By Verl Leon Smith a Thesis Submitted to the Faculty of Th

Total Page:16

File Type:pdf, Size:1020Kb

By Verl Leon Smith a Thesis Submitted to the Faculty of Th Hypogene alteration at the Esperanza Mine, Pima County, Arizona Item Type text; Thesis-Reproduction (electronic) Authors Smith, Verl Leon, 1943- 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 04/10/2021 11:08:00 Link to Item http://hdl.handle.net/10150/566585 HYPOGENE ALTERATION AT THE ESPERANZA MINE, PIMA COUNTY, ARIZONA "by Verl Leon Smith A Thesis Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE In the Graduate College THE UNIVERSITY OF ARIZONA 1 9 7 5 STATEMENT BY AUTHOR This thesis has "been submitted in partial fulfillment of re­ quirements for an advanced degree at The University of Arizona and is deposited in the University Library to be made available to borrowers under rules of the Library. Brief quotations from this thesis are allowable without special permission, provided that accurate acknowledgment of source is made. Requests for permission for extended quotation from or reproduction of this manuscript in whole or in part may be granted by the head of the major department or the Dean of the Graduate College when in his judg­ ment the proposed use of the material is in the interests of scholar­ ship. In all other instances, however, permission must be obtained from the author. APPROVAL BY THESIS DIRECTOR This thesis has been approved on the date shown below: Zf /?7j Date ACKNOWLEDGMENTS I wish to express appreciation to my thesis director, J . M . Guilhert, and other members of my committee and the faculty, especially D. E. Livingston, S. R. Titley, D. L. Norton, T. S. Lovering, T. M. Teska, and W. J. McLean for their guidance and assistance during my studies at The University of Arizona. I also wish to thank the many graduate students who have provided encouragement and assistance. I wish to thank the Duval Corporation for permission to undertake this study and for access to their property. Special thanks also to Duval geologists, C.D. lies and C. A. Oakley, for assistance during the initial phases of this project. I am especially grateful to the National Science Foundation for support, in the form of a graduate fellowship, which made this study and my graduate education possible. And thanks to Sandra for encouragement and patience. iii TABIfi OF CONTENTS Page LIST OF ILLUSTRATIONS....................................... vii LIST OF T A B I E S ................ x ABSTRACT ................................................... xi 1. INTRODUCTION ............................................. .. 1 M e t h o d s .......... ....................................... 1 Location and Setting ............................. 2 H i s t o r y .......... ................................ .. 4 Previous W o r k ........................................... ^ General Geologic S e t t i n g .............. ................ 5 Structural Setting ............ .. ..................... 6 2. PETROGRAPHY............................... ............. 8 Ox Frame V o l c a n i c s .......... 9 Volcanic Breccia ................................... 9 Quartzite........................................... 12 Rhyolite Tuff B r e c c i a ............ 12 Rhyolite Welded Tuff ............................. 15 Rhyolite and Quartz Latite Crystal Tuff . ........... 15 Leucodacite............................ 17 Biotite Quartz Diorite Porphyry.......... '............. 18 Biotite-Horhblende Andesite . ....................... 23 Rhyodacite Porphyry .......................... 25 Leuco-Quartz Diorite Porphyry .............. 31 Dacite Porphyry.................... 32 Quartz Monzonite Porphyry.................. 37 Miscellaneous Rock T y p e s .............. 48 Alaskite ........ ............ ....... 48 Rhyolite Porphyry ..... ......................... 50 A p l i t e ............................................. 51 3. ALTERATION PETROGRAPHY ............ 54 Pervasive Alteration ................................... j)4 Ox Frame Volcanics . ................ ..... ^4 Biotite Quartz Diorite Porphyry ..................... 57 Rhyodacite Porphyry . ............................... 58 Leuco-Quartz Diorite Porphyry ....................... 60 Quartz Monzonite Porphyry ........................... 60 iv V T A M E OF CONTENTS —Continued Page Orthoclase Metasomatite . ........................... 63 Veinlets and Veinlet Controlled Alteration ....... 69 Orthoclase Veinlets ..... ....................... 69 Orthoclase Veinlets in Biotite Quartz Diorite P o r p h y r y .............. ........................ 70 Orthoclase Veinlets in Quartz Monzonite Porphyry 7^ Orthoclase Veinlets in Other Rock T y p e s ........ 75 Alhite Veinlets.................. .............. .. • 75 AlMte Veinlets in Biotite Quartz Diorite P o r p h y r y ................ .......... ............ 75 Alhite Veinlets in Quartz Monzonite Porphyry . 76 Leuco-Quartz D i o r i t e ........................... 77 Quartz-Molybdenite Veinlets ......................... 77 Quartz-Pyrite-Sericite Veinlets . ............. 77 Sericite-C hlorite-Sulfide V e i n l e t s ............ 79 Gypsum Veinlets.................. .................. 81 Supergene Effects ....................................... 82 Fluid Inclusions .......... ....... 82 Summary of Alteration ........ ....... .......... 83 Veinlet D i s t r i b u t i o n ............................... 86 Correlation of Alteration and Mineralization .... 88 Correlation of Mineralization and Rock T y p e ........ 91 4. CHEMICAL DATA ............................................... 92 Major Element Variation ................................. 92 Ca-K-Na Plots ....................................... 97 ACF-AKF P l o t s .........................'.............. 97 Normative Qz-Or-Pl Plots ....................... 105 Minor Elements . ............................. 107 Microprote Data ............................... Ill 5. X-RAY D A T A ..................................... 118 Muscovite Polymorphs .................................... 118 Structural State of Potassium Feldspars . ............... 118 Composition of Potassium F e l d s p a r s ..................... 120 6. INTERPRETATIONS OF THE ALTERATION-MINERALIZATION SYSTEM AT E S P E R A N Z A .................... 122 Backgroundt The Proposed Models ....................... 122 The Ortho-Magmatic M o d e l ........................... 123 The Circulating Meteoric Fluid Model ........ 123 Combination of Models ..... ..................... 124 Vi TABLE OF CONTENTS— Continued Page Interpretation of Alteration Assemblages ............... 124 Biotitization and Orthoclase-Ghlorite Alteration in the Biotite Quartz D i o r i t e ....................... 124 Orthoclase-C hlorite Alteration in the Leucocratic R o c k s ....................................... 131 Altite and Alhite Veining ........................... 132 Final Stages of the Alteration S y s t e m .............. 133 Rock Type Control on Alteration-Mineralization . 135 Zoning of Alteration ............................... 139 Summary of the Alteration S y s t e m ....................... 140 Suggestions for Further Work ......... ........ 142 APPENDIX A: RESULTS OF CHEMICAL ANALYSES ................... 144 APPENDIX Bj X-RAY FLUORESCENCE ANALYTICAL AND DATA REDUCTION TECHNIQUES........................... 150 REFERENCES ................................................. 155 LIST OF ILLUSTRATIONS Figure Page 1. Index map showing location of Esperanza and Sierrita Mines . ......................................... 3 2. Generalized rock distribution map, Esperanza Mine .... 10 3* Sample location map, Esperanza Mine ...... ........ 11 4. Modal Qz-Or-Pl for Ox Frame Volcanics .................. 14 5 . Texture of rhyolite welded tuff ......................... 16 6. Texture of rhyolite crystal tuff ......................... 16 7 . Modal Qz-Or-Pl for biotite quartz diorite .............. 21 8. Biotite cluster with relict hornblende in biotite quartz diorite .................. ....... ........ 22 9. Texture of hornblende a n desite......................... ,, 24 ■> 10. Rapakivi feldspar megacryst in rhyodacite porphyry .... ; 26 11. Modal Qz-Or-Pl for rhyodacite porphyry . ................ 29 12. Texture of rhyodacite p o rphyry........................... 30 13* Detail of rapakivi feldspar in rhyodacite porphyry .... 30 14. Modal Qz-Or-Pl for leuco-quartz diorite porphyry ........ 34 15• Texture of leuco-quartz diorite porphyry ................ 35 16. Matrix of leuco-quartz diorite porphyry ................ 36 17 • Matrix of leuco-quartz diorite porphyry within orthoclase veinlet envelope ................ ...... 36 18. Dacite porphyry matrix ................................. .. 38 19* Texture of "western" quartz monzonite po rphyry.......... 44 20. Plumose granophyre ........................................ 44 vii viii U S T £F ILLUSTRATIONS —Continued Figure Page 21. Texture of "eastern” quartz monzonite porphyry.......... 46 22. Detail of rapaJcivi feldspar in quartz monzonite p o rphyry................................................. 4? 23• Modal Qz-Or-Pl for quartz monzonite porphyry........... 49 24. Diagrammatic veinlet relations........... 55 25* Schematic paragenesis of alteration and veinlet minerals................................. ................ 56 26. Irregular biotite clots in biotite quartz diorite
Recommended publications
  • Part 629 – Glossary of Landform and Geologic Terms
    Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition.
    [Show full text]
  • Schists of the Central Alaska Range
    Schists of the Central Alaska Range By CLYDE WAHRHAFTIG CONTRIBUTIONS TO STRATIGRAPHY GEOLOGICAL SURVEY BULLETIN 1254-E Distribution of schists within Fairbanks A-2, A-3, and A-4 quadrangles and Healy 0-2, 0-3, and 0-4 quadrangles UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1968 UNITED STATES DEPARTMENT OF THE INTEKIOK STEWART I,. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington. D.C. 20402 - Price 15 cents (paper cover) CONTENTS Page Abstract-..---------------------..-----..-----.----------------------- E 1 Introduction---------..-------------------------------------------- General structural and areal relations- - _ _------ ----..-- ------------ --- Birch Creek Schist----___--_-_------------------------------------- Keevy Peak Formation ............................................. Totatlanika Schist-----__--_-_------------------------------------- Moose Creek Member ----_--------------- ...................... California Creek Member ..................... --- ---------- -- -- - Chute Creek, Mystic Creek, and Sheep Creek Members ------------ Age and origin of the Totatlanika Schist -------- ----__-------- -- --- Metavolcanio schists and associated rocks south of the Birch Creek Schist- References cited-___--_-_-__--------------------------------------- ILLUSTRATIONS Page FIGURE1. Index map of Alaska _----_____---------------------------E3 2. Generalized geologic map of part of the central Alaska Range- Fairbanks A-2, A-3, and
    [Show full text]
  • The Steep Nap Prospect: a Low-Sulphidation, Gold-Bearing Epithermal Vein System of Late Neoproterozoic Age, Avalon Zone, Newfoundland Appalachians
    Current Research (1999) Newfoundland Department of Mines and Energy Geological Survey, Report 99-1, pages 255-274 THE STEEP NAP PROSPECT: A LOW-SULPHIDATION, GOLD-BEARING EPITHERMAL VEIN SYSTEM OF LATE NEOPROTEROZOIC AGE, AVALON ZONE, NEWFOUNDLAND APPALACHIANS J. Mills, S.J. O'Brien1, B. DubJ2, R. Mason and C.F. O'Driscoll3 Memorial University of Newfoundland ABSTRACT The Steep Nap Prospect is a vein- and breccia-hosted, low-sulphidation style, epithermal gold–silver occurrence of late Neoproterozoic age. It is situated at the northern end of a 15-km-long hydrothermal alteration zone (the eastern Avalon high- alumina belt), within the eastern part of Newfoundland Avalonian belt. Precious-metal mineralization occurs in a nonwelded tuff unit located near the upper part of a thick, subaerial, caldera-facies volcanic succession of 580 to 570 Ma ash-flow tuffs, rhyolite domes and in-situ breccias, and coarse-grained pyroclastic breccia. The low-sulphidation mineralization, and the adjacent altered rocks of the high-alumina belt, are overlain unconformably by Lower Cambrian shales. The prospect includes both crustiform–colloform-textured quartz–adularia–hematite veins (typically auriferous) and comb-textured quartz–hematite veins (typically barren). Early quartz–adularia-bearing, crustiform- and cockade-textured breccia carries gold. Later breccias are auriferous only where they contain fragments of crustiform veins. Textural and min- eralogical data indicate that the crustiform veins and breccias formed within the precious-metal section of the host epither- mal system, above the boiling level, from near-neutral-pH hydrothermal fluids. A strong positive correlation exists between elevated gold values and the presence of (1) adularia, and (2) recrystallization and replacement textures.
    [Show full text]
  • Analyses of Rocks and Minerals
    UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director / rf Bulletin 878 ANALYSES OF ROCKS AND MINERALS FROM THE LABORATORY OF THE UNITED STATES GEOLOGICAL SURVEY 1914-36 TABULATED BY ROGER C. WELLS Chief Chemist UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1937 For sale by the Superintendent of Documents, Washington, D. C. ------ Price 15 cents V CONTENTS Page Introduction._____________________________________________________ 1 The elements and their relative abundance.__________________________ 3 Abbreviations used._______________________________________________ 5 Classification.___________________________________________________ 5 Analyses of igneous and crystalline rocks____-_________.._____________ 6 Alaska._____-_____-__________---_-_--___-____-_____-_________ 6 \ Central Alaska________________________________________ 6 Southeastern Alaska___________-_--________________________ 7 Arizona._________--____-_---_-------___-_--------_----_______ 8 Ajo district.-_--_.____---------______--_-_--__---_______ 8 Oatman district____________-___-_-________________________ 9 Miscellaneous rocks....-._...._-............_......_._.... 10 Arkansas.____________________________________________________ 11 Austria._____________________________________________________ 11 California.__,_______________--_-_----______-_-_-_-___________ 11 T ' Ivanpah quadrangle.____-_----__--_____----_--_--__.______ 11 Lassen Peak__________________ ___________________________ 12 Mount Whitney quadrangle________________________________
    [Show full text]
  • Preliminary Model of Porphyry Copper Deposits
    Preliminary Model of Porphyry Copper Deposits Open-File Report 2008–1321 U.S. Department of the Interior U.S. Geological Survey Preliminary Model of Porphyry Copper Deposits By Byron R. Berger, Robert A. Ayuso, Jeffrey C. Wynn, and Robert R. Seal Open-File Report 2008–1321 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia: 2008 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Berger, B.R., Ayuso, R.A., Wynn, J.C., and Seal, R.R., 2008, Preliminary model of porphyry copper deposits: U.S. Geological Survey Open-File Report 2008–1321, 55 p. iii Contents Introduction.....................................................................................................................................................1 Regional Environment ...................................................................................................................................3
    [Show full text]
  • Glossary of Geological Terms
    GLOSSARY OF GEOLOGICAL TERMS These terms relate to prospecting and exploration, to the regional geology of Newfoundland and Labrador, and to some of the geological environments and mineral occurrences preserved in the province. Some common rocks, textures and structural terms are also defined. You may come across some of these terms when reading company assessment files, government reports or papers from journals. Underlined words in definitions are explained elsewhere in the glossary. New material will be added as needed - check back often. - A - A-HORIZON SOIL: the uppermost layer of soil also referred to as topsoil. This is the layer of mineral soil with the most organic matter accumulation and soil life. This layer is not usually selected in soil surveys. ADIT: an opening that is driven horizontally (into the side of a mountain or hill) to access a mineral deposit. AIRBORNE SURVEY: a geophysical survey done from the air by systematically crossing an area or mineral property using aircraft outfitted with a variety of sensitive instruments designed to measure variations in the earth=s magnetic, gravitational, electro-magnetic fields, and/or the radiation (Radiometric Surveys) emitted by rocks at or near the surface. These surveys detect anomalies. AIRBORNE MAGNETIC (or AEROMAG) SURVEYS: regional or local magnetic surveys that measures deviations in the earth=s magnetic field and carried out by flying a magnetometer along flight lines on a pre-determined grid pattern. The lower the aircraft and the closer the flight lines, the more sensitive is the survey and the more detail in the resultant maps. Aeromag maps produced from these surveys are important exploration tools and have played a major role in many major discoveries (e.g., the Olympic Dam deposit in Australia).
    [Show full text]
  • Application of U–Pb, Ar/ Ar and (U–Th)/He Chronometers, Bajo
    Miner Deposita (2008) 43:295–314 DOI 10.1007/s00126-007-0151-5 ARTICLE Multimillion year thermal history of a porphyry copper deposit: application of U–Pb, 40Ar/39Ar and (U–Th)/He chronometers, Bajo de la Alumbrera copper–gold deposit, Argentina Anthony C. Harris & W. James Dunlap & Peter W. Reiners & Charlotte M. Allen & David R. Cooke & Noel C. White & Ian H. Campbell & Suzanne D. Golding Received: 17 July 2006 /Accepted: 4 June 2007 /Published online: 16 August 2007 # Springer-Verlag 2007 Abstract Application of multiple chronometers (including spans millions of years. Previous U–Pb geochronology, U–Pb and 40Ar/39Ar geochronology and zircon and apatite combined with our new 40Ar/39Ar data, shows that the (U–Th)/He thermochronology) to porphyry intrusions at the multiple porphyritic intrusions at Bajo de la Alumbrera Bajo de la Alumbrera porphyry copper–gold deposit, were emplaced during two episodes, the first at about Argentina, reveals a complex history of reheating that 8.0 Ma (P2 and associated porphyries) and the second about a million years later (Early and Late P3 porphyries). Complex overprinting alteration events have obscured the Editiorial handling: L. Meinert earliest hydrothermal history of the deposit. By contrast, Electronic supplementary material The online version of this article 40Ar/39Ar data reveal the close temporal relationship of ore- (doi: 10.1007/s00126-007-0151-5) contains supplementary material, bearing potassic alteration assemblages (7.12±0.13 Ma; which is available to authorized users. : : biotite) to the emplacement of the P3 intrusions. Consistent A. C. Harris (*) D. R. Cooke N. C. White with low closure temperatures, younger ages have been de- CODES ARC Centre of Excellence in Ore Deposits, termined for associated hydrothermal alkali feldspar (6.82± University of Tasmania, 7001 Hobart, Australia 0.05 Ma and 6.64±0.09 Ma).
    [Show full text]
  • Nomenclature of the Micas
    Mineralogical Magazine, April 1999, Vol. 63(2), pp. 267-279 Nomenclature of the micas M. RIEDER (CHAIRMAN) Department of Geochemistry, Mineralogy and Mineral Resources, Charles University, Albertov 6, 12843 Praha 2, Czech Republic G. CAVAZZINI Dipartimento di Mineralogia e Petrologia, Universith di Padova, Corso Garibaldi, 37, 1-35122 Padova, Italy Yu. S. D'YAKONOV VSEGEI, Srednii pr., 74, 199 026 Sankt-Peterburg, Russia W. m. FRANK-KAMENETSKII* G. GOTTARDIt S. GUGGENHEIM Department of Geological Sciences, University of Illinois at Chicago, 845 West Taylor St., Chicago, IL 60607-7059, USA P. V. KOVAL' Institut geokhimii SO AN Rossii, ul. Favorskogo la, Irkutsk - 33, Russia 664 033 G. MOLLER Institut fiir Mineralogie und Mineralische Rohstoffe, Technische Universit/it Clausthal, Postfach 1253, D-38670 Clausthal-Zellerfeld, Germany A. M, R. NEIVA Departamento de Ci6ncias da Terra, Universidade de Coimbra, Apartado 3014, 3049 Coimbra CODEX, Portugal E. W. RADOSLOVICH$ J.-L. ROBERT Centre de Recherche sur la Synth6se et la Chimie des Min6raux, C.N.R.S., 1A, Rue de la F6rollerie, 45071 Od6ans CEDEX 2, France F. P. SASSI Dipartimento di Mineralogia e Petrologia, Universit~t di Padova, Corso Garibaldi, 37, 1-35122 Padova, Italy H. TAKEDA Chiba Institute of Technology, 2-17-1 Tsudanuma, Narashino City, Chiba 275, Japan Z. WEISS Central Analytical Laboratory, Technical University of Mining and Metallurgy, T/'. 17.1istopadu, 708 33 Ostrava- Poruba, Czech Republic AND D. R. WONESw * Russia; died 1994 t Italy; died 1988 * Australia; resigned 1986 wUSA; died 1984 1999 The Mineralogical Society M. RIEDER ETAL. ABSTRACT I I End-members and species defined with permissible ranges of composition are presented for the true micas, the brittle micas, and the interlayer-deficient micas.
    [Show full text]
  • OHIO STATE UNIVERSITY a Ttlesis SUBMITTED in PARTIAL FULFILLMENT of T.Tle REQUIREMENTS for the DEGREE OF
    OHIO STATE UNIVERSITY An Investigation of a Selected Group of Cataclastically Deformed Rocks by Petrographic and ~-Ray Diffraction Methods by Gary A. Lurxi A TtlESIS SUBMITTED IN PARTIAL FULFILLMENT OF T.tlE REQUIREMENTS FOR THE DEGREE OF BACHELOR OF SCIENCE Senior Thesis Advisor Dr. John F. Sutter Columbus, Ohio May, 1972 ABSTRACT AN INVESTIGATION OF A SELECTED GROUP OF CATACLASTICALLY DEFOR1'1ED ROCiS BY PETROGRAPHIC AND ~-RAY DIFFRACTION METHODS Gary A. Lund A suite of rocks from the Kings Canyon Shear Zone, located in the Northgate fluorspar district in Jackson county, Colorado, was made available for study by Dr. John F. Sutter, Ohio State University. The investigation of these rocks was limited to the mineralogical and textural changes observed by the use of the petrographic microscope and by 1:..-ray diffraction. Previous studies by Dr. Sutter have been mainly concerned with K/Ar age dating and the geochemistry of these cataclastically deformed rocks. His findings show a decrease in apparent age of tt1e rock from both sides of the shear zone toward the center, and he attributes this to increasing neomineralization toward the center of the shear zone. The samples of cataclastic rock in the suite are, for the most part, derived from a common parent rock type, a hornblende gneiss. The rocks sampled occur at various locations within the shear zone, and they exhibit very well the changing degrees of cataclastic degradation such as granula­ tion, recrystallization, and neomineralization. Intergranular and intra­ granular strain features are apparent in all the samples. Three samples, which occur in the central portion of the shear zone, have a very different texture, mineralogy, and chemistry than the other samples of cataclastic rock in the shear zone.
    [Show full text]
  • George E. Ericksen US Geological
    UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY NEOGENE-QUATERNARY VOLCANISM AND MINERALIZATION IN THE CENTRAL ANDES by George E. Ericksen U.S. Geological Survey, Reston, Va.; V. Raul Eyzaguirre, Lima, Peru; Fernando Urquidi B., American Embassy, La Paz, Bolivia; and Raul Sal as 0., Servicio Nacional de Geologia y Mineria, Santiago, Chile Open-File Report 87- 634 1987 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards ILLUSTRATIONS Page 1. Distribution of Neogene-Quaternary volcanic rocks in the central Andes .............................................. 1A 2. Known and inferred calderas in the central Andes ........... 3A 3. Distribution of metalliferous deposits associated with stratovolcanos and calderas in the central Andes ........... 12A 4. Distribution of native sulfur deposits associated with stratovolcanos in Bolivia and Chile ........................ 15A 5. Distribution of metalliferous deposits associated with dome complexes and with altered vent zones, breccias pipes, and thermal-spring systems not related to known volcanic land- forms ...................................................... 20A Tables Page Table 1. Mineral deposits associated with Neogene-Quaternary volcanic centers in the central Andes....................... 8A ABSTRACT Eruptive centers, which include calderas, stratovolcanos, and flow-dome complexes in the Neogene-Quaternary volcanic complex of the central Andean region of northwestern Argentina, western Boliva, northern Chile, and southern Peru, are potential targets for hydrothermal mineral deposits. This volcanic complex, consisting chiefly of rhyolitic ash-flow tuffs and andesitic lavas, p p extends over an area of about 300,000 knr within a 1,000,000 km area that is one of the world's great mineral provinces. Because many deposits of Cu, Pb, Zn, Sn, W, Sb, Bi, Ag, and Au in this area are of pre-Pliocene age, it had been believed that most of the Neogene-Quaternary volcanic rocks represented post-mineralization cover.
    [Show full text]
  • Clay Minerals in Hydrothermal Systems
    minerals Review Clay Minerals in Hydrothermal Systems Paolo Fulignati Dipartimento di Scienze della Terra, University of Pisa, Via S. Maria 53, 56126 Pisa, Italy; [email protected] Received: 24 August 2020; Accepted: 14 October 2020; Published: 16 October 2020 Abstract: The study of active and fossil hydrothermal systems shows clay minerals to be a fundamental tool for the identification and characterization of hydrothermal alteration facies. The occurrence and composition of hydrothermal alteration facies could provide useful information on the physicochemical conditions of the hydrothermal activity affecting a rock volume. In particular, clay minerals (i.e., smectite group, chlorite, illite, kaoline group, pyrophyllite, biotite) are pivotal for extrapolating important parameters that strongly affect the development of water/rock interaction processes such as the temperature and pH of the hydrothermal environment. This work aims to give a general reference scheme concerning the occurrence of clay minerals in hydrothermal alteration paragenesis, their significance, and the information that can be deduced by their presence and chemical composition, with some examples from active and fossil hydrothermal systems around the world. The main mineralogical geothermometers based on chlorite and illite composition are presented, together with the use of hydrogen and oxygen isotope investigation of clay minerals in hydrothermal systems. These techniques provide a useful tool for the reconstruction of the origin and evolution of fluids involved in hydrothermal alteration. Finally, a list of oxygen and hydrogen fractionation factor equations between the main clay minerals and water is also provided. Keywords: clay minerals; hydrothermal alteration; hydrothermal mineralogical paragenesis; geothermometers 1. Introduction A volume of rock, when affected by hydrothermal fluid circulation, typically undergoes a variety of alteration processes.
    [Show full text]
  • Arizona Geological Survey | 2Mcdowell Sonoran Field Institute
    QUARTZ VEIN INVESTIGATION, MCDOWELL SONORAN PRESERVE, SCOTTSDALE, MARICOPA COUNTY, ARIZONA Brian F. Gootee1 & Daniel G. Gruber2 1Arizona Geological Survey | 2McDowell Sonoran Field Institute State geological survey employees collecting geothermal data. OPEN-FILE REPORT OFR-15-03 July 2015 Arizona Geological Survey www.azgs.az.gov | repository.azgs.az.gov Arizona Geological Survey M. Lee Allison, State Geologist and Director Manuscript approved for publication in July 2015 Printed by the Arizona Geological Survey All rights reserved For an electronic copy of this publication: www.repository.azgs.az.gov Printed copies are on sale at the Arizona Experience Store 416 W. Congress, Tucson, AZ 85701 (520.770.3500) For information on the mission, objectives or geologic products of the Arizona Geological Survey visit www.azgs.az.gov. This publication was prepared by an agency of the State of Arizona. The State of Arizona, or any agency thereof, or any of their employees, makes no warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed in this report. Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the State of Arizona. ___________________________ Recommended Citation: Gootee, B.F. and Gruber, D.G., 2015, Quartz vein investigation, McDowell Sonoran Preserve, Scottsdale, Maricopa County, Arizona. Arizona Geological Survey Open File Report,
    [Show full text]