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- W2181718434 abstract "Summary The Tertiary Yukon Fold Complex is the onshore continuation of the arcuate Beaufort Foldbelt of the western Beaufort Basin (Lane and Dietrich, 1995). Offshore structures such as Adlartok in the Beaufort Foldbelt contain proven hydrocarbon reserves. The age progression of the Beaufort Foldbelt is constrained by biostratigraphy from wells penetrating the seismic sequences (e.g., Lane, 2004) and by seismically imaged unconformities (e.g., Dietrich et al., 1989). Onshore, deformed Paleocene outcrops together with examples of onshore-offshore structural continuity require that the adjacent onshore deformation has similar timing. However, the north Yukon Fold Complex extends southward as far as the Ogilvie Mountains where age constraints are more loosely defined (e.g., Dixon, 1992; Lane, 1998). This overview discusses the ages of uplift and cooling of the North Yukon Fold Complex based on published and unpublished apatite fission track (AFT) ages from across the region. Published AFT cooling ages document an early Eocene event coincident with the regionally dominant deformation offshore (O’Sullivan and Lane, 1997). Uplift magnitudes for the Yukon coastal plain determined from the apatite data are consistent with 5-7 km uplift estimates previously interpreted from well-based thermal maturity analyses (Majorowicz and Dietrich, 1989)." @default.
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- W2181718434 date "2011-01-01" @default.
- W2181718434 modified "2023-09-27" @default.
- W2181718434 title "Overview of the Tertiary Cooling-uplift History of Northernmost Yukon Adjacent to the Beaufort Basin, Based on Apatite Fission Track Studies" @default.
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