The Evolution of Supergene Enrichment in the Morenci
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Download PDF About Minerals Sorted by Mineral Name
MINERALS SORTED BY NAME Here is an alphabetical list of minerals discussed on this site. More information on and photographs of these minerals in Kentucky is available in the book “Rocks and Minerals of Kentucky” (Anderson, 1994). APATITE Crystal system: hexagonal. Fracture: conchoidal. Color: red, brown, white. Hardness: 5.0. Luster: opaque or semitransparent. Specific gravity: 3.1. Apatite, also called cellophane, occurs in peridotites in eastern and western Kentucky. A microcrystalline variety of collophane found in northern Woodford County is dark reddish brown, porous, and occurs in phosphatic beds, lenses, and nodules in the Tanglewood Member of the Lexington Limestone. Some fossils in the Tanglewood Member are coated with phosphate. Beds are generally very thin, but occasionally several feet thick. The Woodford County phosphate beds were mined during the early 1900s near Wallace, Ky. BARITE Crystal system: orthorhombic. Cleavage: often in groups of platy or tabular crystals. Color: usually white, but may be light shades of blue, brown, yellow, or red. Hardness: 3.0 to 3.5. Streak: white. Luster: vitreous to pearly. Specific gravity: 4.5. Tenacity: brittle. Uses: in heavy muds in oil-well drilling, to increase brilliance in the glass-making industry, as filler for paper, cosmetics, textiles, linoleum, rubber goods, paints. Barite generally occurs in a white massive variety (often appearing earthy when weathered), although some clear to bluish, bladed barite crystals have been observed in several vein deposits in central Kentucky, and commonly occurs as a solid solution series with celestite where barium and strontium can substitute for each other. Various nodular zones have been observed in Silurian–Devonian rocks in east-central Kentucky. -
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Tne AMBRrcAx M rNBRALocrsr JOURNAL OF THE MINERALOGICAL SOCIETY OF AMERICA Vol.20 NOVEMBER, 1935 No. 11 THE PEGMATITE MINERALS FROM NEAR AMELIA, VIRGINIA* Jnwrr.r. J. Gless, U. S. Geological'Suraey, Washington, D. C. CoNrnxrs 1' rntroduction 741 2. Rutherfordmine 743 3' Morefield mine ' ' 744 4. Minerals 745 Albite, bertrandite, beryl, biotite, calcite, cassiterite, cerussite, chalcopy- rite, fluorite, galena, manganotantalite, microcline, microlite, monazite, muscovite, phenacite, pyrite, pyrolusite, qtsartz, spessartite, topaz, tourmaline, triplite, zinnwaldite, zircon. 5. Rarer elements identified by spectrographic analyses 764 6. Luminescence of minerals 766 7. Selected bibliography 768 1. INTnooucrroN The first commercial mica mines near Amelia Court House, Virginia, were opened in the early seventies, and the remarkable size and quality of the mica early awakened a keen economic in- terest in the pegmatite dikes of the region, but the richnessof the locality in rare and beautiful mineral specimenshas promoted a scientific interest which has persisted for sixty years. Thirty-six mineral species have been reported from the Rutherford mine alone,and the variety and perfection of many of thesehave led to their inclusion in most of the museums of the world. The concen- tration of unusual minerals in an easily accessible deposit at- tracted various scientific investigators and mineral collectors to this locality for successivegenerations. Such intensive investiga- tion of a locality might suggest that little remains to be learned about its minerals, but the recent opening of a new mine near Amelia and the reopening of the Rutherford mine have given new * Published by permission of the Director, U. S. Geological Survey. 742 THE AMERICAN MINERALOGIST opportunities for study. -
PHASE CHANGES in Cu 2 S AS a FUNCTION of TEMPERATURE 1. PREVIOUS WORK
National Bureau of Standards Special Publication 364, Solid State Chemistry, Proceedings of 5th Materials Research Symposium, issued July 1972. PHASE CHANGES IN cu2s AS A FUNCTION OF TEMPERATURE William R. Cook, Jr. Gould Inc., Gould Laboratories Cleveland, Ohio 44108 and Case Western Reserve University Cleveland, Ohio 44106 The high-'copper phase boundary of Cu2s deviates from stoichiometry above 300 °C, first becoming copper deficient, then above - 1075 °C becoming copper rich. The maximum copper content occurs at the monotectic temperature of 1104 °C. The strong effect of oxygen on the hexagonal-cubic transition in Cu2S was confirmed; the transition was also found to be sensi tive to the type of pretreatment of the material. The high temperature tetragonal "Cu1 96s" phase is stable between Cu1.95S and Cu2s, at temperatures of - 90° to - 140 °C. The tr~nsi tion to the tetragonal phase is extremely sluggish. The true composition of djurleite has been shown to be approximately Cu1.93S. The phases near the chalcocite-digenite region of the diagram may be grouped into those with hexagonal close packing of sulfur atoms and those with cubic close packing of sulfurs. This is important in understanding rates of transformation among the various phases that occur in this area of the diagram. Key words: Chalcocite; cu2s; digenite; djurleite; nonstoichiometry; phase relations. 1. PREVIOUS WORK Fairly thorough explorations of the Cu-s phase diagram between cu2s and cu1• ,shave been made by a number of previous workers [1-8] 1 The resulting diagram may be seen in figure 1 taken largely from Roseboom [7] and Riu [8]. -
A Classification of Riparian Wetland Plant Associations of Colorado a Users Guide to the Classification Project
A Classification of Riparian Wetland Plant Associations of Colorado A Users Guide to the Classification Project September 1, 1999 By Gwen Kittel, Erika VanWie, Mary Damm, Reneé Rondeau Steve Kettler, Amy McMullen and John Sanderson Clockwise from top: Conejos River, Conejos County, Populus angustifolia-Picea pungens/Alnus incana Riparian Woodland Flattop Wilderness, Garfield County, Carex aquatilis Riparian Herbaceous Vegetation South Platte River, Logan County, Populus deltoides/Carex lanuginosa Riparian Woodland California Park, Routt County, Salix boothii/Mesic Graminoids Riparian Shrubland Joe Wright Creek, Larimer County, Abies lasiocarpa-Picea engelmannii/Alnus incana Riparian Forest Dolores River, San Miguel County, Forestiera pubescens Riparian Shrubland Center Photo San Luis Valley, Saguache County, Juncus balticus Riparian Herbaceous Vegetation (Photography by Gwen Kittel) 2 Prepared by: Colorado Natural Heritage Program 254 General Services Bldg. Colorado State University Fort Collins, CO 80523 [email protected] This report should be cited as follows: Kittel, Gwen, Erika VanWie, Mary Damm, Reneé Rondeau, Steve Kettler, Amy McMullen, and John Sanderson. 1999. A Classification of Riparian Wetland Plant Associations of Colorado: User Guide to the Classification Project. Colorado Natural Heritage Program, Colorado State University, Fort Collins, CO. 80523 For more information please contact: Colorado Natural Heritage Program, 254 General Service Building, Colorado State University, Fort Collins, Colorado 80523. (970) -
Gomposition and Occurrence of Electrum Atthe
L37 The Canadian M inerala g i st Vol.33,pp. 137-151(1995) GOMPOSITIONAND OCCURRENCEOF ELECTRUM ATTHE MORNINGSTAR DEPOSIT, SAN BERNARDINOCOUNTY, GALIFORNIA: EVIDENCEFOR REMOBILIZATION OF GOLD AND SILVER RONALD WYNN SIIEETS*, JAMES R. CRAIG em ROBERT J. BODNAR Depanmen of Geolngical Sciences, Virginin Polytechnic h stitate and Stale (Jniversity, 4A44 Dening Hall, Blacl<sburg, Virginin 24060, U.S-A,. Arsrnacr Elecfum, acanthiteand uytenbogaardtite have been examined from six depthswithin the tabular quartzt calcite sockwork and breccia-filled veins in the fault-zone-hostedMorning Star depositof the northeasternMojave Desert, Califomia. Six distinct types of electrum have been identified on the basis of minerat association,grain moryhology and composition. Two types, (1) p1'rite-hostedand (2) quartz-hostedelectrum, occur with acanthite after argentite and base-metalsulfide minerals in unoxidized portions of the orebody; the remaining forr types, (3) goethite-hostedelectrum, (4) electnrm cores, (5) electrumrims and (6) wire electrum,are associatedwith assemblagesof supergeneminerals in its oxidizedportions. Pyrite- hosted quartz-hostedand goethite-hostedelectrum range in compositionfrom 6l ta 75 utt.7oAu and have uniform textures and no zoning. In lower portions ofthe oxidized ore zone, electrum seemsto replacegoethite and occursas small grains on surfacesof the goethite.Textural evidencefavors supergeneremobilization of Au and Ag, which were depositedas electrum on or replacinggoethite. This type of electrumis identical in appearanceand compositionto prinary electrum,In the upper portions of the oxidized zone,secondary electum occursas a gold-rich rim on a core of elechum and as wire-like grains,both with acanthiteand uytenbogaardtite.Such secondaryelectrum contains from 78 to 93 wt./o Au. Textural relations and asso- ciated minerals suggestthat the primary electrum was hydrothermally depositedand partially remobilized by supergene processes. -
Southwest NM Publication List
Southwest New Mexico Publication Inventory Draft Source of Document/Search Purchase Topic Category Keywords County Title Author Date Publication/Journal/Publisher Type of Document Method Price Geology 1 Geology geology, seismic Southwestern NM Six regionally extensive upper-crustal Ackermann, H.D., L.W. 1994 U.S. Geological Survey, Open-File Report 94- Electronic file USGS publication search refraction profiles, seismic refraction profiles in Southwest New Pankratz, D.P. Klein 695 (DJVU) http://pubs.er.usgs.gov/usgspubs/ southwestern New Mexico ofr/ofr94695 Mexico, 2 Geology Geology, Southwestern NM Magmatism and metamorphism at 1.46 Ga in Amato, J.M., A.O. 2008 In New Mexico Geological Society Fall Field Paper in Book http://nmgs.nmt.edu/publications/g $45.00 magmatism, the Burro Mountains, southwestern New Boullion, and A.E. Conference Guidebook - 59, Geology of the Gila uidebooks/59/ metamorphism, Mexico Sanders Wilderness-Silver City area, 107-116. Burro Mountains, southwestern New Mexico 3 Geology Geology, mineral Catron County Geology and mineral resources of York Anderson, O.J. 1986 New Mexico Bureau of Mines and Mineral Electronic file (PDF) NMBGMR search $10.00 for resources, York Ranch SE quadrangle, Cibola and Catron Resources Open File Report 220A, 22 pages. <http://geoinfo.nmt.edu/publicatio CD Ranch, Fence Counties, New Mexico ns/openfile/details.cfml?Volume=2 Lake, Catron, 20A> Cibola 4 Geology Geology, Zuni Salt Catron County Geology of the Zuni Salt Lake 7 1/2 Minute Anderson, O.J. 1994 New Mexico Bureau of Mines and -
NI 43-101 Technical Exploration Report Billali Mine, New Mexico
NI 43-101 Technical Exploration Report Billali Mine, New Mexico Report Date: December 9, 2011 Effective Date: December 9, 2011 Report Prepared for Billali Mine, LLC P. O. Box 207 Duncan, AZ 85534 Report Prepared by Jan C. Rasmussen, Ph. D., R.G., Reg. Mem. SME P. O. Box 36971 Tucson, Arizona 85740 Signed by Qualified Persons: Jan C. Rasmussen, Ph.D., R.G., RM SME NI 43-101 Technical Exploration Report – Billali Mine, New Mexico Page i Summary (Item 1) Property Description and Ownership The Billali mine is a lode mining claim patented in 1899 and now owned by the Billali Mine LLC. The Billali mine is an advanced stage, epithermal, silver-gold quartz vein prospect with minor past production. The mine is located in the northwest end of the Steeple Rock mining district of western New Mexico and adjacent Arizona. The Billali mine project is located in westernmost New Mexico, in the Summit Mountains, Grant County. It is approximately 35 mi (55 km) east of Safford, Arizona, and is approximately 15 mi (25 km) northeast of Duncan, Arizona. The location of the Billali mine adit is approximately latitude 32º53‟04.91” N and longitude 108º59‟01.59” W, elevation 5,343 ft. The claim has a cadastral location of SE ¼ and SW ¼, Section 26, Township 16 South (T16S), Range 21 West (R21W), New Mexico Meridians. Ownership The Billali mine is a patented lode mining claim owned by the Billali Mine LLC. The three managers and owners are Mr. Leslie H. Billingsley, Mr. Richard O. Billingsley, and Mr. Joy J. -
Supergene Mineralisation of the Boyongan Porphyry Copper-Gold Deposit, Surigao Del Norte, Philippines
Supergene Mineralisation of the Boyongan Porphyry Copper-Gold Deposit, Surigao del Norte, Philippines by Allan Maglaya Ignacio B.Sc. Geology, National Institute of Geological Sciences University of the Philippines Thesis submitted in partial fulfilment of the requirements of the Masters of Economic Geology Degree Centre for Ore Deposit Research, University of Tasmania December, 2005 DECLARATION OF ORIGINALITY This thesis contains no material which has been accepted for a degree of diploma by the University of Tasmania or any other institution, except by way of background information and duly acknowledged in the thesis, and contains no previous material previously pub- lished or written by another person except where due acknowledgement is given. Allan Maglaya Ignacio 01 December 2005 _________________________ STATEMENT OF AUTHORITY OF ACCESS This thesis may not to be made available for loan or copying for 1.5 years following the date this statement was signed. Following that time, the thesis may be available for loan and lim- ited copying in accordance with Copyright Act 1968. Allan Maglaya Ignacio 01 December 2005 _________________________ TABLE OF CONTENTS Page (s) LIST OF FIGURES …………………………………………………….. i - iii LIST OF APPENDICES ………………………………………………… iv ACKNOWLEDGMENTS ………………………………………………. v ABSTRACT ……………………………………………………………... vi - vii 1.0 INTRODUCTION ………………………………………………………. 1 - 8 1.1 Introduction …………………………………………………………. 1 1.2 Aims and Objectives ……………………………………………….. 1 1.3 Methods Employed …………………………………………………. 2 1.4 Location and Accessibility …………………………………………. 3 1.5 Climate ……………………………………………………………... 5 1.6 Previous Work ……………………………………………………… 5 2.0 GEOLOGICAL SETTING ………………………………………………. 9 - 37 2.1 Introduction ………………………………………………………. 9 2.2 Regional Tectonics …………….…………………………………. 9 2.3 Regional and Local Stratigraphy ………………………………... 11 2.3.1 Basement (Cretaceous-Paleogene) ………………………. 11 2.3.2 Bacuag Formation (Oliogocene-Miocene) .…………….. -
Sierrita Mine from Mine to Me How Copper Ore Becomes Copper Wire
Sierrita Mine From Mine to Me How copper ore becomes copper wire Arizona Copper Mines 3 Copper Sulfide Ore 5 Copper Oxide Ore 8 Exploration 11 Open Pit Mining 22 Crushing and Milling 37 Flotation 46 Smelting 54 Leaching Oxide Ore 71 2012 Heap Leaching 76 by Jan C. Rasmussen, Ph.D. Solvent Extraction 82 Electrowinning 87 Fabricating - Rod Mill 96 Electrorefining 100 Reclamation 112 Uses of Copper 118 2 Arizona Copper Mines • Bagdad • Bisbee • Carlota • Hayden Smelter • Johnson Camp • Miami • Mineral Park • Mission • Morenci • Pinto Valley • Ray • Resolution • Rosemont X San Manuel • Safford • San Manuel • Sierrita X Bisbee • Silver Bell • Tohono 3 Copper sulfide ore and copper oxide ore are processed in different ways. Exploration Mining Concentrating Sulfide Ore Copper Products Smelting To Customer Rod, Cake, and Cathode Oxide Ore Leaching Solvent Extraction Electrowinning Refining Copper Anodes to Texas Copper Product to Customer (Ray and Silver Bell) 4 Cathode Sulfide ore: Chalcopyrite & Bornite Chalcopyrite Chalcopyrite can be called copper fool’s gold. It is made of copper, iron, and sulfur. It is a brassy yellow, metallic mineral and it is very heavy. Chalcopyrite is not as hard as pyrite, which is called fool’s gold. Chalcopyrite will not scratch glass, but will scratch a copper penny. Pyrite will scratch glass. Chalcopyrite is also a brighter yellow than pyrite. It often tarnishes to a blue-green, iridescent color on weathered surfaces. Chalcopyrite is the main copper sulfide ore. Chalcocite Bornite is also known as Peacock Copper because of the blue-green tarnish. On freshly broken surfaces, it is Chalcocite is a sooty black, bronze colored. -
Formation of Chrysocolla and Secondary Copper Phosphates in the Highly Weathered Supergene Zones of Some Australian Deposits
Records of the Australian Museum (2001) Vol. 53: 49–56. ISSN 0067-1975 Formation of Chrysocolla and Secondary Copper Phosphates in the Highly Weathered Supergene Zones of Some Australian Deposits MARTIN J. CRANE, JAMES L. SHARPE AND PETER A. WILLIAMS School of Science, University of Western Sydney, Locked Bag 1797, Penrith South DC NSW 1797, Australia [email protected] (corresponding author) ABSTRACT. Intense weathering of copper orebodies in New South Wales and Queensland, Australia has produced an unusual suite of secondary copper minerals comprising chrysocolla, azurite, malachite and the phosphates libethenite and pseudomalachite. The phosphates persist in outcrop and show a marked zoning with libethenite confined to near-surface areas. Abundant chrysocolla is also found in these environments, but never replaces the two secondary phosphates or azurite. This leads to unusual assemblages of secondary copper minerals, that can, however, be explained by equilibrium models. Data from the literature are used to develop a comprehensive geochemical model that describes for the first time the origin and geochemical setting of this style of economically important mineralization. CRANE, MARTIN J., JAMES L. SHARPE & PETER A. WILLIAMS, 2001. Formation of chrysocolla and secondary copper phosphates in the highly weathered supergene zones of some Australian deposits. Records of the Australian Museum 53(1): 49–56. Recent exploitation of oxide copper resources in Australia these deposits are characterized by an abundance of the has enabled us to examine supergene mineral distributions secondary copper phosphates libethenite and pseudo- in several orebodies that have been subjected to intense malachite associated with smaller amounts of cornetite and weathering. -
Gossans and Leached Cappings
Gossans and Leached Cappings Roger Taylor Gossans and Leached Cappings Field Assessment Roger Taylor Townsville Queensland 4810 Australia [email protected] ISBN 978-3-642-22050-0 e-ISBN 978-3-642-22051-7 DOI 10.1007/978-3-642-22051-7 Springer Heidelberg Dordrecht London New York Library of Congress Control Number: 2011934477 © Springer-Verlag Berlin Heidelberg 2011 This work is subject to copyright. All rights are reserved, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilm or in any other way, and storage in data banks. Duplication of this publication or parts thereof is permitted only under the provisions of the German Copyright Law of September 9, 1965, in its current version, and permission for use must always be obtained from Springer. Violations are liable to prosecution under the German Copyright Law. The use of general descriptive names, registered names, trademarks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use. Typesetting & Prepress: Elisabeth Sillmann, Landau, www.blaetterwaldDesign.de Cover design: deblik, Berlin Printed on acid-free paper Springer is part of Springer Science+Business Media (www.springer.com) Acknowledgements iven a 30–40 years germination period, it is not surprising that the list of con- tributors is considerable, and it is not feasible to list the input of every student, G colleague, and professional geologist. Th ank you everybody. -
PORPHYRY CU DEPOSITS (MODEL 17; Cox, 1986) by Leslie J. Cox
PORPHYRY CU DEPOSITS (MODEL 17; Cox, 1986) by Leslie J. Cox, Maurice A. Chaffee, Dennis P. Cox, and Douglas P. Klein SUMMARY OF RELEVANT GEOLOGIC, GEOENVIRONMENTAL, AND GEOPHYSICAL INFORMATION Deposit geology Porphyry copper deposits contain copper, molybdenum, and gold minerals, disseminated or in a stockwork of small veinlets within a large mass of altered rock (Singer and Mosier, 1981). The host rock is commonly a pyrite-rich porphyry ranging in composition from granodiorite to tonalite, but alkalic porphyries are locally important. In the southwestern United States, where porphyry copper deposits are abundant, associated igneous rocks are mainly Mesozoic and Cenozoic. Older plutonic, volcanic, sedimentary, and metamorphic rocks intruded by these porphyries also host ore minerals; the highest grades are found in reactive rocks such as limestone, or rocks, such as diabase, which contain abundant iron-rich minerals prior to alteration. Porphyry deposits exhibit a characteristic pattern of hydrothermal alteration, which includes biotite and K-feldspar assemblages in the center and grades outward to chlorite, actinolite, and epidote assemblages. Most deposits have a late-stage alteration assemblage that contains abundant white mica, clay, and carbonate minerals. Examples Bingham, Utah (Lanier and others, 1978); San Manuel, Ariz. (Lowell and Guilbert, 1970); El Salvador, Chile (Gustafson and Hunt, 1975). Spatially and (or) genetically related deposit types Related deposit types (Cox and Singer, 1986) include porphyry copper, skarn-related (Model 18a), base-metal skarn (Model 18c), porphyry copper-gold (Model 20c), porphyry copper-molybdenum (Model 21a), polymetallic vein (Model 22c), polymetallic replacement (Model 19a), volcanic-hosted copper-arsenic-antimony (Model 22a), quartz- alunite gold (Model 25e), distal disseminated silver-gold (Model 19c; Cox, 1992), and gold-skarn deposits.