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Joseph, Devorah, Taylor, Brian, Shor, Alexander N. (1992) New sidescan sonar and gravity evidence that the Nova-Canton Trough is a fracture zone. Geology, 20 (5) 435 doi:10.1130/0091-7613(1992)020<0435:nssage>2.3.co;2

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Reference TypeJournal (article/letter/editorial)
TitleNew sidescan sonar and gravity evidence that the Nova-Canton Trough is a fracture zone
JournalGeology
AuthorsJoseph, DevorahAuthor
Taylor, BrianAuthor
Shor, Alexander N.Author
Year1992Volume20
Issue5
PublisherGeological Society of America
DOIdoi:10.1130/0091-7613(1992)020<0435:nssage>2.3.co;2Search in ResearchGate
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Mindat Ref. ID135026Long-form Identifiermindat:1:5:135026:9
GUID0
Full ReferenceJoseph, Devorah, Taylor, Brian, Shor, Alexander N. (1992) New sidescan sonar and gravity evidence that the Nova-Canton Trough is a fracture zone. Geology, 20 (5) 435 doi:10.1130/0091-7613(1992)020<0435:nssage>2.3.co;2
Plain TextJoseph, Devorah, Taylor, Brian, Shor, Alexander N. (1992) New sidescan sonar and gravity evidence that the Nova-Canton Trough is a fracture zone. Geology, 20 (5) 435 doi:10.1130/0091-7613(1992)0202.3.co;2
In(1992) Geology Vol. 20 (5) Geological Society of America

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Montgomery, David R., Jones, David L. (1992) How wide is the Calaveras fault zone—Evidence for distributed shear along a major fault in central California. Geology, 20 (1) 55 doi:10.1130/0091-7613(1992)020<0055:hwitcf>2.3.co;2
 
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