UUnniivveerrssiittyy ooff SSoouutthh FFlloorriiddaa SScchhoollaarr CCoommmmoonnss Graduate Theses and Dissertations Graduate School 7-18-2003 RReellaattiivvee MMoottiioonn HHiissttoorryy ooff tthhee PPaacciifificc--NNaazzccaa ((FFaarraalllloonn)) PPllaatteess ssiinnccee 3300 MMiilllliioonn YYeeaarrss AAggoo Douglas T. Wilder University of South Florida Follow this and additional works at: https://scholarcommons.usf.edu/etd Part of the American Studies Commons SScchhoollaarr CCoommmmoonnss CCiittaattiioonn Wilder, Douglas T., "Relative Motion History of the Pacific-Nazca (Farallon) Plates since 30 Million Years Ago" (2003). Graduate Theses and Dissertations. https://scholarcommons.usf.edu/etd/1506 This Thesis is brought to you for free and open access by the Graduate School at Scholar Commons. It has been accepted for inclusion in Graduate Theses and Dissertations by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. RELATIVE MOTION HISTORY OF THE PACIFIC-NAZCA (FARALLON) PLATES SINCE 30 MILLION YEARS AGO by DOUGLAS T. WILDER A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science College of Marine Science University of South Florida Co-Major Professor: David F. Naar, Ph.D. Co-Major Professor: Sarah F. Tebbens, Ph.D. Sarah E. Kruse, Ph.D. Date of Approval: July 18, 2003 Keywords: marine geology and geophysics, tectonics, seafloor spreading, magnetic anomaly © Copyright 2003, Douglas T. Wilder Dedication Humbly, to Yvonne and Maeve who endured for me. Acknowledgments This work would not have been possible without the guidance, patience, dedication, support and enthusiasm provided throughout every phase of this research by my advisor Dr. David F. Naar. I am extremely grateful to him for providing me the opportunity to conduct this research and complete my degree. Special thanks also to Dr. Sarah F. Tebbens, my co-major professor, who provided invaluable assistance during the course of this study beginning with initial data acquisition from Lamont-Doherty and including revision of programs used for finite and stage pole calculations. Thanks also to Dr. Sarah E. Kruse, my third committee member, who was extremely helpful at several points during completion of this work and helped immensely in tightening up the text for the final draft. There are many others who provided help or otherwise offered support that contributed to the successful completion of this work. Ruoying He provided programming expertise in the early stages of the work. Doug Myhre committed a great deal of time rewriting the MagBath program in Java and was always there to troubleshoot a myriad of computing problems. Dr. Mark Hafen was instrumental in getting me acquainted with the labs and procedures of the department (now college). William Self offered sight-unseen mathematical assistance from somewhere in cyberspace. Special thanks also to the following for comments and scientific assistance: Dr. Steve Cande, Dr. Yasushi Harada, Dr. Paul Wessel, Dr. Tanya Atwater, Dr. David Sandwell, Dr. Ben Horner-Johnson, Dr. Walter H. F. Smith, Dr. R. Dietmar Müller, Dr. Robert Detenbeck, and Dr. Dawn Wright. The National Science Foundation provided funds that allowed this work to occur. Crucial administrative support that made graduation possible was provided by Barb Daugherty, Nadina Piehl and Flo Cole. Janet R. Giles, of the graduate school office, provided cheerful help with finalizing and submitting this document for graduation. Dr. Ted VanVleet was especially helpful as the graduate coordinator for the college and provided special attention for me on several occasions. As my employer for much of the time I worked on this thesis, Henry Norris exhibited encouragement and flexibility that allowed me to pursue this work. My co-worker, Jim Burd, provided invaluable encouragement and prodding near the completion of this work. Finally, this work was greatly facilitated by the moral support of Michelle McIntyre, my comrade in arms, who lent encouraging words and an open ear along the way. Table of Contents List of Tables iii List of Figures iv Abstract vi Chapter 1 Introduction 1 Chapter 2 Methods 7 Data 7 Anomaly Identification 7 Finite and Stage Poles 9 Reconstruction 14 Chapter 3 Results 16 Magnetic Anomaly Identifications 16 Spreading Rates 16 Asymmetrical Spreading 25 Anomaly Juxtapositions 26 Finite Poles 27 Stage Poles 29 Tectonic Reconstructions 30 Chron 10y 30 Chron 7y 37 Chron 6c 37 Chron 5d 37 Chron 5b 38 Chron 5aa 38 Chron 5o 39 Chron 4a 39 Chron 3a 39 Present 40 Chapter 4 Discussion 41 Chapter 5 Conclusions 47 References 49 i Appendices 53 Appendix A: Data File Information 54 Appendix B: 2D Magnetic Modeling 58 ii List of Tables Table 1. Calculated finite poles for PAC-NAZ. 13 Table 2. Covariance matrices for finite poles calculated in this study. 14 Table 3. Stage poles calculated from finite poles. 14 iii List of Figures Figure 1. General tectonic setting of southeast Pacific. 3 Figure 2. Cruises used in 2D magnetic modeling. 8 Figure 3. Synthetic magnetic anomaly model and magnetic timescale of Cande and Kent (1995) used in this study. 10 Figure 4. Magnetic profiles for cruises CATO4c (A) and EEL29d (B). 11 Figure 5. Magnetic data used in this study. 12 Figure 6. Interpreted magnetic isochrons. 17 Figure 7a. Grey-shade predicted bathymetry, magnetic data, interpreted tectonic lineations (blue lines) and volcanics (red hachures) with anomaly picks used to calculate finite poles for panel A. 18 Figure 7b. Detail of data for panel B. 19 Figure 7c. Detail of data for panel C. 20 Figure 7d. Detail of data for panel D. 21 Figure 7e. Detail of data for panel E. 22 Figure 7f. Detail of data for panel F. 23 Figure 8. Full-spreading rates calculated along estimated flowlines for Pacific-Nazca spreading. 24 Figure 9. Spreading asymmetry calculated from spreading rates (Figures 8). 25 Figure 10. Finite pole comparisons. 28 Figure 11. Stage poles for Pacific-Nazca relative motion. 29 iv Figure 12. Full spreading rate vectors compared to interpreted tectonic features and predicted bathymetry. 31 Figure 13. Tectonic reconstruction for chrons 10y (grey) (A) and 7y (olive) (B). 32 Figure 14. Tectonic reconstruction for chrons 6c (lt. red) (A) and 5d (red) (B). 33 Figure 15. Tectonic reconstruction for chrons 5b (orange) (A) and 5aa (lavender) (B). 34 Figure 16. Tectonic reconstruction for chrons 5o (purple) (A) and 4a (green) (B). 35 Figure 17. Tectonic reconstruction for chrons 3a (lt. blue) (A) and 5d (lt. purple) (B). 36 v
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