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PALEOMAGNETISM OF LATE MESOZOIC ROCKS IN NORTHERN CALIFORNIA: STRUCTURAL SIGNIFICANCE

机译:加利福尼亚北部晚中生代岩石的古地磁:结构意义

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Directions of natural remanent magnetization have been determined at ten sites in the late Jurassic Guadalupe igneous complex and Bucks Lake batholith in the western Sierra Nevada, California. Pale magnetic pole positions from these two put-ons agree with one another and with other late Jurassic and Cretaceous poles from North America. These put-ons, which are located 150 miles apart, have therefore been little affected by later tectonic events. The pole positions are preliminary only, and may be subject to slight modification after removal of secondary components of NRM by a.c. demagnetization of all specimens. One or more geomagnetic field reversals appear to be recorded in the Bucks Lake batholith, but possibly the NRM in titan hematite in both the put-ons has been self-reversed.

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