The electrical conductivity structure between the transitional (near SAFOD) and 
locked (SE of Cholame) segments of the San Andreas Fault, including the source 
region of non-volcanic tremors.

Becken, M.; Ritter, Oliver; Bedrosian, J.; Weckmann, Ute; Munoz, G.; Meqbel, Naser

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The electrical conductivity structure between the transitional (near SAFOD) and locked (SE of Cholame) segments of the San Andreas Fault, including the source region of non-volcanic tremors.

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Becken, M.
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Ritter, Oliver
2.2 Geophysical Deep Sounding, 2.0 Physics of the Earth, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Bedrosian, J.
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Weckmann, Ute
2.2 Geophysical Deep Sounding, 2.0 Physics of the Earth, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Munoz, G.
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Meqbel, Naser
2.2 Geophysical Deep Sounding, 2.0 Physics of the Earth, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

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Becken, M., Ritter, O., Bedrosian, J., Weckmann, U., Munoz, G., Meqbel, N. (2008): The electrical conductivity structure between the transitional (near SAFOD) and locked (SE of Cholame) segments of the San Andreas Fault, including the source region of non-volcanic tremors., SAFOD Mini-Workshop (Potsdam, Germany 2008).

https://gfzpublic.gfz-potsdam.de/pubman/item/item_237565

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