scholarly journals Magnetic field monitoring of tectonic stress in Southern California

1981 ◽  
Author(s):  
Floyd J. Williams
Keyword(s):  
Magnetic Field ◽  
Southern California ◽  
Tectonic Stress ◽  
Field Monitoring

scholarly journals Characterization and correction of eddy-current artifacts in unipolar and bipolar diffusion sequences using magnetic field monitoring

2014 ◽  
Vol 244 ◽  
pp. 74-84 ◽  
Author(s):  
Rachel W. Chan ◽  
Constantin von Deuster ◽  
Daniel Giese ◽  
Christian T. Stoeck ◽  
Jack Harmer ◽  
...  
Keyword(s):  
Magnetic Field ◽  
Eddy Current ◽  
Field Monitoring

Long term magnetic field monitoring near power lines

1997 ◽  
Vol 12 (2) ◽  
pp. 922-927 ◽  
Author(s):  
P.S. Wong ◽  
M.A. Janoska ◽  
C. Light ◽  
R.W. McCourt
Keyword(s):  
Magnetic Field ◽  
Field Monitoring ◽  
Power Lines

Continuous Magnetic Field Monitoring Using Rapid Re-Excitation of NMR Probe Sets

2016 ◽  
Vol 35 (6) ◽  
pp. 1452-1462 ◽  
Author(s):  
Benjamin E. Dietrich ◽  
David O. Brunner ◽  
Bertram J. Wilm ◽  
Christoph Barmet ◽  
Klaas P. Pruessmann
Keyword(s):  
Magnetic Field ◽  
Field Monitoring

scholarly journals A transmit/receive system for magnetic field monitoring of in vivo MRI

2009 ◽  
Vol 62 (1) ◽  
pp. 269-276 ◽  
Author(s):  
Christoph Barmet ◽  
Nicola De Zanche ◽  
Bertram J. Wilm ◽  
Klaas P. Pruessmann
Keyword(s):  
Magnetic Field ◽  
Field Monitoring ◽  
Receive System

scholarly journals Regional tectonic stress near the San Andreas fault in central and southern California

2021 ◽  
Author(s):  
John Townend ◽  
M Zoback
Keyword(s):  
Compressive Stress ◽  
San Francisco ◽  
Southern California ◽  
San Andreas Fault ◽  
Horizontal Stress ◽  
Tectonic Stress ◽  
Bay Area ◽  
San Andreas ◽  
Regional Tectonic ◽  
Horizontal Compressive Stress

Throughout central and southern California, a uniform NNE-SSW direction of maximum horizontal compressive stress is observed that is remarkably consistent with the superposition of stresses arising from lateral variations in lithospheric buoyancy in the western United States, and farfield Pacific-North America plate interaction. In central California, the axis of maximum horizontal compressive stress lies at a high angle to the San Andreas fault (SAF). Despite relatively few observations near (±10 km) the fault, observations in the greater San Francisco Bay area indicate an angle of as much as 85°, implying extremely low fault strength. In southern California, observations of stress orientations near the SAF are rotated slightly counter-clockwise with respect to the regional field. Nevertheless, we observe an approximately constant angle between the SAF and the maximum horizontal stress direction of 68 ± 7° along ∼400 km of the fault, indicating that the SAF has moderately low frictional strength in southern California. Copyright 2004 by the American Geophysical Union.

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