Geology of the Silver King Area, Superior, Arizona by Frederic

Total Page:16

File Type:pdf, Size:1020Kb

Geology of the Silver King Area, Superior, Arizona by Frederic Geology of the Silver King area, Superior, Arizona Item Type text; Dissertation-Reproduction (electronic) Authors Galbraith, Frederic W. (Frederic Williams), 1903- Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 07/10/2021 11:46:57 Link to Item http://hdl.handle.net/10150/565555 Geology of the Silver King Area, Superior, Arizona by Frederic William Galbraith 3rd. Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy Graduate College University of Arizona 1935 Approved: / ^ __ J ■ Q ^ r z ^ Z - V - 3 t Major professor /Date . ' ' X r f//" ^ 3 Contents Page Outline of report........................ ......... Introduction...................................... Scope of investigation......................... Location and extent of the area................ Acknowledgements............................... Bibliography................................... Climate, flora and fauna..... .................. Early history of the region.................... CDcnzv>roHHH-< Topographic features of the area............... 13 General geology................................... 15 Principal features............................. 15 Previous geological investigation.............. 17 Globe quadrangle............. 19 Pinal schist............................. 19 Apache group..............................20 Bay quadrangle.............................. 21 Pinal schist..............................22 Apache group............................. 22 Me tamorphic pre-Cambrian rocks................. 24 Pinal schist................................ 24 Petrographic detail of schist............ 24 Petrographic detail of greenstone......... 25 Petrographic detail of gneissoid facies...26 Origin of the Pinal schist.................. 27 Sedimentary rocks.............................. 27 Pre-Cambrian system........ 27 Apache group............................. 27 Scanlan conglomerate.................. 27 Pioneer shale......................... 29 Barnes conglomerate................... 31 Dripping Spring quartzite............. 32 Petrographic detail of quartzite....33 Mescal limestone...................... 34 Basalt................................ 35 Petrographic detail of basalt...... 36 Ajgexjciv Jfrxuex Thickness of the pre-Cambrian formations.... 45 Paleozoic system............ 46 Troy quartzite........................ 46 Martin limestone...................... 48 Escabrosa and Naco limestones......... 49 Tertiary system............................. 51 Dacite conglomerate................... 51 Quaternary system........................... 53 Recent alluvium....................... 53 u’ ° Consolidated alluvium.............. 53 Unconsolidated alluvium............ 54 (ii) General geology - Continued. Igneous rooks. ............... .................... ...... 55 Diabase................................. 55 General character........... ...55 Petrographic detail of diabase ............... 57 Petrographic detail of altered diabase......59 Basaltic facies of diabase. .. ................ .61 Petrographic detail of basaltic facies......61 Petrographic detail of sericitized basalt...63 Contact metamorphism. .............................64 Age of the diabase... ................. .65 Andesite. ....... ..... ............... ............66 General character and age. ......... ..66 Petrographic detail of andesite.............67 Petrographic detail of albitized andesite...68 Contact me tamorphi sm. ............ 69 Quartz diorite. ........................ ....... 69 General character.... ..69 Petrographic detail of quartz diorite.......70 Petrographic detail of porphyritic diorite..72 Border facies of the quartz diorite.... ........74 Petrographic detail of diorite porphyry.... 74 Petrographic detail of porphyritic augite quartz diorite.. ........ ......... 75 Petrographic detail of porphyritic augite diorite.......... 76 Silicified Kornblende granite. ...... .........77 Complementary rocks............ 78 Andesite prophyry dike........... .78 Quartz monzonite porphyry dikes.............79 Porphyritic alkali granite dike.............80 Aplitic quartz monzoni te ........... ... 82 Hornblende granite ................... 83 Pel si te .............. .......... 84 Gabbro ........... 85 Petrographic detail of gabbro. ........... .85 Contact me tamorphi sm. ............ 87 Age of the quartz diorite.................... ...88 Silver King porphyry......... 89 General character. ......... ...... ....... ..... .89 Petrographic detail of Silver King porphyry.... ............................. .90 Contact me tamorphi sm. ........... ....95 Age of the porphyry ......... ....... .......... .96 Differentiation of the quartz diorite magma....... 96 The Central Arizona Batholith....... .97 Rhyolite tuff....... .98 General character.................................98 Petrographic detail of rhyolite tuff.......101 (ill) General geology - Continued Igneous rocks - Continued Dacite series.t *................................ 102 General character.............................. 102 Petrographic detail of rhyolite........... 103 Petrographic detail of dacite tuff........ 104 Petrographic detail of dacite............. 104 Age of the dacite series...................... 106 Andesite....................... 106 Petrographic detail of andesite........... 107 Structure...................... 108 Folding............................................ 109 Faulting........................................... 110 Geologic history...................................... 114 Economic geology......................................... 118 Discovery of the Silver King Mine................... 118 Development and production.......................... 120 The Silver King ore body................... 127 Microscopic study of the ores....................... 130 Introduction. ................................... 150 Criteria of ore mineral panagenesis............. 130 Textures indicating replacement......... 130 Textures indicating contemporaneity.......... 152 Graphic textures............................... 134 Identification methods...................... 136 Polarised light................................ 156 Etch tests................... 137 Micro chemical methods......................... 137 Description and par agenesis of minerals ......... 138 General statement....... 138 Hypo gene minerals............................. 138 Pyrite......................... 138 Sphalerite................ 139 Galena.................................... 139 Chalcopyrite and tetrahedrite............. 140 Bornite..................................... 141 Stromeyerite......... 142 Native silver............................... 142 Argentite.... '.................... ......... 143 Super gene minerals....................... 143 Stromeyerite................... 143 Massive chalcocite................ 146 Blue chalcocite........................... 147 Covellite........... ...'................... 147 Chalcopyrite.... ........ 148 Native silver.............................. 148 Cuprite.... ................... 149 Azurite and malachite............ 150 Angle site ........................ 150 Gangue minerals...... 150 Quart z ....... 150 Barite........................ 151 Calcite......................... 151 (It ) Economic geology - Continued The Apache Silver Mining Company’s prospect 152 (v) Outline of Report The Silver King mine, whose discovery opened up a large mineralized area previously overrun by hostile Apaches, produced nearly $7,000,000 in silver, nearly all of it be­ tween 1875 and 1889. Activity was intermittent in the years following, and at present a little work is being carried on to the east of the Silver King ground and there is talk of reopening the old mine, which is flooded. Sedimentary rocks.- The sedimentary rocks in the Silver King area range in age from pre-Cambrian to Recent. The Apache group, of Algonkian age, rests upon the Archeani':} Pinal schist, and is made up of the Scanlan conglomerate, Pioneer shale, Barnes conglomerate, Dripping Spring quartz­ ite and the Mescal limestone which is overlain by a thin basalt flow. Paleozoic rocks consist of the Cambrain Troy quartzite, Devonian Martin limestone, and Carboniferous Escabrosa and Naco limestones. No beds of Mesozoic age are present, in the area. The Tertiary segmentary rocks con­ sist of interbedded conglomerates, and tuffs. Local Quat­ ernary deposits of both consolidated and unconsolidated gravels are present. Intrusive igneous rocks.- There are three major in­ trusive bodies in the area. The oldest is diabase which occurs as thick sills in the pre-Cambrian formations and is probably of early Paleozoic age. A small stock of Tertiary (vi) quartz diorite is exposed over a large part of the area. Closely associated with the quartz diorite is a smaller stock of porphyritic quartz diorite locally known as the Silver King porphyry, as it was in this rock that the ore body of the Silver King mine was formed. Several varieties of complementary rocks are associated with the dioritie intrusives, and range in composition from.gabbro to alkali granite. Igneous rocks apparently not closely related to the quartz diorite are two ages of andesite. The whole igneous series may be considered as different phases in the history of what is known as the Central Arizona Batholith.
Recommended publications
  • 45. Myrmekite Formed by Na- and Ca-Metasomatism of K- Feldspar
    1 ISSN 1526-5757 45. Myrmekite formed by Na- and Ca-metasomatism of K- feldspar Jiashu RONG Beijing Research Institute of Uranium Geology P.O. Box 9818, Beijing, 100029 Peoples Republic of China Email address: [email protected] September 23, 2002 Abstract Myrmekite, an intergrowth of plagioclase and quartz vermicules, often occurs in felsic-to-intermediate, calc-alkalic plutonic and gneissic rocks. Several hypotheses for myrmekite genesis are briefly reviewed and discussed. The proportional relationship between the volume of quartz vermicules and the An value of plagioclase is consistent with the hypothesis or replacement, solid state exsolution, and recrystallization of primary plagioclase. (1) Perthitic albite and K- feldspar relicts in myrmekite and (2) swapped myrmekite between two differently oriented K-feldspar crystals obviously indicate that myrmekite is formed by nibble replacement of K-feldspar by myrmekitic plagioclase because of modification by Ca-bearing sodic emanation or fluid. Myrmekite of different morphology and spatial distribution are of the same metasomatic origin. The myrmekite that was produced during deformation should be later than that formed prior to deformation. Characteristics of myrmekite Myrmekite was first described by Michel-Lévy (1874) and named by Sederholm (1897) as an intergrowth of plagioclase and quartz vermicules. Myrmekite is commonly observed in felsic-to-intermediate calc-alkalic granitic rocks (but not in alkalic-tending plutonic rocks) and in granitic gneisses of similar composition. 2 On the basis of the geologic environment, Phillips (1974) classified myrmekite in the following ways: 1. rim myrmekite, occurring at the contact of plagioclase with another differently oriented K-feldspar; 2. intergranular myrmekite, situated at the boundary between two differently oriented K-feldspars; 3.
    [Show full text]
  • Structural Geology of the Upper Rock Creek Area, Inyo County, California, and Its Relation to the Regional Structure of the Sierra Nevada
    Structural geology of the upper Rock Creek area, Inyo County, California, and its relation to the regional structure of the Sierra Nevada Item Type text; Dissertation-Reproduction (electronic); maps Authors Trent, D. D. Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 27/09/2021 06:38:23 Link to Item http://hdl.handle.net/10150/565293 STRUCTURAL GEOLOGY OF THE UPPER ROCK CREEK AREA, INYO COUNTY, CALIFORNIA, AND ITS RELATION TO THE REGIONAL STRUCTURE OF THE SIERRA NEVADA by Dee Dexter Trent A Dissertation Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES In Partial Fulfillment of the Requirements For the Degree of DOCTOR OF PHILOSOPHY In the Graduate College THE UNIVERSITY OF ARIZONA 1 9 7 3 THE UNIVERSITY OF ARIZONA GRADUATE COLLEGE I hereby recommend that this dissertation prepared under my direction by __________ Dee Dexter Trent______________________ entitled Structural Geology of the Upper Rock Creek Area . Tnvo County, California, and Its Relation to the Regional Structure of the Sierra Nevada ________________ be accepted as fulfilling the dissertation requirement of the degree of ____________Doctor of Philosophy_________ ___________ P). /in /'-/7. 3 Dissertation Director fJ Date After inspection of the final copy of the dissertation, the following members of the Final Examination Committee concur in its approval and recommend its acceptance:* f t M m /q 2 g ££2 3 This approval and acceptance is contingent on the candidate's adequate performance and defense of this dissertation at the final oral examination.
    [Show full text]
  • A Crystal Size Distribution (CSD) Study of Microcline in the Cathedral Peak Granodiorite, Sierra Nevada, California
    Origin of megacrysts in granitoids by texturai coarsening: a crystal size distribution (CSD) study of microcline in the Cathedral Peak Granodiorite, Sierra Nevada, California MICHAEL D. HIGGINS Sciences de la Terre, Université du Québec à Chicoutimi, Chicoutimi, G7H 2Bl, Canada (e-mail: [email protected]) Abstract: Microcline megacrysts in the Cathedra! Peak Granodiorite and other parts of the Tuolumne Intrusive Suite were formed by texturai coarsening (Ostwald Ripening) of earlier formed crystals. The early-formed crystals nucleated and grew in an environment of increasing undercooling, probably during the ascent of the magma. Emplacement of the magma into warm host rocks promoted texturai coarsening. Crystals smaller than a certain size (the critical size) dissolved in the interstitial melt whilst larger crystals grew. Microcline was most sensitive to this effect as the magma temperature was buffered close to its liquidus for a long period by the release of latent heat of crystallization. Positive feedback between texturai coarsening and magma permeability channelled the flow of interstitial melt to produce a heterogeneous distribution of megacrysts. Megacryst growth was halted when cooling resumed at the end of the intrusive cycle. K-feldspar nucleation was then renewed and K-feldspar crystals grew to form part of the groundmass. lt was the particular thermal history of this pluton that promoted texturai coarsening-chemically similar plutons that lack megacrysts probably did not have the pause during cooling that was necessary for the development of this texture. Euhedral K-feldspar megacrysts up to 20 cm Swanson (1977) and Fenn (1977) measured the long are a striking and relatively common nucleation and growth rates of plagioclase, component of many granitoid plutons, but K-feldspar and quartz crystallizing from glassy their origin is still controversial.
    [Show full text]
  • 43. Myrmekite Formation at Temecula, California, Revisited: a Photomicrographic Essay Illustrating Replacement Textures
    1 ISSN 1526-5757 43. Myrmekite formation at Temecula, California, revisited: A photomicrographic essay illustrating replacement textures Lorence G. Collins and Barbara J. Collins Email: [email protected] May 18, 2002 Abstract A sequence of sixteen photomicrographs of thin sections of unaltered quartz diorite through a zone of deformation to myrmekite-bearing granite near Temecula, California, shows the textural and mineralogical changes that occurred in a quartz diorite as (1) K-metasomatism altered the primary plagioclase crystals to form microcline, myrmekite, quartz-bleb clusters, and recrystallized sodic plagioclase and as (2) Si-metasomatism converted microfractured biotite and hornblende into quartz. Cathodoluminescence, electron microprobe, and scanning electron studies confirm the chemical changes that occurred in the altered and recrystallized minerals. These photomicrographs and others (a) provide clues to the origin of metasomatic granitic in other terranes, (b) show that massive granite lacking gneissic fabric or cataclasis can be formed by K-metasomatism, (c) indicate that sharp contacts between mafic and felsic igneous rocks are not always caused by injection of magma into fractured rock, (d) reveal that complete cataclasis of all normally zoned plagioclase crystals in a mafic rock followed by K-metasomatism results in metasomatic granite lacking both normally zoned plagioclase and K- feldspar megacrysts, and (e) suggest that selective deformation of a few normally zoned plagioclase crystals in a primary rock can result in K-feldspar megacrysts coexisting with normally zoned plagioclase in granodiorite or quartz monzonite. Introduction This article is intended to be a supplement to articles http://www.csun.edu/~vcgeo005/Nr1Myrm.pdf and http://www.csun.edu/~vcgeo005/Nr2Myrm.pdf and to provide additional illustrations that show how myrmekite formed in the site near Temecula, California (Collins, 1988ab; Hunt et al., 1992).
    [Show full text]
  • Metamorphism and the Origin of Granitic Rocks Northgate District Colorado
    Metamorphism and the Origin of Granitic Rocks Northgate District Colorado GEOLOGICAL SURVEY PROFESSIONAL PAPER 274-M Metamorphism and the Origin of Granitic Rocks Northgate District Colorado By T. A. STEVEN SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 274-M A discussion of the progressive metamorphism, granitixation, and local rheomorphism of a layered sequence of rocks, and of the later emplacement and deuteric alteration of an unrelated granitic stock UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1957 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. CONTENTS Page Page Abstract_________________________________ 335 Pre-Cambrian geology—Continued Introduction-_______________________________________ 335 Dacite porphyry—____ ——— __ —— _____________ 364 Acknowledgments__ ___--_____-____-_____-______-_ 336 Intrusive quartz monzonite_-____--_-__-_--_-_-_. 365 Geologic setting._______ — _________________________ 336 Petrography ________—— —— _______________ 365 Pre-Cambrian geology—___________________________ 337 Main body of the stock____________— 366 Hornblende gneiss___-_________-_-_____-________ 338 Marginal dikes_________-____-__-__——— 366 Quartz monzonite gneiss_________________________ 342 Satellitic dikes___-___.__________ 367 Biotite-garnet gneiss___________________________ 345 Wall-rock alteration_________ _ __——_ 368 Pegmatite_________________________________
    [Show full text]
  • Chronology of Emplacement of Mesozoic Batholithic Complexes in California and Western Nevada by J
    Chronology of Emplacement of Mesozoic Batholithic Complexes In California and Western Nevada By J. F. EVERNDEN and R. W. KISTLER GEOLOGICAL SURVEY PROFESSIONAL PAPER 623 Prepared in cooperation with the University of California (Berkeley) Department of Geological Sciences UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1970 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Con;gress CSJtalog-card No. 7s-.60.38'60 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price $1.25 (paper cover) CONTENTS Page Abstract-------------------------------~---------------------------------------------------------------------- 1 Introduction--------------------------------------------------------------------------------~----------------- 1 Analyt:cal problems ____________________ -._______________________________________________________________________ 2 Analytical procedures______________________________________________________________________________________ 2 Precision and accuracy ___________________ -.- __ _ _ _ _ __ _ _ _ __ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 2 Potassium determinations_______________________________________________________________________________ · 2 Argon determinations--------~------------------~------------------------------------------------------ 5 Chemical and crystallographic effects on potassium-argon ages----------.-----------------------------------------
    [Show full text]
  • Myrmekite and Strain Weakening in Granitoid Mylonites
    Solid Earth Discuss., https://doi.org/10.5194/se-2018-70 Manuscript under review for journal Solid Earth Discussion started: 1 August 2018 c Author(s) 2018. CC BY 4.0 License. Myrmekite and strain weakening in granitoid mylonites Alberto Ceccato1*, Luca Menegon2, Giorgio Pennacchioni1, Luiz Fernando Grafulha Morales3 1 Department of Geosciences, University of Padova, 35131 Padova, Italy 2 School of Geography, Earth and Environmental Sciences, University of Plymouth, PL48AA Plymouth, UK 5 3 Scientific Centre for Optical and Electron Microscopy (ScopeM) - ETH Zürich, Switzerland Correspondence to: Alberto Ceccato ([email protected]) * Now at: School of Geography, Earth and Environmental Sciences, University of Plymouth, PL48AA Plymouth, UK Abstract. At mid-crustal conditions, deformation of feldspar is mainly accomplished by a combination of fracturing, dissolution/precipitation and reaction-weakening mechanisms. In particular, K-feldspar 10 is reaction-weakened by formation of strain-induced myrmekite - a fine-grained symplectite of plagioclase and quartz. Here we investigate with EBSD the microstructure of a granodiorite mylonite, developed at 420-460 °C during cooling of the Rieserferner pluton (Eastern Alps), to assess the microstructural processes and the role of weakening associated with myrmekite development. Our analysis shows that the crystallographic orientation of the plagioclase of pristine myrmekite was 15 controlled by that of the replaced K-feldspar. Myrmekite nucleation resulted in both grain size reduction and ordered phase mixing by heterogeneous nucleation of quartz and plagioclase. The fine grain size of sheared myrmekite promoted grain size-sensitive creep mechanisms including fluid- assisted grain boundary sliding in plagioclase, coupled with heterogeneous nucleation of quartz within creep cavitation pores.
    [Show full text]
  • 5. Myrmekite Formed by Exsolution?
    1 ISSN 1526-5757 5. MYRMEKITE FORMED BY EXSOLUTION? Lorence G. Collins email: [email protected] February 3, 1997 In order to remain open to other possibilities for the origin of myrmekite, I report the following two sites in this presentation in which bulbous myrmekite on the border of perthitic orthoclase is suggested by other investigators to form by exsolution. Weinsberg (Moldanubian) Granite, Austria At the first site, the Weinsberg (Moldanubian) granite and an older quartz- monzonite facies of the South Bohemian pluton in Austria both contain orthopyroxene and clinopyroxene and must have crystallized from magmas at high temperatures. The granite contains orthoclase megacrysts (as much as 10 to 20 cm long), which (1) are chemically zoned with Ba-rich cores (1 to 2 % mol Cs; and locally as much as 6 to 8 % Cs) and (2) are mineralogically zoned with aligned inclusions of plagioclase whose subhedral to euhedral faces are parallel to potential faces of the orthoclase (from illustrations at poster session, III Hutton Symposium, Koller and Kloetzli, 1995; personal communication, Koller, 1996). The megacrysts are perthitic and locally are bordered by small bulbous myrmekite with tiny quartz vermicules. Plagioclase lamellae are absent in the orthoclase adjacent to the myrmekite. The myrmekite is also associated with symplectic biotite which Koller and Kloetzli (1995) suggest is formed by the breakdown reaction orthopyroxene + K-feldspar + water = biotite + quartz. Discussion Koller (personal communication at the Hutton Symposium, 1995) suggested that the myrmekite bordering the orthoclase megacrysts was formed by exsolution. If that is true, it should have contrasting characteristics with myrmekite formed by K-metasomatism.
    [Show full text]
  • Origin of Myrmekite As It Relates to K-, Na-, and Ca-Metasomatism and the Metasomatic Origin of Some Granite Masses Where Myrmekite Occurs
    1 Origin of myrmekite as it relates to K-, Na-, and Ca-metasomatism and the metasomatic origin of some granite masses where myrmekite occurs. Lorence Gene Collins1 1Department of Geological Sciences, California State University Northridge, Northridge, CA 91330 Barbara Jane Collins2 2Department of Biology, California Lutheran University, Thousand Oaks, CA 91360 1email: [email protected] December 2013 Key words: metasomatism, K-feldspar, granite, myrmekite ABSTRACT Petrologists generally agree that granitic rocks form by crystallization from magma. Some granitic bodies, however, have been modified by alkali metasomatism at subsolvus temperatures (350-550°C). Myrmekite offers a petrographic means to detect the occurrence and conditions of alkali metasomatism in granitic rocks. Because metasomatic minerals inherit the hypidiomorphic textures of the former magmatic rocks, K-, Na-, and Ca-metasomatism may go unrecognized were it not for the additional presence of myrmekite in combination with other textural and mineralogical features, including microfractures, parallel alignments of silicate lattices and feldspar twin planes, quartz sieve-textures in ferromagnesian silicates, and sizes of quartz vermicules. Deformation is a precursor for myrmekite formation, but recrystallization may obliterate the deformation textures, so that myrmekite is the only remnant of prior deformation history. Crystals under stress develop a porosity that opens rocks to hydrous fluid that moves through the crystals and create a large-scale, coupled, dissolution-reprecipitation that totally modifies the rocks’ compositions. The loss of displaced Ca, Mg, Fe, and Al on a plutonic scale causes shrinkages as the residue becomes more granitic. The maximum width of the quartz vermicules in myrmekite correlates with the An content of the primary plagioclase being replaced that was once in the surrounding non-myrmekite-bearing relatively more-mafic rock.
    [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]
  • Deformation Conditions During Syn-Convergent Extension Along the Cordillera Blanca Shear Zone, Peru
    University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Earth and Planetary Sciences Publications and Other Works Earth and Planetary Sciences 6-13-2019 Deformation conditions during syn-convergent extension along the Cordillera Blanca shear zone, Peru Cameron A. Hughes University of Tennessee, Knoxville, [email protected] Michah J. Jessup University of Tennessee, Knoxville Colin A. Shaw Montana State, Bozeman Dennis L. Newell Utah State University Follow this and additional works at: https://trace.tennessee.edu/utk_eartpubs Recommended Citation Hughes, C.A., Jessup, M.J., Shaw, C.A., and Newell, D.L., 2019, Deformation conditions during syn- convergent extension along the Cordillera Blanca shear zone, Peru: Geosphere, v. 15, no. X, p. 1–26, https://doi.org/10.1130/GES02040.1. This Article is brought to you for free and open access by the Earth and Planetary Sciences at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Earth and Planetary Sciences Publications and Other Works by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. Research Paper GEOSPHERE Deformation conditions during syn-convergent extension along the Cordillera Blanca shear zone, Peru 1 1 2 3 GEOSPHERE, v. 15, no. X Cameron A. Hughes , Micah J. Jessup , Colin A. Shaw , and Dennis L. Newell 1Department of Earth and Planetary Sciences, University of Tennessee–Knoxville, 1621 Cumberland Avenue, 602 Strong Hall, Knoxville, Tennessee 37996-1526, USA 2Department of Earth Sciences, Montana State University, P.O. Box 173480, Bozeman, Montana 59717-3480, USA https://doi.org/10.1130/GES02040.1 3Department of Geology, Utah State University, 4505 Old Main Hill, Logan, Utah 84322, USA 11 figures; 3 tables; 1 set of supplemental files ■ ABSTRACT and Behr, 2011a; Sullivan et al., 2013; Spruzeniece and Piazolo, 2015).
    [Show full text]
  • 39. Scientific Errors That Can Result When Myrmekite and Geologic Evidence Are Ignored
    1 ISSN 1526-5757 39. Scientific errors that can result when myrmekite and geologic evidence are ignored Lorence G. Collins email: [email protected] April 18, 2001 Introduction The present studies of granitoid rocks from the 1980s into the year 2001 are dominantly directed toward chemical analyses and experimental and theoretical petrology rather than the determination of textures and petrography as seen in thin sections. Values for chemical studies of the granitoids are that they (a) support classifications into source types (S-I-A-M), (b) demonstrate liquid line of descent toward the temperature minimum of the Ab-Or-Qtz system, (c) enable the plotting of Harker diagrams of major oxides and spider diagrams of major and trace elements to show differentiation trends, (d) serve to discriminate among possible tectonic settings, and (e) provide data to enable the determination of ages by using various isotopes (Winter, 2001). For most granitoids this method of investigation is without reproach. However, when only chemical studies are used to study a granitoid, many changes in the solidified magmatic rocks may be hidden or unsuspected. Therefore, scientific errors in interpretation can result. Recent work suggests that where the granitoids contain rim and/or wartlike myrmekite, improper assumptions can be made concerning the complete history of these rocks (Collins website articles in http://www.csun.edu/~vcgeo005/index.html). Following solidification, deformation and modification by fluids containing K and Si can cause differentiation progressively toward the temperature minimum of the Ab-Or-Qtz system. This occurs because recrystallized minerals in granitic rocks formed by replacement processes below melting temperatures are stable there just as those formed from a melt.
    [Show full text]