Joint Orientations and Near‐Surface Structure and Stratigraphy in the Vicinity of Large Sediment Boils Erupted During a Major Earthquake

Author(s):  
R. D. Bolger ◽  
J. R. Pelton ◽  
L. M. Liberty ◽  
C. J. Waag
2015 ◽  
Author(s):  
Tongju Gong* ◽  
Miao Liu ◽  
Yiming Wang ◽  
Zhiwei Zhu ◽  
Baoqing Zhang

2018 ◽  
Vol 38 (4) ◽  
pp. 851-870 ◽  
Author(s):  
Marianne Vandenbossche ◽  
Gesine Gunkel-Grabole ◽  
Anja Car ◽  
Laetitia Bernard ◽  
Patrick Rupper ◽  
...  

2001 ◽  
Vol 39 (16) ◽  
pp. 1824-1838 ◽  
Author(s):  
Mahendra Dabral ◽  
Xinyun Xia ◽  
W. W. Gerberich ◽  
L. F. Francis ◽  
L. E. Scriven

1974 ◽  
Vol 12 (3) ◽  
pp. 291 ◽  
Author(s):  
Michael R. Cooper ◽  
Robert L. Kovach ◽  
Joel S. Watkins

1971 ◽  
Vol 8 (8) ◽  
pp. 961-966 ◽  
Author(s):  
F. W. Jones

Electromagnetic induction in three two-dimensional models of conductors with two regions of different conductivity is considered. Solutions are obtained for both the H-polarization and E-polarization cases by a numerical method. Apparent resistivity as a function of period is plotted for various locations relative to the surface contact. For the H-polarization case, the apparent resistivity values calculated for points near the surface contact are affected by the varying surface charge on the interface between the regions, and a value different from the expected value is obtained. In the E-polarization case the apparent resistivity curves exhibit a "dip" characteristic when the apparent resistivity is calculated for surface points near a shelf or step structure. In both cases the value of apparent resistivity calculated at or near surface contacts between different conducting regions depends greatly on the sub-surface structure.


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