
A comprehensive series of experiments aimed at:
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SAFODSan Andreas Fault Observatory at Depth
A comprehensive series of experiments aimed at:
• Sampling fault zone materials and fluids
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SAFODSan Andreas Fault Observatory at Depth
A comprehensive series of experiments aimed at:
• Sampling fault zone materials and fluids
• Measuring a wide variety of physical properties
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SAFODSan Andreas Fault Observatory at Depth
A comprehensive series of experiments aimed at:
• Sampling fault zone materials and fluids
• Measuring a wide variety of physical properties
• Monitoring a creeping and seismically active fault zone at depth
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SAFODSan Andreas Fault Observatory at Depth
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SAFODSan Andreas Fault Observatory at Depth
• A 4-km-deep hole into the San Andreas fault zone
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SAFODSan Andreas Fault Observatory at Depth
• A 4-km-deep hole into the San Andreas fault zone
• Close to the hypocenter of the 1966 M~6 Parkfield earthquake
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SAFODSan Andreas Fault Observatory at Depth
• A 4-km-deep hole into the San Andreas fault zone
• Close to the hypocenter of the 1966 M~6 Parkfield earthquake
• Where the San Andreas slips through a combination of creep & small-to-moderate magnitude earthquakes
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1906 M 7.8
1966 M 6.0
1989 M 6.9
1857 M 8.0
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InSAR will enable:
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InSAR will enable:• Synoptic mapping of surface movements before, during
and after earthquakes and volcanic eruptions
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InSAR will enable:• Synoptic mapping of surface movements before, during
and after earthquakes and volcanic eruptions
• Imaging the time-evolution of active fault systems, providing unique insights into the mechanics of fault loading and earthquake rupture
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InSAR will enable:• Synoptic mapping of surface movements before, during
and after earthquakes and volcanic eruptions
• Imaging the time-evolution of active fault systems, providing unique insights into the mechanics of fault loading and earthquake rupture
• Mapping strain accumulation across broad tectonic regions to identify zones of strain concentration, and to improve our understanding of crust and upper mantle rheology
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InSAR will enable:• Synoptic mapping of surface movements before, during
and after earthquakes and volcanic eruptions
• Imaging the time-evolution of active fault systems, providing unique insights into the mechanics of fault loading and earthquake rupture
• Mapping strain accumulation across broad tectonic regions to identify zones of strain concentration, and to improve our understanding of crust and upper mantle rheology
• Imaging the deformation of volcanic edifices to infer the nature of source zones and the dynamics of magma migration
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InSAR will enable:• Synoptic mapping of surface movements before, during
and after earthquakes and volcanic eruptions
• Imaging the time-evolution of active fault systems, providing unique insights into the mechanics of fault loading and earthquake rupture
• Mapping strain accumulation across broad tectonic regions to identify zones of strain concentration, and to improve our understanding of crust and upper mantle rheology
• Imaging the deformation of volcanic edifices to infer the nature of source zones and the dynamics of magma migration
• All-weather mapping of surface change associated with a wide range of natural hazards
![Page 53: A New View of Earthcais.gsi.go.jp/UJNR/UJNR4P/Whitcomb-NSF.pdf · San Andreas Fault Observatory at Depth • A 4-km-deep hole into the San Andreas fault zone • Close to the hypocenter](https://reader036.vdocuments.mx/reader036/viewer/2022070713/5ed3229cf1dee620f72fd981/html5/thumbnails/53.jpg)
InSAR Image of the Hector Mine Earthquake
• A satellite-generated Interferometric Synthetic Aperture Radar (InSAR) image of the 1999 Hector Mine earthquake.
• Shows the displacement field in the direction of radar imaging.
• Each fringe (e.g., from red to red) corresponds to a few centimeters of displacement.
![Page 54: A New View of Earthcais.gsi.go.jp/UJNR/UJNR4P/Whitcomb-NSF.pdf · San Andreas Fault Observatory at Depth • A 4-km-deep hole into the San Andreas fault zone • Close to the hypocenter](https://reader036.vdocuments.mx/reader036/viewer/2022070713/5ed3229cf1dee620f72fd981/html5/thumbnails/54.jpg)
Uplift of the ground surface near the Three Sistersvolcanoes, central Oregon Cascade Range
Occurred between 1996 and 2000; covers an area of 15 to 20 kmin diameter with a maximum uplift at its center of about 10 cm
![Page 55: A New View of Earthcais.gsi.go.jp/UJNR/UJNR4P/Whitcomb-NSF.pdf · San Andreas Fault Observatory at Depth • A 4-km-deep hole into the San Andreas fault zone • Close to the hypocenter](https://reader036.vdocuments.mx/reader036/viewer/2022070713/5ed3229cf1dee620f72fd981/html5/thumbnails/55.jpg)
EarthScope Integration
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EarthScope Integration• Structural Representation
p
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EarthScope Integration• Structural Representation
p
• Structural Geology Field Investigations
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EarthScope Integration• Structural Representation
p
• Structural Geology Field Investigations• Seismic Imaging (USArray)
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EarthScope Integration• Structural Representation
p
• Structural Geology Field Investigations• Seismic Imaging (USArray)• Gravity and Electromagnetic Surveying
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EarthScope Integration• Structural Representation
p
• Structural Geology Field Investigations• Seismic Imaging (USArray)• Gravity and Electromagnetic Surveying
• Kinematic (Deformational) Representation
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EarthScope Integration• Structural Representation
p
• Structural Geology Field Investigations• Seismic Imaging (USArray)• Gravity and Electromagnetic Surveying
• Kinematic (Deformational) Representation• Geologic Structures
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EarthScope Integration• Structural Representation
p
• Structural Geology Field Investigations• Seismic Imaging (USArray)• Gravity and Electromagnetic Surveying
• Kinematic (Deformational) Representation• Geologic Structures• Geochronology
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EarthScope Integration• Structural Representation
p
• Structural Geology Field Investigations• Seismic Imaging (USArray)• Gravity and Electromagnetic Surveying
• Kinematic (Deformational) Representation• Geologic Structures• Geochronology• Geodesy (PBO and InSAR)
![Page 64: A New View of Earthcais.gsi.go.jp/UJNR/UJNR4P/Whitcomb-NSF.pdf · San Andreas Fault Observatory at Depth • A 4-km-deep hole into the San Andreas fault zone • Close to the hypocenter](https://reader036.vdocuments.mx/reader036/viewer/2022070713/5ed3229cf1dee620f72fd981/html5/thumbnails/64.jpg)
EarthScope Integration• Structural Representation
p
• Structural Geology Field Investigations• Seismic Imaging (USArray)• Gravity and Electromagnetic Surveying
• Kinematic (Deformational) Representation• Geologic Structures• Geochronology• Geodesy (PBO and InSAR)• Earthquake Seismology (ANSS)
![Page 65: A New View of Earthcais.gsi.go.jp/UJNR/UJNR4P/Whitcomb-NSF.pdf · San Andreas Fault Observatory at Depth • A 4-km-deep hole into the San Andreas fault zone • Close to the hypocenter](https://reader036.vdocuments.mx/reader036/viewer/2022070713/5ed3229cf1dee620f72fd981/html5/thumbnails/65.jpg)
EarthScope Integration• Structural Representation
p
• Structural Geology Field Investigations• Seismic Imaging (USArray)• Gravity and Electromagnetic Surveying
• Kinematic (Deformational) Representation• Geologic Structures• Geochronology• Geodesy (PBO and InSAR)• Earthquake Seismology (ANSS)
• Behavioral (Material Properties) Representation
![Page 66: A New View of Earthcais.gsi.go.jp/UJNR/UJNR4P/Whitcomb-NSF.pdf · San Andreas Fault Observatory at Depth • A 4-km-deep hole into the San Andreas fault zone • Close to the hypocenter](https://reader036.vdocuments.mx/reader036/viewer/2022070713/5ed3229cf1dee620f72fd981/html5/thumbnails/66.jpg)
EarthScope Integration• Structural Representation
p
• Structural Geology Field Investigations• Seismic Imaging (USArray)• Gravity and Electromagnetic Surveying
• Kinematic (Deformational) Representation• Geologic Structures• Geochronology• Geodesy (PBO and InSAR)• Earthquake Seismology (ANSS)
• Behavioral (Material Properties) Representation• Subsurface Sampling (SAFOD)
![Page 67: A New View of Earthcais.gsi.go.jp/UJNR/UJNR4P/Whitcomb-NSF.pdf · San Andreas Fault Observatory at Depth • A 4-km-deep hole into the San Andreas fault zone • Close to the hypocenter](https://reader036.vdocuments.mx/reader036/viewer/2022070713/5ed3229cf1dee620f72fd981/html5/thumbnails/67.jpg)
EarthScope Integration• Structural Representation
p
• Structural Geology Field Investigations• Seismic Imaging (USArray)• Gravity and Electromagnetic Surveying
• Kinematic (Deformational) Representation• Geologic Structures• Geochronology• Geodesy (PBO and InSAR)• Earthquake Seismology (ANSS)
• Behavioral (Material Properties) Representation• Subsurface Sampling (SAFOD)• Seismic Wave Propagation
![Page 68: A New View of Earthcais.gsi.go.jp/UJNR/UJNR4P/Whitcomb-NSF.pdf · San Andreas Fault Observatory at Depth • A 4-km-deep hole into the San Andreas fault zone • Close to the hypocenter](https://reader036.vdocuments.mx/reader036/viewer/2022070713/5ed3229cf1dee620f72fd981/html5/thumbnails/68.jpg)
EarthScope Integration• Structural Representation
p
• Structural Geology Field Investigations• Seismic Imaging (USArray)• Gravity and Electromagnetic Surveying
• Kinematic (Deformational) Representation• Geologic Structures• Geochronology• Geodesy (PBO and InSAR)• Earthquake Seismology (ANSS)
• Behavioral (Material Properties) Representation• Subsurface Sampling (SAFOD)• Seismic Wave Propagation
• Structures Deformation Material properties Process (community models) Prediction
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EarthScope Integration• Structural Representation
p
• Structural Geology Field Investigations• Seismic Imaging (USArray)• Gravity and Electromagnetic Surveying
• Kinematic (Deformational) Representation• Geologic Structures• Geochronology• Geodesy (PBO and InSAR)• Earthquake Seismology (ANSS)
• Behavioral (Material Properties) Representation• Subsurface Sampling (SAFOD)• Seismic Wave Propagation
• Structures Deformation Material properties Process (community models) Prediction
![Page 70: A New View of Earthcais.gsi.go.jp/UJNR/UJNR4P/Whitcomb-NSF.pdf · San Andreas Fault Observatory at Depth • A 4-km-deep hole into the San Andreas fault zone • Close to the hypocenter](https://reader036.vdocuments.mx/reader036/viewer/2022070713/5ed3229cf1dee620f72fd981/html5/thumbnails/70.jpg)
EarthScope Integration• Structural Representation
p
• Structural Geology Field Investigations• Seismic Imaging (USArray)• Gravity and Electromagnetic Surveying
• Kinematic (Deformational) Representation• Geologic Structures• Geochronology• Geodesy (PBO and InSAR)• Earthquake Seismology (ANSS)
• Behavioral (Material Properties) Representation• Subsurface Sampling (SAFOD)• Seismic Wave Propagation
• Structures Deformation Material properties Process (community models) Prediction
![Page 71: A New View of Earthcais.gsi.go.jp/UJNR/UJNR4P/Whitcomb-NSF.pdf · San Andreas Fault Observatory at Depth • A 4-km-deep hole into the San Andreas fault zone • Close to the hypocenter](https://reader036.vdocuments.mx/reader036/viewer/2022070713/5ed3229cf1dee620f72fd981/html5/thumbnails/71.jpg)
EarthScope Integration• Structural Representation
p
• Structural Geology Field Investigations• Seismic Imaging (USArray)• Gravity and Electromagnetic Surveying
• Kinematic (Deformational) Representation• Geologic Structures• Geochronology• Geodesy (PBO and InSAR)• Earthquake Seismology (ANSS)
• Behavioral (Material Properties) Representation• Subsurface Sampling (SAFOD)• Seismic Wave Propagation
• Structures Deformation Material properties Process (community models) Prediction
=
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EarthScope Integration• Structural Representation
p
• Structural Geology Field Investigations• Seismic Imaging (USArray)• Gravity and Electromagnetic Surveying
• Kinematic (Deformational) Representation• Geologic Structures• Geochronology• Geodesy (PBO and InSAR)• Earthquake Seismology (ANSS)
• Behavioral (Material Properties) Representation• Subsurface Sampling (SAFOD)• Seismic Wave Propagation
• Structures Deformation Material properties Process (community models) Prediction
=
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SeismicHazardModel
SeismicityPaleoseismology Local site effects
Geologic structure
Faults
Stresstransfer
Crustal motion Crustal deformation Velocity structure
Rupturedynamics
Seismic Hazard Model Ingredients
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EarthScope as an NSF/EAR Facility• Goal
– Data in support of EAR science goals• Science directed• Community driven• Open access
• Product– Data
• Science-appropriate
• Cutting edge technology
• Free and open access
• Quality control
• Management Plan– Oversight and governance
• Coordination and balance
– Equipment Acquisition• Specification • Procurement • Inventory and control
– Operations• Operation and
maintenance• Data management• Technology R&D
– Partnerships
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EarthScope as an NSF/EARScience Program
• Goal– Fundamental
advances in geoscience
• Science driven
• Research based
• Peer reviewed
• Product– Scientific
results
• Management Plan– NSF open program
announcement• Individual research grants• Collaborative research grants
– Focused research• External research direction• Integrative research centers
– Strong partnerships• USGS, NASA, DOE• State surveys• International
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NSF USGS NASA DOE
Interagency Coordinating Group
EarthScopeCoordinatingCommittee
Operations &Science
Coordination &Planning
EarthScopeSAFOD
PBO
USArray
InSAR
Operations Coordination
Oversight Review &Community InputFacility
Funding&
FiscalControl
CommunityScienceCouncil
EarthScope Management Plan