Constitution and Genesis of the Central Part of the Sierra Nevada Batholith, California

Total Page:16

File Type:pdf, Size:1020Kb

Constitution and Genesis of the Central Part of the Sierra Nevada Batholith, California DEPARTMENT OF INTERIOR U.S. GEOLOGICAL SURVEY Constitution and Genesis of the Central Part of the Sierra Nevada Batholith, California by Paul C. Batemanl/ This report supplements Open File Report 87-670, Pre-Tertiary bedrock geologic map of the Mariposa 1* by 2* quadrangle, California. It provides expanded descriptions of the features shown on the map and interpretations of their significance and origin. It does not include the map. Open-File Report 88-382 This report is preliminary and has not been reviewed for conformity with U.S, Geological Survey editorial standards. Any use of trade names is for descriptive purposes only and does not imply endorsement by the USGS. Park, California Note for New Publications of the U.S. Geological Survey Open File Report . Constitution and genesis of the central part of the Sierra Nevada batholith, California, by Paul C. Bateman. This publication supplements Open File Report 87-670, Pre-Tertiary bedrock geologic map of the Mariposa 1° by 2° quadrangle, California by providing descriptions and interpretations of the rocks and structures shown on the map. Summarizes the results of more than 35 years of study by members of the Geological Survey of the bedrock geology of the central part of the Sierra Nevada batholith between 37° and 38° N. Lat. CONTENTS Page Abstract 12 Introduction 16 Stratigraphic and structural setting 17 Hetamorphism 18 Late Proterozoic and Paleozoic strata of the White and northern Inyo Mountains 19 Wyman Formation, Reed Dolomite, and Deep Spring Formation 19 Campito Formation 20 Poleta, Harkless, Saline Valley, and Mule Spring Formations 20 Monola Formation and Bonanza King and Tamarack Canyon Dolomites 20 Emigrant (?) Formation 21 Cambrian strata, undivided 21 Al Rose, Badger Flat, Barrel Spring, Johnson Spring, Palmetto, and Sunday Canyon Formations 21 Perdido Formation, Rest Spring Shale, and Keeler Canyon Formation 21 Paleozoic strata in roof pendants of the eastern Sierra Nevada 21 Mesozoic strata in roof pendants and in the White Mountains 22 Koip sequence and other Triassic (?) and Jurassic metavolcanic rocks 23 Dominantly pyroclastic strata of Early Cretaceous age 25 Dana sequence 25 Minarets sequence 25 Metavolcanic rocks, undivided 26 Kings sequence 27 Strata east of the Melones fault zone within and adjacent to the western metamorphic belt 28 Quartzite of Pilot Ridge 30 Phyllite and chert of Hites Cove 30 Phyllite of Briceburg 30 Greenstone of Bullion Mountain 31 Strata in roof pendants south of the western metamorphic belt 31 Mariposa Formation and adjacent strata west of the Melones fault zone -31 Structures in the country-rock sequences 32 Structures in the White and northern Inyo Mountains 33 Structures in roof pendants of the eastern Sierra Nevada 35 Structures in the Kings sequence 36 Structures within the western metamorphic belt 37 Tectonic episodes 39 Mississippian (Antler? ) orogeny 39 Early Triassic (Sonoman?) orogeny 39 Late Triassic deformation 39 Late Jurassic Nevadan orogeny 40 Late Early Cretaceous deformation 40 Mid-Cretaceous deformation 40 Late Cretaceous (and Tertiary?) deformations 41 Hierarchial organization of granitic units 41 Plutons 42 Lithodemes 42 Intrusive suites 43 Roof pendants, septa, and inclusions 44 Sampling, analytical proceedures, and reporting of data 44 Chemical analyses 44 Modal analyses 45 Isotopic ages 46 I-type and S-type and magnetite-series and ilmenite-series granitoids 46 Physical features of the granitic rocks 47 Minerals 47 Quartz 47 Alkali feldspar 47 Alkali-feldspar megacrysts 48 Plagioclase 50 Biotite and hornblende 50 Accessory minerals 51 Texture 52 Texture in undeformed granitoids 52 Texture in deformed granitoids 52 Foliation and lineation 53 Primary magmatic foliation and lineation 53 Disturbed primary foliation 54 Ductile foliation and lineation 54 Deformation attributed to regional stress 54 Shear zones in the eastern Sierra Nevada 55 Deformation associated with emplacement of intrusions 56 Deformation associated with emplacement of the Ward Mountain Trondhjemite 57 Deformation associated with intrusions in the White and northern Inyo Mountains 58 Mafic inclusions 59 Schlieren 61 Comb layering and orbicules 62 Joints and microfaults 63 Magma emplacement and solidification 64 Depth of erosion since plutonism 64 Physical constitution of Sierran magmas 65 Mode of emplacement (the space problem) 67 Foreible emplacement 67 Stoping 69 Regional extension 69 Erosion and volcanism 70 Sequence of crystallization of minerals 70 Crystallization in relation to the salic tetrahedron 72 Low-Or Fine Gold Intrusive Suite 73 Medium-Or Tuolumne Intrusive Suite 74 High-Or Soldier Pass Intrusive Suite 74 Interpretation of modal plots 75 Fine Gold Intrusive Suite 75 Tuolumne Intrusive Suite 75 Soldier Pass Intrusive Suite 76 Magma mixing 76 Regional age patterns 77 History of isotopic dating in the central Sierra Nevada 77 Ages of intrusive suites and unassigned units 78 Triassic intrusive rocks 79 Jurassic intrusive rocks 79 Cretaceous intrusive rocks 80 Rate of eastward migration of plutonism during the Cretaceous 80 Duration of magmatism in the formation of intrusive suites 81 Compositional patterns 81 Patterns within intrusive units 81 Tuolumne Intrusive Suite 81 Shaver Intrusive Suite 8A Mount Givens Granodiorite 85 Palisade Crest Intrusive Suite 86 Tinemaha Granodiorite 87 Granodiorite of McMurry Meadows 88 Regional patterns 88 Modal variations 89 Variations of major oxides 89 Variations in the alkali-lime (Peacock) index 90 Variations of minor elements 91 Isotopic variations 91 Strontium 91 Neodymium 93 Oxygen 93 Relations of volcanism and plutonism 9A Shifts in the loci of magma t ism - ---- _____ 95 Subsurface structure 96 Seismic data 97 Gravity data 98 Magnetic data 98 Heat generation and heat flow 99 Xenoliths in Tertiary volcanic rocks 99 Water composition in springs and wells 101 Composition, age and origin of the Sierran root 102 Westward tilting and uplift of the Sierra Nevada 103 Ore deposits 10A Gold 104 Copper 107 Tungsten skarn deposits 107 General features of skarns 108 Structural and stratigraphic setting 108 Mineralogical and chemical relations 109 Donut ore body of the Pine Creek mine 109 Pine Creek mine 109 Strawberry mine 112 Skarns in the Mount Morrison roof pendant 113 Working model for the origin and emplacement of the batholith 113 Previous proposals 11A Present reconstruction 116 Descriptions of the plutonic rocks 121 Western slope of the Sierra Nevada 121 Fine Gold Intrusive Suite 121 Tonalite of Ross Creek (Kro) 122 Bass Lake Tonalite (Kbl) 122 Granodiorite of Arch Rock and other small plutons of biotite granite and granodiorite (Kar) 124 Ward Mountain Trondhjemite (Kwt) 124 Knowles Granodiorite (Kkn) 125 Intrusive suite of Yosemite Valley 126 El Cap it an Granite (Kec) 126 Granite of Rancheria Mountain (Krm) 127 Taft Granite and leucogranite of Ten Lakes (Kt) 127 Shaver Intrusive Suite 127 Dinkey Creek Granodiorite (Kdc, Kdcp) 128 Granodiorite of McKinley Grove (Kink) 129 Granodiorite of Pick and Shovel mine area (Kps) and granite of Ordinance Creek (Ko) 129 Granite of Shuteye Peak (Ksp) 129 Granites of Dinkey Dome, Short Hair Creek, Sheepthief Creek lower Bear Creek, Mushroom Rock, and north of Snow Corral Meadow (Kdd) 129 Possible additional units of the Shaver Intrusive Suite: Granodiorites of Whisky Ridge and Stevenson Creek (Kwr) 130 Intrusive suite of Buena Vista Crest 131 Quartz diorite dikes in El Cap it an (Kqe) 131 Granodiorites of Illilouette Creek and Tamarack Creek, tonalite of Crane Creek, and Leaning Tower Granite (Ki) 131 Granodiorite of Ostrander Lake (Kol) 132 Granodiorite of Breeze Lake (Kbz) 132 Bridalveil Granodiorite and granodiorite of Horse Ridge (Kbd) 132 Granite of Chilnualna Lake (Kcl) 132 Intrusive suite of Merced Peak 132 Granodiorite of Jackass Lakes (Kja) 133 Leucogranites of Timber Knob and Morris Creek (Ktk) 133 Intrusive Suite of Washburn Lake 133 Granodiorite of Red Devil Lake (Krd) 133 Granite of Turner Lake (Ktl) 134 Granite porphyry of Cony Crags (Kcc) 134 Relations of the intrusive suites of Buena Vista Crest, Merced Peak, and Washburn Lake to one another and to the Minarets sequence 134 Tuolumne Intrusive Suite 134 Granodiorites of Kuna Crest and Grayling Lake, and tonalites of Glen Aulin and Glacier Point (Kk) 135 Half Dome Granodiorite (Khd, Khdp) 135 Cathedral Peak Granodiorite (Kcp) 136 Johnson Granite Porphyry (Kj) 137 Possible earlier units of the Tuolumne Intrusive Suite 137 Granodiorite of Yosemite Creek (Kyc) 137 Sentinel Granodiorite (Kse) 138 John Muir Intrusive Suite 138 Lamarck Granodiorite (Klk) 138 Mount Givens Granodiorite (King, Kmgp) 139 Lake Edison Granodiorite (Kle) 140 Granite of Rock Creek Lake (Krd) 141 Round Valley Peak Granodiorite (Krv) 141 ^*w»lvJ vsL C61v xTJ/O-ili v?6 \ xxXlivJ / ««». »«««»«..«« «. __. «« M» « «.«»*»«.»»«.» «.»«.«.«.«.«. A *r t Evolution Basin Alaskite (Kev) 142 Small intrusions west of the Mount Givens Granodiorite 144 Granodiorites of Red Lake, Eagle Peak, ^Mnnrt *V* RIPL* A£) Wl»rVoelr v^ XV xfVr-1 XVI. A /\ ______________ __ _____ _ __________ __ 1A "T"TAA Leucogranite of Bald Mountain (Kbm) 146 Leucogranites of Big Sandy Bluffs and Lion Point, and leucogranodiorites of Burrough and Black Mountains& * W V* I A V> d- A I A 0 flfbb^\ IX \J%Jf ________________________________«-«-«- » ««__« _________» » « « « «_ « » «_ 1^ A&«^ ^j Granitic rocks of the western slope of the Sierra Nevada not assigned to intrusive suites 146 Granitoids of Jurassic age in the northwest corner of t^lPi IT13.C &1769. - ' ' ' ' - ' - « ' - - - - - - - - - - - - -^ «_ .. 1 A 6 Tonalite of Granite Creek (Jgc) 146 \yl/cUl JL t-C w » IW WOS JC\ JLU^6 ^ *j iVL / *"~ ~ ~~ ~~ - "- «.«.«.«_«. «.«.«.«.«.«.^c| j Tonalite of Millerton Lake (Kml) 147 Unassigned granitic rocks of the Yo Semite area 147 Granite Porphyry of Star Lakes Ksl) 147 Tonalite of Aspen Valley (Kav) 148 Quartz diorite of Mount Gibson (Kgi) 148 Granodiorite of Bearup Lake (Kbu) 148 Granitoids at the northwest end of the Mount Givens fZt^onnrf\7i. ^UA%J%&AV^1» \ r\Y*\ JL i"o\+^Z «- «-«-«-«-«- _ «~ _ _^.«_ .« « « _«.« « _«.«_«_«.« __ _ «.«.«__ _ __ M-.
Recommended publications
  • Frontispiece the 1864 Field Party of the California Geological Survey
    U.S. DEPARTMENT OF THE INTERIOR U. S. GEOLOGICAL SURVEY GEOLOGIC ROAD GUIDE TO KINGS CANYON AND SEQUOIA NATIONAL PARKS, CENTRAL SIERRA NEVADA, CALIFORNIA By James G. Moore, Warren J. Nokleberg, and Thomas W. Sisson* Open-File Report 94-650 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. * Menlo Park, CA 94025 Frontispiece The 1864 field party of the California Geological Survey. From left to right: James T. Gardiner, Richard D. Cotter, William H. Brewer, and Clarence King. INTRODUCTION This field trip guide includes road logs for the three principal roadways on the west slope of the Sierra Nevada that are adjacent to, or pass through, parts of Sequoia and Kings Canyon National Parks (Figs. 1,2, 3). The roads include State Route 180 from Fresno to Cedar Grove in Kings Canyon Park (the Kings Canyon Highway), State Route 198 from Visalia to Sequoia Park ending near Grant Grove (the Generals Highway) and the Mineral King road (county route 375) from State Route 198 near Three Rivers to Mineral King. These roads provide a good overview of this part of the Sierra Nevada which lies in the middle of a 250 km span over which no roads completely cross the range. The Kings Canyon highway penetrates about three-quarters of the distance across the range and the State Route 198~Mineral King road traverses about one-half the distance (Figs.
    [Show full text]
  • Subduction Cycles Under Western North America During the Mesozoic and Cenozoic Eras
    .. Geological Society of America Special Paper 299 1995 Subduction cycles under western North America during the Mesozoic and Cenozoic eras Peter L. Ward U.S. Geological Survey, 345 Middlefield Road, MS 977, Menlo Park, California 94025 ABSTRACT An extensive review of geologic and tectonic features of western North America suggests that the interaction of oceanic plates with the continent follows a broad cycli- cal pattern. In a typical cycle, periods of rapid subduction (7-15 cdyr), andesitic vol- canism, and trench-normal contraction are followed by a shift to trench-normal extension, the onset of voluminous silicic volcanism, formation of large calderas, and the creation of major batholiths. Extension becomes pervasive in metamorphic core complexes, and there is a shift to fundamentally basaltic volcanism, formation of flood basalts, widespread rifting, rotation of terranes, and extensive circulation of flu- ids throughout the plate margin. Strike-slip faulting becomes widespread with the creation of new tectonostratigraphic terranes. A new subduction zone forms and the cycle repeats. Each cycle is 50-80 m.y. long; cycles since the Triassic have ended and begun at approximately 225, 152, 92, 44, and 15 Ma. The youngest two cycles are diachronous, one from Oregon to Alaska, the other from central Mexico to Califor- nia. The transitions from one cycle to the next cycle are characterized by rapid and pervasive changes termed, in this chapter, “major chaotic tectonic events.” These events appear to be related to the necking or breaking apart of the formerly sub- ducted slab at shallow depth, the resulting delamination of the plate margin, and the onset of a new subduction cycle.
    [Show full text]
  • Construction and Emplacement of Cretaceous Plutons in the Crystal Range, Southwest of Lake Tahoe, California
    San Jose State University SJSU ScholarWorks Master's Theses Master's Theses and Graduate Research Summer 2017 Construction and Emplacement of Cretaceous Plutons in the Crystal Range, Southwest of Lake Tahoe, California Brad Buerer San Jose State University Follow this and additional works at: https://scholarworks.sjsu.edu/etd_theses Recommended Citation Buerer, Brad, "Construction and Emplacement of Cretaceous Plutons in the Crystal Range, Southwest of Lake Tahoe, California" (2017). Master's Theses. 4837. DOI: https://doi.org/10.31979/etd.eyj9-3w7m https://scholarworks.sjsu.edu/etd_theses/4837 This Thesis is brought to you for free and open access by the Master's Theses and Graduate Research at SJSU ScholarWorks. It has been accepted for inclusion in Master's Theses by an authorized administrator of SJSU ScholarWorks. For more information, please contact [email protected]. CONSTRUCTION AND EMPLACEMENT OF CRETACEOUS PLUTONS IN THE CRYSTAL RANGE, SOUTHWEST OF LAKE TAHOE, CALIFORNIA A Thesis Presented to The Faculty of the Department of Geology San José State University In Partial Fulfillment of the Requirements for the Degree Master of Science by Brad Buerer August 2017 © 2017 Brad Buerer ALL RIGHTS RESERVED The Designated Thesis Committee Approves the Thesis Titled CONSTRUCTION AND EMPLACEMENT OF CRETACEOUS PLUTONS IN THE CRYSTAL RANGE, SOUTHWEST OF LAKE TAHOE, CALIFORNIA by Brad Buerer APPROVED FOR THE DEPARTMENT OF GEOLOGY SAN JOSÉ STATE UNIVERSITY August 2017 Dr. Robert Miller Department of Geology Dr. Jonathan Miller Department of Geology Dr. Dave Andersen Department of Geology ABSTRACT CONSTRUCTION AND EMPLACEMENT OF CRETACEOUS PLUTONS IN THE CRYSTAL RANGE, SOUTHWEST OF LAKE TAHOE, CALIFORNIA by Brad Buerer Three Cretaceous plutons are investigated to determine their construction and emplacement histories, focusing on magmatic foliation patterns and contact relationships with each other and with the Jurassic metasedimentary host rocks of the Sailor Canyon Formation.
    [Show full text]
  • Birth of the Sierra Nevada Magmatic Arc: Early Mesozoic Plutonism and Volcanism in the East-Central Sierra Nevada of California
    Origin and Evolution of the Sierra Nevada and Walker Lane themed issue Birth of the Sierra Nevada magmatic arc: Early Mesozoic plutonism and volcanism in the east-central Sierra Nevada of California A.P. Barth1, J.D. Walker2, J.L. Wooden3, N.R. Riggs4, and R.A. Schweickert5 1Department of Earth Sciences, Indiana University–Purdue University, Indianapolis, 723 West Michigan Street, SL118, Indianapolis, Indiana 46202, USA 2Department of Geology, University of Kansas, 1475 Jayhawk Boulevard, Lawrence, Kansas 66045, USA 3Department of Geological and Environmental Sciences, Stanford University, 450 Serra Mall, Stanford, California 94305, USA 4School of Earth Sciences and Environmental Sustainability, Northern Arizona University, Campus Box 4099, Flagstaff, Arizona 86011, USA 5Department of Geological Sciences, University of Nevada, Reno, Nevada 89557, USA ABSTRACT continued during emplacement of the 226– the older, northeast-trending margin (Schweick- 218 Ma Scheelite Intrusive Suite. Ash-fl ow ert and Lahren, 1987; Greene et al., 1997a; Ste- Granitic and volcanic rocks in the east- tuffs are hydrothermally altered but have vens et al., 1997; Stevens and Greene, 2000; central Sierra Nevada, western United high fi eld strength element abundances and Fig. 1), and the initiation of arc volcanism. This States, record the earliest stages of magma- Nd isotopic compositions, suggesting affi nity early Mesozoic volcanism and associated plu- tism in the eastern Sierra Nevada magmatic to the relatively felsic parts of the Wheeler ton emplacement are key constraints on tectonic arc, allowing us to examine magma sources Crest Granodiorite and the granite of Lee models for subduction initiation at the west- and connections between plutonic and volca- Vining Canyon.
    [Show full text]
  • Wallrocks of the Central Sierra Nevada Batholith, California: a Collage of Accreted Tectono-Stratigraphic Terranes
    Wallrocks of the Central Sierra Nevada Batholith, California: A Collage of Accreted Tectono-Stratigraphic Terranes GEOLOGICAL SURVEY PROFESSIONAL PAPER 1255 Wallrocks of the Central Sierra Nevada Batholith, California: A Collage of Accreted Tectono-Stratigraphic Terranes By WARREN J. NOKLEBERG GEOLOGICAL SURVEY PROFESSIONAL PAPER 1255 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1983 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Nokleberg, Warren J. Wallrocks of the central Sierra Nevada batholith, California. (Geological Survey Professional Paper 1255) Bibliography: 28 p. Supt. of Doca. No.: I 19.16:1255 1. Batholiths Sierra Nevada Mountains (Calif, and Nev.) I. Title. II. Series. QE461.N64 552'.3 81-607153 AACR2 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract .................................... 1 Cretaceous metavolcanic rocks ..................... 14 Introduction .................................. 1 Occurrence ............................... 14 Definitions ................................ 2 Stratigraphy and structure .................... 14 Acknowledgments ........................... 2 Kings terrane ................................ 14 Relation of multiple regional deformation to terrane Occurrence ............................... 14 accretion .................................. 2 Stratigraphy .............................. 15 Relation of terranes
    [Show full text]
  • 216196482.Pdf
    TECTONICS, VOL. 5, NO. 1, PAGES 65-94, FEBRUARY1986 STRUCTURAL HISTORY OF CONTINENTAL VOLCANIC ARC ROCKS, EASTERN SIERRA NEVADA, CALIFORNIA: A CASE FOR EXTENSIONAL TECTONICS Othmar T. Tobisch Earth Science Department, Applied Science Building, University of California Santa Cruz Jason B. Saleeby Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena Richard S. Fiske National Museum of Natural History Smithsonian Institution Washington, D.C. Abstract. Mesozoic metavolcanic rocks and greater constrictional component than forming part of the continental volcanic the Ritter Range for rocks of comparable arc along the eastern Sierra Nevada near age. Calculations based on the strain data Mt. Goddard and in the Ritter Range show a suggest tile Mt. Goddard section has been complex history related to extensional thinned by about 50% norma] to bedding, tectonics. The rocks comprise a thick sec- much as that documentedpreviously for tion of tuffs, breccias, lava flows, rocks in the Ritter Range. Deformation sills, and ash-flow tuffs deposited in a within this part of the continental arc subaerial to subaqueous environment, with was originally thought to have formed by some subvolcanic sill-like plutons. Pb/U regional compression during the late Jur- ages of the rocks in the Mt. Goddard area assic (Nevadan) orogeny. However, our range from ca. 130-160 Ma, while rocks in study indicates that (1) parts of the the Ritter Range have a somewhat wider age deformed volcanic section are younger than range as reported previously. Repetition late 0urassic, (2) Nevadan-age breaks in of the section occurs by faulting, and deposition are not present, (3) large-scale with the exception of parts of the mid- folds expected during a regional compres- Cretaceous Minarets Caldera, all the vol- sion event are not common, and (4) the beds canic rocks show a regional slaty cleavage were tilted to a high dip prior to internal which was subsequently crenulated and/or deformation.
    [Show full text]
  • The Structural and Metamorphic History of the Oakhurst Roof Pendant, Mariposa and Madera Counties, California
    UNLV Theses, Dissertations, Professional Papers, and Capstones 12-1972 The structural and metamorphic history of the Oakhurst roof pendant, Mariposa and Madera counties, California Lee R. Russell Texas Tech University Follow this and additional works at: https://digitalscholarship.unlv.edu/thesesdissertations Part of the Geology Commons, and the Tectonics and Structure Commons Repository Citation Russell, Lee R., "The structural and metamorphic history of the Oakhurst roof pendant, Mariposa and Madera counties, California" (1972). UNLV Theses, Dissertations, Professional Papers, and Capstones. 1443. http://dx.doi.org/10.34917/3432680 This Thesis is protected by copyright and/or related rights. It has been brought to you by Digital Scholarship@UNLV with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in UNLV Theses, Dissertations, Professional Papers, and Capstones by an authorized administrator of Digital Scholarship@UNLV. For more information, please contact [email protected]. THE STRUCTURAL AND METAMORPHIC HISTORY OF THE OAKHURST ROOF PENDANT, MARIPOSA AND MADERA COUNTIES, CALIFORNIA by LEE R. RUSSELL, B.A. A THESIS IN GEOLOOY Submitted to the Graduate Faculty of Texas Tech University in Partial Fulfillment of i. the Requ~rements for .the Degree of MASTER OF SCIENCE Director December, 1972 .. ,.,... --- ----------·~ AC: £tJ5' 13 !97Z (\)o.
    [Show full text]
  • Emplacement Mechanisms and Magma Driving Pressure of the Proterozoic Curecanti Pluton; the Black Canyon of the Gunnison, Colorado
    University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Masters Theses Graduate School 5-2013 EMPLACEMENT MECHANISMS AND MAGMA DRIVING PRESSURE OF THE PROTEROZOIC CURECANTI PLUTON; THE BLACK CANYON OF THE GUNNISON, COLORADO Gordon Leonard Hicks The University of Tennessee, Knoxville, [email protected] Follow this and additional works at: https://trace.tennessee.edu/utk_gradthes Part of the Geology Commons, and the Tectonics and Structure Commons Recommended Citation Hicks, Gordon Leonard, "EMPLACEMENT MECHANISMS AND MAGMA DRIVING PRESSURE OF THE PROTEROZOIC CURECANTI PLUTON; THE BLACK CANYON OF THE GUNNISON, COLORADO. " Master's Thesis, University of Tennessee, 2013. https://trace.tennessee.edu/utk_gradthes/1626 This Thesis is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Masters Theses by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a thesis written by Gordon Leonard Hicks entitled "EMPLACEMENT MECHANISMS AND MAGMA DRIVING PRESSURE OF THE PROTEROZOIC CURECANTI PLUTON; THE BLACK CANYON OF THE GUNNISON, COLORADO." I have examined the final electronic copy of this thesis for form and content and recommend that it be accepted in partial fulfillment of the requirements for the degree of Master of Science, with a major in Geology. Micah J. Jessup, Major Professor We have read
    [Show full text]
  • Plutonism in the Central Part of the Sierra Nevada Batholith, California
    Plutonism in the Central Part of the '5n«Sierra Nevada Batholith,* California *~r ._*» U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1483 Plutonism in the Central Part of the Sierra Nevada Batholith, California By PAUL C. BATEMAN U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1483 A study of the structure, composition, and pre-Tertiary history of the Sierra Nevada batholith in the Mariposa 1° by 2° quadrangle UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1992 U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY DALLAS L. PECK, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging-in-Publication Data Bateman, Paul Charles, 1910- Plutonism in the central part of the Sierra Nevada batholith, California / by Paul C. Bateman p. cm. (U.S. Geological Survey professional paper ; 1483) Includes bibliographical references. 1. Batholiths Sierra Nevada Mountains (Calif, and Nev.) 2. Geology Sierra Nevada Mountains (Calif, and Nev.) I. Title. II. Series: Geological Survey professional paper ; 1483. QE11.5.U6B36 1992 91-14788 552M dc20 CIP For sale by the Books and Open-File Report Sales, U.S. Geological Survey, Federal Center, Box 25286, Denver, CO 80225 CONTENTS Page Hierarchical organization of granitic units 24 Introduction Plutons 25 Stratigraphic and structural setting Lithodemes 25 Metamorphism Late Proterozoic and Paleozoic strata of the White and Roof pendants, septa, and inclusions
    [Show full text]
  • Paleotectonic and Paleogeographic Significance of the Calaveras Complex, Western Sierra Nevada, Californ I A
    PALEOTECTONIC AND PALEOGEOGRAPHIC SIGNIFICANCE OF THE CALAVERAS COMPLEX, WESTERN SIERRA NEVADA, CALIFORN I A Richard A. Schweicker t Lamont-Doherty Geological Observatory of Columbia Uni ver sit y, Palisades , N. Y. 10964 Jason B. Saleeby Department of Geo logy and Geophysics Univer sity of California, Berkeley, California 94720 Othmar T. Tobisch Unive r sit y of California, Santa Cruz, California Ea rth Science Board, Applied Science Building Sant a Cruz , California 95064 William H. Wr ight, III Depar tment of Geology , California State College Sonoma , Rohne rt Park, California 94928 ABSTRACT marginal basin i s consider ed to have been situated be tween the Co rdilleran miogeocline to the southeas t The Calave r as Complex of the western Sierra and a volcanic arc t errane to the northwest. The Nevada , as defined he re , cons ists of a 375 km l ong, late Paleozoic Havallah sequence of north-central 35 km wide belt of metasediment ary and me t avolcanic Nevada i s bel ieved to have accumulated in the same r ocks , bounded on the west by the Melones faul t zone marginal basin. and Kings- Kaweah suture , and on the east by the The Me lones fault zone and Kings- Kaweah s uture Sierr a Nevada bathol ith. The Calave ras Compl ex forms r epresent a zone of early Mesozoic t ectonic trunca­ a cont inuous northwest-trendi ng belt between t he tion a long which the Calaveras Complex is j uxtaposed Placerville ar ea and the Mer ced Rive r area . South of against upper Paleozoic ophiolitic r ocks and Jurassic t he Me r ced River the belt extends in numerous r oof volcan ic and epiclast ic r ocks.
    [Show full text]
  • Geology and Climatology of the Saddlebag Lake Region Near Tioga Pass, California
    Geology and Climatology of the Saddlebag Lake Region near Tioga Pass, California. Ryan J Hollister – Turlock High School – www.mrhollister.com Laura K Hollister – Pitman High School This field trip is designed around a five mile hiking tour into the stunningly beautiful eastern crest of the Sierra Nevada just north of Tioga Pass in the Twenty Lakes Basin of the Hoover Wilderness Area. The tour will explore the glacially-incised boundary zone between the Sierra Nevada Batholith and Saddlebag Lake Pendant which contains rocks from the earliest beginnings of the Sierra Nevada. A good chunk of time will also be given to the exploration of past and present climatology of the area including prehistoric glaciations and historic weather phenomena created by seasonal fluctuations of land and sea temperatures. 4 4 Figure 1 - Roadmap of stops on this trip. Hiking at Saddlebag Lake takes place at Stop 4. A detailed map of the hike route and topography can be found on Figure 2. 1 = Baker Station. 2 = Leavitt Falls, 3 = Saddlebag Lake Pullout. 4 = Saddlebag Lake Hike. 5 = Lateral Moraines. 6 = Wave Cut Terraces of Lake Russell. 7 = Mono Winds Discussion at Conway Summit. Moderate to strenuous hiking at elevations over 10,000’ is required. Also, an $11 dollar water taxi fee across Saddlebag Lake that will eliminate four extra miles of hiking. The roads up to Saddlebag Lake and Log Cabin Mine Road are rough gravel, but most high clearance 2WD vehicles should have no problem navigating them. NAGT Far West Region. Fall 2012 Conference - Ryan & Laura Hollister Our road log follows a very similar path to that of Garry Hayes’ (see A Teachers Guide to the Eastern Sierra Nevada between Sonora Pass and June Lake, California) who has done an exceptional job explaining details of roadside attractions all the way south to the June Lake Loop.
    [Show full text]
  • Stratigraphy and Structure of the Saddlebag Lake Roof Pendant, Sierra Nevada, California
    Stratigraphy and structure of the Saddlebag Lake roof pendant, Sierra Nevada, California CHARLES A. BROOK* Department of Geology, California State University, Fresno, Fresno, California 93740 ABSTRACT more apparent that an understanding of the structural and strati- graphic histories of the Sierran metamorphic rocks is essential to Geologic mapping of the southern part of the Saddlebag Lake understanding the Mesozoic and pre-Mesozoic tectonics of the roof pendant, east-central Sierra Nevada, California, reveals three western margin of North America. Concepts learned here will in rock sequences that have been multiply deformed. The oldest se- turn influence interpretations on the origin of the Sierra Nevada quence consists of the metamorphosed equivalents of marine batholith. With this in mind, I will describe and then attempt to sedimentary rocks of Silurian(?)-Ordovician(?) age. Metamor- correlate rocks and structures in the Saddlebag Lake roof pendant phosed volcanic and volcaniclastic rocks and basal conglomerate with those in other roof pendants of the central Sierra Nevada. As (possibly in part continental) of Permian age unconformably overlie such, this will enlarge upon data and ideas presented in an earlier the older sequence. Another metavolcanic and metasedimentary abstract (Brook, 1974). sequence of unknown age, here designated Permian(?)-Triassic(?), and of uncertain boundary relationships with the two older se- LOCATION quences crops out in the southern part of the pendant. Field observations of minor structures and structural analysis in- The Saddlebag Lake roof pendant is located in the east-central dicate that rocks of the Silurian(?)-Ordovician(?) sequence have Sierra Nevada, California, approximately 10 km west of Mono undergone three episodes of deformation, whereas the Permian and Lake (Fig.
    [Show full text]