Year: 1991
Type: article
Abstract: The Upper Ordovician Trenton Group of New York State is one of a number of Appalachian limestones which yields paleomagnetic poles suggesting disturbance in the late Paleozoic. Calcite fractions dissolved from samples of the Trenton Limestone define a 238U‐206Pb age of 454±8 Ma (MSWD=12.8) in excellent agreement with 40Ar−39 Ar and U‐Pb ages for the deposition of the underlying Diecke Bentonite. This requires that the U‐Pb system in the calcite has been preserved since deposition and early diagenesis. If late Paleozoic remagnetization of this limestone was induced by fluids, these fluids did not interact with significant amounts of carbonate. The apparent robustness of the U‐Pb system, and the large spread in µ values (18.17–118.8), offers potential precision of ±1 Ma in determining the Paleozoic time scale.
Source: Geophysical Research Letters
DOI: 10.1029/91gl01278
Authors: Charles P. DeWolf, Alex N. Halliday
Institution: University of Michigan
Language: English
Subfield: Geophysics
Field: Earth and Planetary Sciences
Domain: Physical Sciences
Open Access status: bronze
OpenAlex ID: W2163666478