Reorientation of remanent magnetism during tectonic fabric development: an example from the Waynesboro Formation, Pennsylvania, U.S.A.

Autor: Vetter, James R., Kodama, Kenneth P., Goldstein, Arthur
Zdroj: Tectonophysics; January 1989, Vol. 165 Issue: 1 p29-39, 11p
Abstrakt: A paleomagnetic study of the late Early-early Middle Cambrian Waynesboro Formation in south, central Pennsylvania reveals a pre-folding magnetization which is close to the expected Cambrian field at three sites, while other site mean directions are rotated by as much as 82° from the expected Cambrian field. These results are based on detailed thermal demagnetization analysis of 84 red siltstone and sandstone samples from nine sites collected over a 163 km 2area. Local faulting, fault block rotation, and remanence acquisition during rapid apparent polar wander do not appear to be responsible for the observed remanence deviations.
Databáze: Supplemental Index