Catalina Schist
The Catalina Schist is a
Channel Islands of California
.
It formed during the Cretaceous Period of the Mesozoic Era.
Geology
The Catalina Schist is broadly correlated with the
Franciscan Complex, a similar metamorphic complex formed along the California margin.[1]
Both of these units record
Farallon plate beneath North America during the Mesozoic Era. The Catalina Schist is differentiated from the Franciscan primarily in the style of mélange
formed during subduction.
In the Los Angeles Harbor Region, Catalina Schist is associated with the Wilmington Oil Field.
See also
References
- ^ Rowland, Stephan M., Geology of Santa Catalina Island, California Geology, 1984 "Archived copy" (PDF). Archived from the original (PDF) on 2012-10-29. Retrieved 2011-10-30.
{{cite web}}: CS1 maint: archived copy as title (link)
33°24′14″N 118°22′41″W / 33.404°N 118.378°W
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