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The Salton Trough a Dissertation Submitted to the Department of Geophysics

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The Salton Trough a Dissertation Submitted to the Department of Geophysics PASSIVE SEISMIC STUDY OF A MAGMA-DOMINATED RIFT: THE SALTON TROUGH A DISSERTATION SUBMITTED TO THE DEPARTMENT OF GEOPHYSICS AND THE COMMITTEE ON GRADUATE STUDIES OF STANFORD UNIVERSITY IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY Shahar Barak November 2016 c Copyright by Shahar Barak 2017 All Rights Reserved ii I certify that I have read this dissertation and that, in my opinion, it is fully adequate in scope and quality as a dissertation for the degree of Doctor of Philosophy. (Simon Klemperer) Principal Adviser I certify that I have read this dissertation and that, in my opinion, it is fully adequate in scope and quality as a dissertation for the degree of Doctor of Philosophy. (Greg Beroza) I certify that I have read this dissertation and that, in my opinion, it is fully adequate in scope and quality as a dissertation for the degree of Doctor of Philosophy. (Norm Sleep) Approved for the Stanford University Committee on Graduate Studies iii Preface This PhD thesis began with the aim to solely study the magmatic structure beneath Salton Trough transtensional rift basin in southernmost California using a temporary array of seismometers deployed across the basin and its margins. However, during the 2-year station deployment period, I added a large data set from permanent and other temporary seismometer arrays in aim to improve data coverage above the study re- gion. As a result, I created a larger than planned Rayleigh-wave group-velocity model of the entire western U.S.A. and a shear-wave velocity model of southern California (See Chapter 2). In chapter 2, published in G-Cubed, I present new results and interpretations on the structure of the southern San Andreas Fault, the Peninsular Ranges batholith and southernmost Sierra Nevada batholith, in addition to this the- sis's main area of focus, the Salton Trough. The reader can find a detailed geological and geophysical background for the aforementioned regions in Chapter 2. The chapters in this thesis are divided by methodology. In chapter 2, I use ambient- noise tomography to create a 3D shear-velocity model of southern California's crust and upper-mantle. The new 3D model reveals previously unimaged structure be- neath the San Andreas Fault, Peninsular Ranges batholith, southern Sierra Nevada batholith and the Salton Trough, with implications on the geologic and tectonic his- tory of the region. In chapter 3, published in Geology, I use shear-wave splitting of seismic waves, caused by anisotropic upper-mantle structure beneath the Salton Trough. I show evidence of a sharp rheological boundary in the upper-mantle beneath the Salton Trough region, at the southwest limit of the San Andreas Fault system, and infer the presence of upper-mantle melt-filled inclusions oriented parallel to transform motion on the San Andreas Fault. In the final chapter, I calculate receiver functions iv on my array, and jointly invert them with my surface-wave dispersion curves (Chap- ter 2) to obtain a 2D shear-wave velocity model across the Salton Trough. I show improved imaging of the mantle upwelling beneath the rift. v Acknowledgments First and foremost I would like to thank my adviser Simon Klemperer, whose tireless enthusiasm and unfailing support made all of this work possible. Jesse Lawrence was a stalwart resource during my graduate studies, and I am grateful for his collaboration and advice over the years. The receiver-function stacking code used in Chapter 4 was principally of his writing. Greg Beroza and Norm Sleep, and George Thompson provided valuable comments during my annual reviews and Oral Defense. I thank Gary Fuis for sharing his SAF model and advice, Vicky Langenheim for sharing data and ideas, and Marty Grove for geological insights. I also thank Alex Kinsella (SURGE intern) and Monica Poletti (IRIS intern), my undergraduate interns, for improving my mentorship skills. And finally, the biggest thanks of all go to my parents, Yehuda and Merav, and my wife, Sivan, without whom none of this would have been possible. vi Contents Preface iv Acknowledgments vi 1 Introduction 1 2 San Andreas Fault dip, Peninsular Ranges mafic lower crust and partial melt in the Salton Trough, Southern California, from ambient-noise tomography 6 2.1 Abstract . .7 2.2 Introduction . .9 2.3 Geological and Geophysical Background . 10 2.3.1 San Andreas Fault . 10 2.3.2 The Mesozoic Arcs . 10 2.3.3 The Salton Trough . 13 2.4 Data and Method . 15 2.4.1 Data . 15 2.4.2 Seismic Waveform Processing . 15 2.4.3 2-D Tomographic Inversion . 16 2.4.4 Inversion to VS(z) . 17 2.5 Rayleigh Group-Velocity Model . 19 2.6 Shear-Wave Velocity Model . 21 2.6.1 San Andreas Fault . 25 2.6.2 The Mesozoic Batholiths: Peninsular Ranges and Sierra Nevada 31 vii 2.6.3 Salton Trough . 39 2.7 Summary . 47 2.8 Appendix: Calculation of Pore Geometry and Partial Melt . 48 2.9 Acknowledgments . 49 3 Rapid variation in upper-mantle rheology across the San Andreas fault system and Salton Trough, southernmost California 50 3.1 Abstract . 51 3.2 Introduction . 51 3.3 Analysis of Shear-Wave Splitting Measurements . 53 3.4 Results . 55 3.5 Discussion . 56 3.6 Conclusions . 59 3.7 Acknowledgments . 59 4 Imaging upper-mantle upwelling beneath the Salton Trough using joint inversion of receiver functions and surface wave dispersion curves 60 4.1 Abstract . 62 4.2 Introduction . 62 4.3 Data and Method . 62 4.4 Results . 62 4.5 Discussion . 62 4.6 Conclusions . 62 4.7 Acknowledgments . 62 A Data Acquisition 63 viii List of Tables ix List of Figures 1.1 A: Pacific (PAC)-North America (NAM) plate boundary (black: trans- form, orange: spreading center), showing location of B (black rectan- gle). B: Shaded-relief topography overlain with the broadband stations of the Salton Seismic Imaging Project (stars). CM-Chocolate Moun- tains; PRB-Peninsular Ranges Batholith; ST-Salton Trough. Red lines show major faults of the San Andreas fault system (SAFs) (AF- Algodones, EF-Elsinore, IF-Imperial, LSF-Laguna Salada, SAF-San Andreas, SHF-Sand Hills, SJF-San Jacinto) (Plesch et al., 2007). .2 x 2.1 (a) Map of stations used for ambient noise cross correlations, colored by recording epochs. Physiographic provinces from USGS (1946). Rect- angle shows area of (b) & (c). GOC: Gulf of California. Figure 2.1b shows Geographical and geological features. Broad black-dashed line: Compositional and geochemical boundary between the western Penin- sular Ranges Batholoith (PRB) and the eastern PRB from Todd et al. (1988). Red lines: fault traces after Plesch et al. (2007). AF: Algodones Fault; BSZ: Brawley Seismic Zone; CM: Chocolate Mountains; CP: Cerro Prieto volcano; CR: Coast Ranges; EF: Elsinore Fault; GF: Gar- lock Fault; GV: Great Valley; IF: Imperial Fault; IV: Imperial Valley; KCF: Kerns Canyon Fault; LSB: Laguna Salada Basin; LSF: Laguna Salada Fault; OVF: Owens Valley Fault; ePRB and wPRB: east and west Peninsular Ranges Batholith; SAF: San Andreas Fault; SB: Salton Buttes; SBM: San Bernardino Mountains; SGM: San Gabriel Moun- tains; SGP: San Gorgonio Pass (black dot); SHF: Sand Hills Fault; SJF: San Jacinto Fault; SNB: Sierra Nevada Batholith WTR: West- ern Transverse Ranges. Controlled source profiles: NB82: (Nava and Brune, 1982); PM96: (Parsons and McCarthy, 1996); H13:(Han et al., 2013). Figure 2.1c shows locations of profiles in Figures 2.6{ 2.11: San Andreas Fault: AA0{II0 (red); Peninsular Ranges: (PR)aa0{cc0 (green); Sierra Nevada: (SN)aa0{bb0 (blue); Salton Trough: (ST)aa0{cc0 (yel- low). Dipping SAF model (Fuis et al., 2012) colored by depth. .8 2.2 Schematic of 13 starting models used for each 1-D profile of VP , VS and ρ extracted from CVM-H11.9, created by increasing and decreasing the velocity up to 15%. 18 2.3 (left) Comparison of our Rayleigh group-velocity model to (right) Moschetti et al. (2007) showing deviation from the mean group velocity (U) at 14 s. Dashed-line rectangle: area of the model we inverted for shear-wave velocity. Solid thin lines: state and physiographic boundaries after USGS (1946). 20 xi 2.4 Maps of our Rayleigh group-velocity model in southern California, at periods of 8, 16, 24, and 40 s, shown as deviation from the mean group velocity (U) of the entire western U.S. model for that period, with color range varying between maps due to the large variation in velocity perturbations. Annotations as in Figure 2.1b. 22 2.5 Depth slices through our final Vs model at 7, 20 and 42 km depth. 24 2.6 Caption on previous page. 27 2.6 ....................................... 28 2.6 ....................................... 29 2.7 (a) Depth to the shallowest 3.6 km/s isovelocity surface, showing deep- ening (lower velocities) NE of the SAF and NE of the boundary between wPRB and ePRB. (b) Depth to the shallowest 3.8 km/s isovelocity sur- face, showing deepening (lower velocity) NE of the PRB and E of the prebatholithic suture in the SNB (see Figure 2.10). Fault traces and physiographic divisions as in Figure 2.1. Depth contours at 5km interval. 32 2.8 West-east profiles across the PRB through our VS final model, as shown in Figure 2.1c. Figure annotation as in Figure 2.6. Dashed line: com- positional boundary between wPRB and ePRB, extrapolated to depth at a 45◦ angle (cf. Langenheim et al., 2014). 33 2.9 Comparison along PRb{PRb0 (Figure 2.8b) between our model (a), CVM-H11.9 (initial model; b), and CVM-S4.26 (c). (d) Standard de- viation of our model.
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