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      THE SALTON SEA SCIENTIFIC DRILLING PROJECT

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      Journal of Geophysical Research: Solid Earth
      American Geophysical Union (AGU)

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          Heat flow in southernmost California and the origin of the Salton Trough

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            Crustal Spreading in Southern California: The Imperial Valley and the Gulf of California formed by the rifting apart of a continental plate.

            The current excitement among geologists and geophysicists stemming from the "new global tectonics" has led to a widespread, speculative reinterpretation of continental geology. The Gulf of California and its continuation into the Imperial Valley provide an excellent opportunity for studying the border zone between the North American and Pacific plates, and an interface of continental and oceanic tectonics. The Salton trough, the landward extension of the gulf, is a broad structural depression, comparable in size with the deeper marine basins of the southern part of the gulf, but here partially filled with sediments deposited by the Colorado River.
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              Active Metamorphism of Upper Cenozoic Sediments in the Salton Sea Geothermal Field and the Salton Trough, Southeastern California

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                Author and article information

                Journal
                Journal of Geophysical Research: Solid Earth
                J. Geophys. Res.
                American Geophysical Union (AGU)
                01480227
                November 10 1988
                November 10 1988
                : 93
                : B11
                : 12953-12968
                Article
                10.1029/JB093iB11p12953
                d16d53b4-c28a-4595-b886-87c27919703f
                © 1988

                http://doi.wiley.com/10.1002/tdm_license_1.1

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