BC Geological Survey Assessment Report 38071
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Pleistocene Volcanism in the Anahim Volcanic Belt, West-Central British Columbia
University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2014-10-24 A Second North American Hot-spot: Pleistocene Volcanism in the Anahim Volcanic Belt, west-central British Columbia Kuehn, Christian Kuehn, C. (2014). A Second North American Hot-spot: Pleistocene Volcanism in the Anahim Volcanic Belt, west-central British Columbia (Unpublished doctoral thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/25002 http://hdl.handle.net/11023/1936 doctoral thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY A Second North American Hot-spot: Pleistocene Volcanism in the Anahim Volcanic Belt, west-central British Columbia by Christian Kuehn A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY GRADUATE PROGRAM IN GEOLOGY AND GEOPHYSICS CALGARY, ALBERTA OCTOBER, 2014 © Christian Kuehn 2014 Abstract Alkaline and peralkaline magmatism occurred along the Anahim Volcanic Belt (AVB), a 330 km long linear feature in west-central British Columbia. The belt includes three felsic shield volcanoes, the Rainbow, Ilgachuz and Itcha ranges as its most notable features, as well as regionally extensive cone fields, lava flows, dyke swarms and a pluton. Volcanic activity took place periodically from the Late Miocene to the Holocene. -
CANLAVA Mining Corp. 203 – 1312 Ketch Court Coquitlam, B.C
2016 GEOLOGICAL REPORT ON THE NAZKO PROPERTY CARIBOO MINING DIVISION BRITISH COLUMBIA BCGS MAPS 093B.082 AND 093B.092 LATITUDE 52° 55’ 32.3” N AND LONGITUDE 123° 44’ 10.8” W STATEMENT OF WORK EVENT: 5611358 Prepared for: CANLAVA Mining Corp. 203 – 1312 Ketch Court Coquitlam, B.C. V3K 6W1 Prepared by: R. A. (Bob) Lane, P.Geo. Plateau Minerals Corp. Date: June 30, 2016 NAZKO PROPERTY - 2016 ASSESSMENT REPORT TABLE OF CONTENTS 1 EXECUTIVE SUMMARY .............................................................................................. 1 2 INTRODUCTION ........................................................................................................ 2 2.1 LOCATION AND ACCESS ............................................................................................................................. 2 2.2 PHYSIOGRAPHY AND CLIMATE .................................................................................................................. 2 2.3 PROPERTY STATUS AND OWNERSHIP ...................................................................................................... 2 2.4 DEVELOPMENT AND EXPLORATION HISTORY ......................................................................................... 6 3 REGIONAL GEOLOGY ................................................................................................. 6 4 PROPERTY GEOLOGY ................................................................................................ 7 5 MINERALIZATION .................................................................................................... -
Ministry of Energy and Mines BC Geological Survey Assessment
Ministry of Energy and Mines Assessment Report BC Geological Survey Title Page and Summary TYPE OF REPORT [type of survey(s)]: Geological and Geochemical TOTAL COST: $12,214.45 AUT!-IOR(S): R.A. (Bob) Lane NOTICE OF WORK PERMIT NUMBER(S)/DATE(S): -n/a---- ----------- ------- YEAR OF WORK: 2017 STATEMENT OF WORK - CASH PAYMENTS EVENT NUMBER(S)/DATE(S): 5653004 (June 15,2017) ------------------------- PROPERTY NAME: Nazko ------------------------------------------- CLAIM NAME(S) (on which the work was done): 552594, 1041719, 1047066 --------------------------------- COMMODITIES SOUGHT: Au, Ag ---"-------------------------------------- MINERAL INVENTORY MINFILE NUMBER(S), IF KNOWN: ------------------------------ MINING DIVISION: Cariboo NTS/BCGS: 093B.082 and 093B.092 -------------------- LATITUDE: 52 ° 55 • 32.3 " LONGITUDE: 123 ° 44 ' 10.8 " (at centre of work) OWNER(S): 1) CANLAVA Mining Corp. 2) ----------------------- MAILING ADDRESS: 203 - 1312 Keitch Court Coquitlam, B.C. V3K 6W1 OPERATOR(S) [who paid for the work]: 1) CANLAVA Mining Corp. 2) ----------------------- MAILING ADDRESS: 203 - 1312 Keitch Court Coquitlam, B.C. V3K 6W1 PROPERTY GEOLOGY KEYWORDS (lithology, age, stratigraphy, structure, alteration, mineralization, size and attitude): Eocene Ootsa lake Group, rhyolite, basalt, Cretaceous Skeena Group, elastic sedimentary rocks, gold-silver quartz veins REFERENCES TO PREVIOUS ASSESSMENT WORK AND ASSESSMENT REPORT NUMBERS: ------------------36171 Next Page TYPE OF WORK IN EXTENT OF WORK ON WHICH CLAIMS PROJECT COSTS THIS REPORT -
Summary of Activities 2015, Geoscience BC, Report 2016-1, P
TREK Geological Mapping Project, Year 2: Update on Bedrock Geology and Mineralization in the TREK Project Area, Central British Columbia (parts of NTS 093B, C, F, G) J.J. Angen, Mineral Deposit Research Unit, University of British Columbia, Vancouver, BC, [email protected] J.M. Logan, Consulting Geologist, North Saanich, BC C.J.R. Hart, Mineral Deposit Research Unit, University of British Columbia, Vancouver, BC R. Kim, Mineral Deposit Research Unit, University of British Columbia, Vancouver, BC Angen, J.J., Logan, J.M., Hart, C.J.R. and Kim, R. (2016): TREK geological mapping project, year 2: update on bedrock geology and min- eralization in the TREK project area, central British Columbia (parts of NTS 093B, C, F, G); in Geoscience BC Summary of Activities 2015, Geoscience BC, Report 2016-1, p. 1–16. Introduction The Interior Plateau region of British Columbia is con- sidered to have high exploration potential as it hosts a variety of deposit types including Late Cretaceous and Eocene epithermal Au and Ag deposits (e.g., Blackwa- ter, Capoose and Wolf) and porphyry Cu and Mo depos- its (e.g., Endako and Chu) ranging in age from Late Ju- rassic to Eocene. Exploration activity has historically been hindered by a limited understanding of the charac- ter and distribution of prospective units owing to the masking effects of overlying Eocene and Neogene ba- salt flows and extensive glacial till cover. The Targeting Resources through Exploration and Knowledge (TREK) project is a Geoscience BC initiative to inte- grate geophysical, geological and geochemical data in order to improve our geological understanding and, ul- timately, reduce the risk associated with exploration in such a poorly understood region (Clifford and Hart, 2014). -
Evidence of Geothermal Activity Near the Nazko Volcanic Cone, British Columbia, Canada, from Ground and Surface Water Chemistry
Newsletter for the Association of Applied Geochemists NUMBER 175 JUNE 2017 Evidence of geothermal activity near the Nazko volcanic cone, British Columbia, Canada, from ground and surface water chemistry R. E. Lett1, and W. Jackaman2; 13956 Ashford Rd. Victoria, BC, Canada, V8P 3S5; 2Noble Exploration Ser- vices Ltd. 3890 Trailhead Drive, Jordan River, BC, Canada, V9Z 1L1 Introduction tion minerals in surface and ground water may be a guide to Water-rock and water-mineral interactions, aquifer ge- water temperature. ology, solution residence times, environmental factors and Here we describe evidence of geothermal activity from reaction rates are all factors that affect ground and surface a study of the water chemistry in two wetlands, informally water geochemistry. In areas where there is evidence of named the North and South Bogs, near the Nazko volcanic geothermal activity, variations of surface and ground water cone, British Columbia, Canada (Fig. 1). The bog water chemistry can also reflect accelerated rock weathering, chemical data are interpreted by their comparison to other changes in mineral solubility with increasing temperature geothermal areas, from a thermodynamic simulation with and the mixing of hot and cold ground water. For example, the PHREEQC software (Parkhurst & Appelo 2013) and 18 13 Pasvanoğlu (2013) interpreted high dissolved CO2, Si, Li, from the results of stable isotope (δD, δ O, δ C) analysis As, Hg and B concentrations in the thermal waters from of bog water. wells in Eastern Turkey to be the result of reactions be- There has been past interest in the geothermal poten- tween hot water and silica-rich volcanic rocks and by mixing tial of the area because of the presence of scattered traver- of hot and cold solutions during the ascent of water through tine deposits on the wetland surface, calcium carbonate-rich rock fractures to the surface. -
BC Geological Survey Assessment Report 38436
2019 TEST PITTING REPORT ON THE NAZKO PROPERTY CARIBOO MINING DIVISION BRITISH COLUMBIA BCGS MAPS 093B.082 AND 093B.092 LATITUDE 52° 55’ 32.3” N AND LONGITUDE 123° 44’ 10.8” W STATEMENT OF WORK EVENT: 5747079 Prepared for: CANLAVA Mining Corp. B140 5525 272nd Street Langley, B.C. V4W 1P1 Prepared by: R. A. (Bob) Lane, P.Geo. Plateau Minerals Corp. Date: September 5, 2019 NAZKO PROPERTY – 2019 ASSESSMENT REPORT TABLE OF CONTENTS 1 EXECUTIVE SUMMARY .............................................................................................. 1 INTRODUCTION ..................................................................................................................... 2 1.1 LOCATION AND ACCESS ............................................................................................................................. 2 1.2 PHYSIOGRAPHY AND CLIMATE .................................................................................................................. 2 1.3 PROPERTY STATUS AND OWNERSHIP ...................................................................................................... 2 1.4 DEVELOPMENT AND EXPLORATION HISTORY ......................................................................................... 4 2 REGIONAL GEOLOGY ................................................................................................. 6 3 PROPERTY GEOLOGY ................................................................................................ 7 4 MINERALIZATION ....................................................................................................