Our model correlates the PST to the normal-polarity zone just below the C6-C5E boundary (18.748 Ma) of the astronomically tuned Geomagnetic Polarity Time Scale.
After emplacement of the Peach Spring Tuff at Alvord Mountain and the Cady Mountains, the southern part of the Northeast Mojave Domain (between Cady and Coyote Lake faults) underwent clockwise rotation of 30°–55°.
Our approach is to use the high throughput of the u-channel SRM to: Materials for study come from a wide range of sources, including international science programs such as the Integrated Ocean Drilling Program and the International Continental Drilling Program, PI driven field programs and retrospective research on the large core collection available at the OSU-Marine Geology Repository. After an exciting week of getting settled into my apartment, I joined graduate students, REU students, our P. by Brendan Reilly | Jun 8, 2017 The OSU P-mag group is getting bigger!
by Ben Freiberg | Aug 16, 2017 Brendan arrived around mid-afternoon in academic fashion, behind the wheel of a Subaru Forrester. We welcome Ben Freiberg, from Skidmore College, and Nick Lavoie, from North Carolina State University, who have made it just in time for Mo Walczak’s research cruise off the Oregon Margin next week.
81–3090.) So how do scientists use the earth's wandering magnetic field to date archaeological sites? Certain clays have a naturally high iron (Fe) content.