Language:
English
繁體中文
Help
Login
Back
Switch To:
Labeled
|
MARC Mode
|
ISBD
Enhanced Surface Imaging of Crustal ...
~
Dimitrova, Lada L.
Enhanced Surface Imaging of Crustal Deformation = Obtaining Tectonic Force Fields Using GPS Data /
Record Type:
Language materials, printed : Monograph/item
Title/Author:
Enhanced Surface Imaging of Crustal Deformation/ by A. John Haines, Lada L. Dimitrova, Laura M. Wallace, Charles A. Williams.
Reminder of title:
Obtaining Tectonic Force Fields Using GPS Data /
Author:
Haines, A. John.
other author:
Dimitrova, Lada L.
Description:
X, 99 p. 50 illus., 37 illus. in color.online resource. :
Contained By:
Springer Nature eBook
Subject:
Geophysics. -
Online resource:
https://doi.org/10.1007/978-3-319-21578-5
ISBN:
9783319215785
Enhanced Surface Imaging of Crustal Deformation = Obtaining Tectonic Force Fields Using GPS Data /
Haines, A. John.
Enhanced Surface Imaging of Crustal Deformation
Obtaining Tectonic Force Fields Using GPS Data /[electronic resource] :by A. John Haines, Lada L. Dimitrova, Laura M. Wallace, Charles A. Williams. - 1st ed. 2015. - X, 99 p. 50 illus., 37 illus. in color.online resource. - SpringerBriefs in Earth Sciences,2191-5369. - SpringerBriefs in Earth Sciences,.
1. Introduction.- 2. Introduction to the Vertical Derivatives of Horizontal Stress (VDoHS) Rates -- 3. Inversion Methodology -- 4. 1-Dimensional Synthetic Examples -- 5. Application to Central South Island, New Zealand -- 6. 2-Dimensional Examples -- 7. Concluding Remarks.
This book takes an in depth look at a novel methodology for analyzing Global Positioning System (GPS) data to obtain the highest possible resolution surface imaging of tectonic deformation sources without prescribing the nature of either the sources or the subsurface medium. GPS methods are widely used to track the surface expression of crustal deformation at tectonic plate boundaries, and are typically expressed in terms of velocity fields or strain rate fields. Vertical derivatives of horizontal stress (VDoHS) rates at the Earth’s surface can also be derived from GPS velocities, and VDoHS rates provide much higher resolution information about subsurface deformation sources than velocities or strain rates. In particular, VDoHS rates allow for high precision estimates of fault dips, slip rates and locking depths, as well as objective characterization of previously unknown (or hidden) tectonic deformation zones.
ISBN: 9783319215785
Standard No.: 10.1007/978-3-319-21578-5doiSubjects--Topical Terms:
686174
Geophysics.
LC Class. No.: QC801-809
Dewey Class. No.: 550
Enhanced Surface Imaging of Crustal Deformation = Obtaining Tectonic Force Fields Using GPS Data /
LDR
:02709nam a22004095i 4500
001
967509
003
DE-He213
005
20200706084328.0
007
cr nn 008mamaa
008
201211s2015 gw | s |||| 0|eng d
020
$a
9783319215785
$9
978-3-319-21578-5
024
7
$a
10.1007/978-3-319-21578-5
$2
doi
035
$a
978-3-319-21578-5
050
4
$a
QC801-809
072
7
$a
PHVG
$2
bicssc
072
7
$a
SCI032000
$2
bisacsh
072
7
$a
PHVG
$2
thema
082
0 4
$a
550
$2
23
082
0 4
$a
526.1
$2
23
100
1
$a
Haines, A. John.
$4
aut
$4
http://id.loc.gov/vocabulary/relators/aut
$3
1067846
245
1 0
$a
Enhanced Surface Imaging of Crustal Deformation
$h
[electronic resource] :
$b
Obtaining Tectonic Force Fields Using GPS Data /
$c
by A. John Haines, Lada L. Dimitrova, Laura M. Wallace, Charles A. Williams.
250
$a
1st ed. 2015.
264
1
$a
Cham :
$b
Springer International Publishing :
$b
Imprint: Springer,
$c
2015.
300
$a
X, 99 p. 50 illus., 37 illus. in color.
$b
online resource.
336
$a
text
$b
txt
$2
rdacontent
337
$a
computer
$b
c
$2
rdamedia
338
$a
online resource
$b
cr
$2
rdacarrier
347
$a
text file
$b
PDF
$2
rda
490
1
$a
SpringerBriefs in Earth Sciences,
$x
2191-5369
505
0
$a
1. Introduction.- 2. Introduction to the Vertical Derivatives of Horizontal Stress (VDoHS) Rates -- 3. Inversion Methodology -- 4. 1-Dimensional Synthetic Examples -- 5. Application to Central South Island, New Zealand -- 6. 2-Dimensional Examples -- 7. Concluding Remarks.
520
$a
This book takes an in depth look at a novel methodology for analyzing Global Positioning System (GPS) data to obtain the highest possible resolution surface imaging of tectonic deformation sources without prescribing the nature of either the sources or the subsurface medium. GPS methods are widely used to track the surface expression of crustal deformation at tectonic plate boundaries, and are typically expressed in terms of velocity fields or strain rate fields. Vertical derivatives of horizontal stress (VDoHS) rates at the Earth’s surface can also be derived from GPS velocities, and VDoHS rates provide much higher resolution information about subsurface deformation sources than velocities or strain rates. In particular, VDoHS rates allow for high precision estimates of fault dips, slip rates and locking depths, as well as objective characterization of previously unknown (or hidden) tectonic deformation zones.
650
0
$a
Geophysics.
$3
686174
650
0
$a
Natural disasters.
$3
555029
650
0
$a
Mathematical physics.
$3
527831
650
1 4
$a
Geophysics/Geodesy.
$3
668510
650
2 4
$a
Natural Hazards.
$3
784090
650
2 4
$a
Mathematical Applications in the Physical Sciences.
$3
786649
700
1
$a
Dimitrova, Lada L.
$e
author.
$4
aut
$4
http://id.loc.gov/vocabulary/relators/aut
$3
1263167
700
1
$a
Wallace, Laura M.
$e
author.
$4
aut
$4
http://id.loc.gov/vocabulary/relators/aut
$3
1263168
700
1
$a
Williams, Charles A.
$e
author.
$4
aut
$4
http://id.loc.gov/vocabulary/relators/aut
$3
1263169
710
2
$a
SpringerLink (Online service)
$3
593884
773
0
$t
Springer Nature eBook
776
0 8
$i
Printed edition:
$z
9783319215778
776
0 8
$i
Printed edition:
$z
9783319215792
830
0
$a
SpringerBriefs in Earth Sciences,
$x
2191-5369
$3
1253546
856
4 0
$u
https://doi.org/10.1007/978-3-319-21578-5
912
$a
ZDB-2-EES
912
$a
ZDB-2-SXEE
950
$a
Earth and Environmental Science (SpringerNature-11646)
950
$a
Earth and Environmental Science (R0) (SpringerNature-43711)
based on 0 review(s)
Multimedia
Reviews
Add a review
and share your thoughts with other readers
Export
pickup library
Processing
...
Change password
Login