Early Cretaceous uplift and erosion of the northern Appalachian Basin, New York, based on apatite fission track analysis

Details Early Cretaceous uplift and erosion of the northern Appalachian Basin, New York, based on apatite fission track analysis Early Cretaceous uplift and erosion of the northern Appalachian Basin, New York, based on apatite fission track analysis

May 1989

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1989e%26psl..93...35m&link_type=abstract

Earth and Planetary Science Letters, Volume 93, Issue 1, p. 35-49.

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Scientific paper

The thermal history of outcropping Devonian sediments of the northern Appalachian Basin, New York, has been investigated using fission track analysis of detrital apatites from 57 sandstone samples. Based on lengths and apparent age measurements using fission tracks in apatite it is concluded that Lower Devonian sediments presently at the surface in the Catskill region were cooled rapidly from temperatures higher than about 110°C during Early Cretaceous times (120-140 Ma ago). In the western part of New York (Wellsville-Buffalo) data from late Devonian sediments are consistent with cooling at the same time as that identified for the Catskill region but from lower temperatures, in the range of approximately 80-110°C, the maximum temperature these sediments experienced since deposition. For a pre-uplift paleogeothermal gradient of 25-35°C/km, the confined track length data indicates uplift and erosion of ~ 2-3 km for western New York and greater than ~ 3-4 km for the Catskill region, a differential uplift pattern which is consistent with the historical stratigraphic data from the region. This conclusion is at variance with earlier interpretations put forth by others.
Rapid broad scale uplift and erosion of the scale identified imply that large volumes of sediment could have been supplied from the northern Appalachian Basin during the Early Cretaceous. This timing for the dominant post-Devonian cooling phase in the basin is not accounted for by recent models of the tectonic evolution of the Appalachian Orogen but is compatible with the change from carbonate to siliciclastic deposition in the Atlantic coastal plain. It is suggested that this style of broad regional uplift without significant deformation is characteristic of a tectonic regime associated with, and subsequent to, continental rifting.
Apatite fission track analysis is shown to be a basic tool in providing fundamental limits for thermal history assessment in regional tectonic problems.
Sample collection and laboratory research done, in part, during I.R.D.'s visit to Rensselaer Polytechnic Institute in 1984. Manuscript preparation done, in part, during D.S.M.'s visit to University of Melbourne in 1988.

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