An examination of folded Eocene turbidites,
Douglas County, southwestern Oregon

By
Carol Stack

A thesis submitted in partial fulfillment of the
requirements for the degree of

MASTER OF SCIENCE
in
GEOLOGY

Portland State University
1998

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Table of Contents

Abstract
Dedication
Acknowledgments
Table of Contents
List of Tables
List of Figures
Introduction
Regional Geologic Setting
Geographic Location
Regional Physiography and Geology
Stratigraphy
Siletz River Volcanics
Umpqua Group
Tyee Formation
Structure
Folds
Faults
Tectonic History
Geologic Setting of the Study Area
Methods
Outcrop Observations
Bedding
Fractures
Fold Form
Section I
Bed Form
Fold Form
Fractures
Section II
Section III
Sections IV and V
Section VI
Discussion
Outcrop Fold Package
Folding Mechanism
Fold Form
Asymmetry
Unit Thickness
Outcrop Setting
Conclusion
Bibliography
Appendix A
Appendix B
Appendix C

List of Tables

Table 1. A summary by section of bed thickness and sandstone to shale ratios.
Table 2. Summary of fold form by section (Figure 8).
Table 3. A summary of bed thickness and sandstone to shale ratios by folding unit.
Table 4. Results of applying the model relating multilayer thickness, number of structural units, and viscosity contrast in a multilayer with free slip.

List of Figures

Figure 1. Location of study area.
Figure 2. Location of study area in Sutherlin subbasin.
Figure 3. Stratigraphic nomenclature for the region containing the study area.
Figure 4. Schematic fence diagram of wells and measured sections surrounding the study area (after Ryu and others, 1992).
Figure 5. Paleogeographic reconstruction of the Pacific Northwest at 55±5 Ma (after Heller and others, 1987, Fig. 5).
Figure 6. Cross-section of Sutherlin subbasin through study area.
Figure 7. Estimated thickness of Umpqua Group units in the study area.
Figure 8. N-S cross-section of folds with axial survey points, and map view of axial survey points.
Figure 9. Schematic showing thickness of measured fold limbs from north to south.
Figure 10. Bed deformed into low-amplitude sine wave with wavelength of about two meters.
Figure 11. Duplex-like feature.
Figure 12. Asymmetry of folds defined.
Figure 13. Section I folds.
Figure 14. Folds 3 and 4 of Section I.
Figure 15. Envelopes of a bed traced through the folds of Section I.
Figure 16. Bedding thrusts and sub-horizontal faults in the concentric-like fold of Section I.
Figure 17. Section I folds and faults not at low angle to bedding.
Figure 18. Section II and Section III folds.
Figure 19. Idealized kink form imposed on schematic drawing of kink-like fold.
Figure 20. Fractures and contacts in kink-like fold.
Figure 21. Tan siltstone and associated calcareous nodule at base of kink-like fold of Section III.
Figure 22. Thrust fault zone immediately north of (stratigraphically below) the kink-like fold.
Figure 23. Section IV and Section V folds.
Figure 24. Jointed hinge of fold 14 in Section IV.
Figure 25. Section VI asymmetric chevron-like folds.
Figure 26. Schematic folding of conjugate fault zones in layers of Section VI.
Figure 27. Anticlinal fold 21 in Section VI.
Figure 28. Duplication of layers in south anticline of Section VI.
Figure 29. Boudin layer in curve of drag fold in fold 21, Section VI.
Figure 30. Model of folding units in the study outcrop.
Figure 31. Theoretical multilayer folds.
Figure 32. Fold form of Section I.
Figure 33. Parameters for multilayer folding models.
Figure 34. Opposite sense of asymmetry of monoclinal kink and drag folds.
Figure 35. Sense of fold asymmetry for the outcrop setting in a thrust sheet.
Figure 36. Chart of layer to average media viscosity.
Figure 37. Chart of initial thickness as a function of layer to average media viscosity contrast.
Figure 38. Relation of the wavelength to thickness ratio in rigid and soft media, for various ratios of media to normal viscosity of the multilayer.
Figure 39. Order of deformation.

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