Source Water Protection Planning North Bay – Mattawa Source Protection Area Conceptual Water Budget
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Geology and Age of the Lac a La Perdrix Fenite, Southern Gatineau District, Quebec
CA9700383 -4- Geology and age of the Lac a la Perdrix fenite, southern Gatineau district, Quebec D.D. Hogarth1 and Otto van Breemen2 Hogarth, D.D. and van Breemen, 0., 1996: Geology and age of the Lac a la Perdrix fenite, southern Gatineau district, Quebec; inRadiogenic Age and Isotopic Studies: Report 9; Geological Survey of Canada, Current Research 1995-F, p. 33-41. Abstract: The Lac a la Perdrix fenite lies in the Central Metasedimentary Belt of the Grenville Province. This 30 m wide fenite, adjacent to a narrow calciocarbonatite sill, replaces diopside-oligoclase gneiss and is composed of magnesio-arfvedsonite, aegirine, microcline, albite, and fluorapatite. Near the contact with carbonatite, it contains appreciable monazite and barite whereas aegirine virtually disappears. Fenitization probably took place early in the igneous stage of carbonatite development. A Pb/U monazite age of 1026 ± 2 Ma is thought to date fenite formation. Together with published data, this age shows that carbonatite intruded metamorphic rocks near the close of the Grenville Orogeny. Resume : La fenite de Lac a la Perdrix s'observe dans la ceinture metasedimentaire de la Province de Grenville. Cette fenite, mesurant 30 m de largeur et en position adjacente par rapport a un etroit filon-couche de calciocarbonatite, remplace un gneiss a diopside-oligoclase et se compose de magnesio-arfvedsonite, d'aegirine, de microcline, d'albite et de fluorapatite. Pres du contact avec la carbonatite, la fenite contient de la monazite et de la barytine en quantite appreciable, tandis que l'aegirine disparait pratiquement. La fenitisation a probablement eu lieu au debut de l'episode igne durant lequel s'est form6 la carbonatite. -
An Assessment of the Groundwater Resources of Northern Ontario
Hydrogeology of Ontario Series (Report 2) AN ASSESSMENT OF THE GROUNDWATER RESOURCES OF NORTHERN ONTARIO AREAS DRAINING INTO HUDSON BAY, JAMES BAY AND UPPER OTTAWA RIVER BY S. N. SINGER AND C. K. CHENG ENVIRONMENTAL MONITORING AND REPORTING BRANCH MINISTRY OF THE ENVIRONMENT TORONTO ONTARIO 2002 KK PREFACE This report provides a regional assessment of the groundwater resources of areas draining into Hudson Bay, James Bay, and the Upper Ottawa River in northern Ontario in terms of the geologic conditions under which the groundwater flow systems operate. A hydrologic budget approach was used to assess precipitation, streamflow, baseflow, and potential and actual evapotranspiration in seven major basins in the study area on a monthly, annual and long-term basis. The report is intended to provide basic information that can be used for the wise management of the groundwater resources in the study area. Toronto, July 2002. DISCLAIMER The Ontario Ministry of the Environment does not make any 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. Reference therein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply endorsement, recommendation, or favoring by the ministry. KKK TABLE OF CONTENTS Page 1. EXECUTIVE SUMMARY 1 2. INTRODUCTION 7 2.1 LOCATION OF THE STUDY AREA 7 2.2 IMPORTANCE OF SCALE IN HYDROGEOLOGIC STUDIES 7 2.3 PURPOSE AND SCOPE OF THE STUDY 8 2.4 THE SIGNIFICANCE OF THE GROUNDWATER RESOURCES 8 2.5 PREVIOUS INVESTIGATIONS 9 2.6 ACKNOWLEDGEMENTS 13 3. -
Publication No
GEOLOGYAND GEOCHEMISTRY OF ORDOVICIANCARBONATITE DIKES IN THELEMITAR MOUNTAINS, SOCORROCOUNTY, NEW MEXICO Virginia T. McLemore New Mexico Bureau of Mines and Mineral Resources Open-FileReport 158 February, 1982 ABSTRACT Ordovician (449k16 m.y.) carbonatites intrude the complex Precambrian terrain in the Lemitar Mountains. They occur as dikes, stockworks, and veins and notare associated with any alkalic rocks or kimberlites. These radioactive carbonatites exhibit igneous textures and intrusive relationships with the country rocks and display the mineralogy and chemistry typical of such rocks. Sodic fenitization is present along some carbona- tite dikes. The Lemitar carbonatites can be grouped1) asxenolith- bearing breccia and microbreccia silicocarbonatite dikes and 2) xenolith-free carbonatites. The xenolith-free carbonatites are subdivided into a) fine-grained calcitic to dolomitic silico- carbonatite dikes, b) sijvite and rauhaug.ite veins, c) ankeritic- dolomitic carbonatite dikes, and d) stockwork carbonatites. Primary magmatic (with igneous textures.) and replacement (with relict replacement textures) fine-grain calcitic to dolomitic silicocarbonatite dikes are differentiated. The Lemitar carbona- tites consistof greater than 50% carbonate minerals with various amounts of magnetite,apatite, hematite, biotite/phlogopite, quartz, and numerous accessory minerals. These rocks are characterized by steep light rare-earth element enriched chondrite-normalized patterns, diagnostic of carbonatites. Similar carbonatites are found in the Chupadera Mountains, Socorro County and the Monte Largo area, Bernalillo County. The Lemitar carbonatites are enriched in uranium, thorium, rare-earth elements, barite, and fluorite; although the economic potential of these carbonatites ii is probably low. The Lemitar carbonatites are similarin texture, emplacement, mineralogy, and chemistry to the mantle-derived carbonatites in the Wet Mountains, Colorado, which suggests that the Lemitar carbonatites have a similar origin. -
Geol Callander Bay Area
31L*3NW9758 L. NIPIS I5A1 HIMSWORTH 010 GBOLOGT OALLAKDBR B AT ABBA 0. S. OHEMB forth Bty, Ontario. NoT*aft*r 6* 1956* OBOLOQT CAI.UMTOB BAT AREA IFIBODUCTIOM A regional geological reconnaissance program was initiated in th* Xorth Bay area, in tb* spring of 1956, with th* object of *jqploving for favourable eoluobiun and uraidm bearing areas. During th* course of this work aignifio&nt mineralogical and structural features w*r* observed in th* vicinity of Callander, Ontario. Detailed exMdnation revealed rook* on Zaland* A ei B, Ibrtb RJjssworth Towriahip, very closely resenfcling thoee found in tb* vicinity of tb* Beaueag* ooluabiuB-uraniua deposits. LOCATION The town of CaTltnrter is situated tight mil** south of th* city of Korth Bay, Ontario, on tb* Bain highway and on tb* Canadian National Railways mini in* to Toronto. Islands A fc B*, North Hinsvovth Township, li* two adl*s west of the town of Callander, in tb* western part of th* Southeast Bay of Lak* KLpissing. Locally this bay is called Callander Bay. HI3TOHI Tb* earliect ooansrcial activity in tb* Lak* RLpissing district was centred in Calland*r Bay as this *as th* starting point in tb* transhipasnt of 3 arg* pin* logs to th* Kaibuskong, Mattawa, and Ottawa rivers. Later with the ooadng of th* Canadian National and Canadian Pacific railways several sawsrtUs operated on th* shor* of the bay. On* of these is still in sodst*ne* drawing its logs from tb* Sturgeon River aero** tb* lak*. * call*d Darling Island on to* topographic map*. Tha shoreline of Callandar Bay ia a popular aimer resort eantra. -
ONTARIO, CANADA Truly Northern Experiences for Over 100 Years
OFFICIAL VISITORS’ GUIDE ONTARIO, CANADA Truly northern experiences for over 100 years. Aanin / Hello: On behalf of the Nipissing First Nation Council and community, I would like to welcome you to our traditional territory. The Nipissing (or Nbisiing) people have lived in the area of Lake Nipissing since time immemorial. Nbisiing means “little water” and was likely a comparison to the larger Great Lakes to the west and south. Historically, the Nipissings were traders due to Lake Nipissing’s ideal central location at the junction of the trade routes. Today, Nipissing First Nation is a progressive, culturally strong and self-governing Nation with a diverse economy. We remain proud stewards of our lands and waters, and hope you enjoy exploring the beautiful surroundings during your stay. Bi-biingeyok maa Nbisiing / Welcome to Nipissing First Nation. Chief Scott McLeod On behalf of myself, North Bay City Councillors and the citizens, I would like to welcome you to the city of North Bay. It is our hope that you will find our city a beautiful and relaxing place to visit; that you make new friends and memories; and, that you avail yourself of the amenities it has to offer. We are delighted that you will be spending time in the city of North Bay and, whether it be business or pleasure, we hope that you take some time from your scheduled plans to enjoy the City’s pleasant sights and Northern hospitality. We hope you enjoy your stay and we look forward to having you visit us again soon! Yours In Hospitality, Al McDonald Mayor, City of North Bay By land or air, North Bay couldn’t be more accessible. -
Durham E-Theses
Durham E-Theses The petrology and geochemistry of the north qoroq centre igaliko complex, south greenland Chambers, A. D. How to cite: Chambers, A. D. (1976) The petrology and geochemistry of the north qoroq centre igaliko complex, south greenland, Durham theses, Durham University. Available at Durham E-Theses Online: http://etheses.dur.ac.uk/8342/ Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in Durham E-Theses • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full Durham E-Theses policy for further details. Academic Support Oce, Durham University, University Oce, Old Elvet, Durham DH1 3HP e-mail: [email protected] Tel: +44 0191 334 6107 http://etheses.dur.ac.uk 2 THE PETROLOGY AND GEOCHEMISTRY OF THE NORTH QOROQ CENTRE IGALIKO COMPLEX, SOUTH GREENLAND A.D. Chambers, B.Sc. (Dunelm) A thesis submitted for the Degree of Doctor of Philosophy in the University of Durham September 1976 The copyright of this thesis rests with the author. No quotation from it should be published without his prior written consent and information derived from it should be acknowledged. 1 8£ Til.S Frontispiece. View of the Igdlerfigssalik Centre taken from the North Qoroq Centre. -
U.S. DEPARTMENT of the INTERIOR U.S.GEOLOGICAL SURVEY ALK.BIB a Selected Bibliography of Alkaline Igneous Rocks and Related Mine
U.S. DEPARTMENT OF THE INTERIOR U.S.GEOLOGICAL SURVEY ALK.BIB A selected bibliography of alkaline igneous rocks and related mineral deposits, with an emphasis on western North America compiled by Felix E. Mutschler, D. Chad Johnson, and Thomas C. Mooney Open-File Report 94-624 1994 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. INTRODUCTION This bibliography contains 3,406 references on alkaline igneous rocks and related mineral deposits compiled in conjunction with ongoing studies of alkaline igneous rocks, metallogeny, and tectonics in western North America. Much of the literature on these topics is not readily recovered by searches of current bibliographies and computerized reference systems. We hope that by making this bibliography available, it will help other workers to access this occasionally hard to find literature. The bibliography is available in two formats: (1) paper hardcopy and (2) Apple Macintosh computer-readable 3.5 inch double density diskette. The computer-readable version of the bibliography is a 725 KB WORD (version 5.0) document. Individual literature citations are arranged alphabetically by author(s) and the order of items in each citation follows the standard U.S. Geological Survey format. Version 3.4 1 February 1994 BIBLIOGRAPHY Abbott, J. G., Gordey, S. P., and Tempelman-Kluit, D. J., 1986, Setting of stratiform, sediment- hosted lead-zinc deposits in Yukon and northeastern British Columbia, in Morin, J. -
Carbonatites in the Lemitar and Chupadera Mountains, Socorro County, New Mexico Virginia T
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/34 Carbonatites in the Lemitar and Chupadera Mountains, Socorro County, New Mexico Virginia T. McLemore, 1983, pp. 235-240 in: Socorro Region II, Chapin, C. E.; Callender, J. F.; [eds.], New Mexico Geological Society 34th Annual Fall Field Conference Guidebook, 344 p. This is one of many related papers that were included in the 1983 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
NBMCA Integrated Watershed Management Strategy FINAL
NBMCA Integrated Watershed Management Strategy Final Report Prepared for: North Bay-Mattawa Conservation Authority Prepared by: Stantec Consulting Ltd. July 8, 2015 This document entitled NBMCA Integrated Watershed Management Strategy was prepared by Stantec Consulting Ltd. (“Stantec”) for the account of North Bay‐Mattawa Conservation Authority (the “Client”). Any reliance on this document by any third party is strictly prohibited. The material in it reflects Stantec’s professional judgment in light of the scope, schedule and other limitations stated in the document and in the contract between Stantec and the Client. The opinions in the document are based on conditions and information existing at the time the document was published and do not take into account any subsequent changes. Mapping has been generated by the North Bay‐Mattawa Conservation Authority using data supplied under license by Ontario Geospatial Data Exchange/Land Information Ontario and is copyrighted by the Queen’s Printer of Ontario (2014). Mapping is illustrative only and should not be relied upon for precise indication of routes, location of features or as a guide for navigation. In preparing the document, Stantec did not verify information supplied to it by others. Any use which a third party makes of this document is the responsibility of such third party. Such third party agrees that neither Stantec nor the North Bay‐Mattawa Conservation Authority shall be held responsible for any costs or damages of any kind, if any, suffered by it or any other third party as a result of decisions made or actions taken based on this document. Prepared by :Peter Bullock, BES Reviewed by: Stephane D’Aoust, M.A.Sc., P.Eng. -
Your Use of This Ontario Geological Survey Document (The “Content”) Is Governed by the Terms Set out on This Page (“Terms of Use”)
THESE TERMS GOVERN YOUR USE OF THIS DOCUMENT Your use of this Ontario Geological Survey document (the “Content”) is governed by the terms set out on this page (“Terms of Use”). By downloading this Content, you (the “User”) have accepted, and have agreed to be bound by, the Terms of Use. Content: This Content is offered by the Province of Ontario’s Ministry of Northern Development and Mines (MNDM) as a public service, on an “as-is” basis. Recommendations and statements of opinion expressed in the Content are those of the author or authors and are not to be construed as statement of government policy. You are solely responsible for your use of the Content. You should not rely on the Content for legal advice nor as authoritative in your particular circumstances. Users should verify the accuracy and applicability of any Content before acting on it. MNDM does not guarantee, or make any warranty express or implied, that the Content is current, accurate, complete or reliable. MNDM is not responsible for any damage however caused, which results, directly or indirectly, from your use of the Content. MNDM assumes no legal liability or responsibility for the Content whatsoever. Links to Other Web Sites: This Content may contain links, to Web sites that are not operated by MNDM. Linked Web sites may not be available in French. MNDM neither endorses nor assumes any responsibility for the safety, accuracy or availability of linked Web sites or the information contained on them. The linked Web sites, their operation and content are the responsibility of the person or entity for which they were created or maintained (the “Owner”). -
The Grønnedal-Ika Carbonatite–Syenite Complex, South Greenland: Carbonatite Formation by Liquid Immiscibility
JOURNAL OF PETROLOGY VOLUME 46 NUMBER 1 PAGES 191–217 2005 doi:10.1093/petrology/egh069 The Grønnedal-Ika Carbonatite–Syenite Complex, South Greenland: Carbonatite Formation by Liquid Immiscibility RALF HALAMA1,*, TORSTEN VENNEMANN2, WOLFGANG SIEBEL1 AND GREGOR MARKL1,y 1INSTITUT FU¨ R GEOWISSENSCHAFTEN, EBERHARD-KARLS-UNIVERSITA¨ TTU¨ BINGEN, WILHELMSTRASSE 56, D-72074,TU¨ BINGEN, GERMANY 2INSTITUT DE MINEERALOGIE ET GEEOCHIMIE, UNIVERSITE DE LAUSANNE, UNIL-BFSH2, CH-1015 LAUSANNE, SWITZERLAND RECEIVED NOVEMBER 6, 2003; ACCEPTED AUGUST 2, 2004 ADVANCE ACCESS PUBLICATION SEPTEMBER 9, 2004 The Grønnedal-Ika complex is dominated by layered nepheline between carbonatites and syenites, are consistent with derivation of syenites which were intruded by a xenolithic syenite and a central the carbonatites from the syenites via liquid immiscibility. plug of calcite to calcite–siderite carbonatite. Aegirine–augite, alkali feldspar and nepheline are the major mineral phases in the syenites, along with rare calcite. Temperatures of 680–910 C and silica KEY WORDS: alkaline magmatism; carbonatite; Gardar Province; liquid activities of 0Á28–0Á43 were determined for the crystallization of the immiscibility; nepheline syenite syenites on the basis of mineral equilibria. Oxygen fugacities, esti- mated using titanomagnetite compositions, were between 2 and 5 log units above the fayalite–magnetite–quartz buffer during the magmatic stage. Chondrite-normalized REE patterns of magmatic INTRODUCTION calcite in both carbonatites and syenites are characterized by REE Carbonatites typically occur in close association with enrichment (LaCN–YbCN ¼ 10–70). Calcite from the carbonatites alkaline silicate igneous rocks, either in individual has higher Ba ( 5490 ppm) and lower HREE concentrations complexes or in a regional association within particular than calcite from the syenites (54–106 ppm Ba). -
RARE-EARTH ELEMENT MINERALIZATION and FORMATION of the IRON HILL CARBONATITE COMPLEX, GUNNISON COUNTY, COLORADO, USA by Jae Er
RARE-EARTH ELEMENT MINERALIZATION AND FORMATION OF THE IRON HILL CARBONATITE COMPLEX, GUNNISON COUNTY, COLORADO, USA by Jae Erickson A thesis submitted to the Faculty and Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Master of Science (Geology). Golden, Colorado Date ________________ Signed: ________________________ Jae Erickson Signed: ________________________ Dr. Katharina Pfaff Thesis Advisor Golden, Colorado Date ________________ Signed: ________________________ Dr. Paul Santi Professor and Head Department of Geology and Geological Engineering ii ABSTRACT The Iron Hill carbonatite complex is located in the Powderhorn district in Gunnison County, Colorado, USA, roughly 35 km south-southwest of the city of Gunnison. The complex consists of a ringed series of silica-deficient alkalic igneous rocks with a carbonatite stock at the center. The genesis of Rare Earth Element (REE)-enriched igneous complexes like Iron Hill is contentious, and the processes involved with REE enrichment at these complexes are poorly understood. The complex is one of the largest known niobium and titanium endowments in the United States and contains significant amounts of light REEs and thorium. The igneous rocks of the Iron Hill complex intruded Proterozoic granite, syenite, and metamorphic country rock roughly 600 million years ago. From oldest to youngest, the major rock types found at the complex are pyroxenite, uncompahgrite, ijolite, nepheline syenite, and an ankeritic dolomite carbonatite stock. Carbonatite dikes, as well as jasper, limonite-barite, orthoclase-quartz-thorite, and fluorite-quartz veins are present. All major lithological units at Iron Hill are enriched in REEs, including a halo of intense fenitization within the surrounding country rock.