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Depositional History Of The Eocene Chumstick Formation: Implications Of Tectonic Partitioning For The History Of The Leavenworth And Entiat-Eagle Creek Fault Systems, Washington - Reply, James E. Evans
School of Earth, Environment and Society Faculty Publications
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Depositional History Of The Eocene Chumstick Formation - Implications Of Tectonic Partitioning For The History Of The Leavenworth And Entiat-Eagle Creek Fault Systems, Washington, James E. Evans
School of Earth, Environment and Society Faculty Publications
The Chumstick basin opened as an extensional half-graben prior to 51 Ma, and was subsequently modified by two episodes of tectonic partitioning of drainage prior to basin deformation. Initially, westward flowing fluvial systems formed a unified depositional system with the Swauk basin. Tectonic partitioning of drainage at 51-49 Ma and at 44-42 Ma was controlled by localized uplift on the Leavenworth (LFZ), Eagle Creek (ECFZ), and Entiat (EFZ) fault zones and led in each instance to the truncation of regional depositional systems, modification and reversal of paleoflow, and internal drainage. Relief on the LFZ at 51-49 Ma may be the …