Abstract
We report paleomagnetic and rock magnetic data from sedimentary carbonates of the Appalachian Basin that have implications for the mechanism of widespread late Paleozoic remagnetization in this rock type. Sampling was accomplished mostly along two across-basin transects, one in Devonian carbonates of New York State and the other in Ordovician and Mississippian carbonates of Tennessee and Alabama. -from Authors
Original language | English (US) |
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Pages (from-to) | 10,429-10,443 |
Journal | Journal of Geophysical Research |
Volume | 94 |
Issue number | B8 |
DOIs | |
State | Published - 1989 |
Externally published | Yes |