Cenozoic tectonic and thermal history of the Nenana basin, central interior Alaska: new constraints from seismic reflection data, fracture history and apatite fission-track analyses

The Nenana basin of interior Alaska forms a segment of the diffuse plate boundary between the Bering and North American plates and is located within a complex zone of crustal-scale strike-slip deformation that accommodates compressional stresses due to oblique plate convergence to the south. The basin is currently the focus of new oil and gas exploration. Integration of seismic reflection and well data, fracture data and apatite fission track analyses with regional data improves our understanding of the tectonic development of this continental strike-slip basin.The Nenana basin formed during the Late Paleocene as a 13-km-wide half-graben, affected by regional intraplate magmatism and localized crustal thinning across the Minto fault in south-central Alaska. The basin was uplifted and exhumed along this faulted margin in Early Eocene through to Late Oligocene time in response to oblique subduction along the southern Alaska margin. This event resulted in the removal of up to 1.5 km of Late Paleocene strata from the basin. Renewed rifting and subsidence during Early Miocene time widened the basin to the west resulting in deposition of Miocene nonmarine clastic rocks in reactivated and newly-formed extensional half-grabens. In Middle to Late Miocene time, left lateral strike-slip faulting was superimposed on this half-graben system, with rapid subsidence beginning in Pliocene time and continuing to the present-day. At present, the Nenana basin is in a zone of transtensional deformation that accommodates compressional stresses due to oblique plate convergence and allows tectonic subsidence by oblique-extension along major basin-bounding strike-slip faults.The accepted manuscript in pdf format is listed with the files at the bottom of this page. The presentation of the authors' names and (or) special characters in the title of the manuscript may differ slightly between what is listed on this page and what is listed in the pdf file of the accepted manuscript; that in the pdf file of the accepted manuscript is what was submitted by the author