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Intrusion-Related Gold Deposits
INTRUSION-RELATED GOLD DEPOSITS SE Europe Geoscience Foundation Shortcourse Dr Tim Baker Economic Geology Research Unit, School of Earth Sciences, James Cook University Townsville, QLD 4811, Australia Ph: 61-7-47814756, Email: [email protected] OVERVIEW • Part 1: Classification, nomenclature & deposit comparison • Part 2: Examples: Tintina Gold Province • Part 3: Other examples & exploration INTRUSION RELATED GOLD DEPOSITS CHARACTERISTICS • Sillitoe (1991) – Gold-rich porphyry deposits – Epithermal & skarn in porphyry Cu environments – Gold related to alkalic magmatism – Mostly associated oxidized intrusions – Intrusion related gold deposits in Sn-W terranes (Thompson et al., 1999) NOMENCLATURE • Porphyry Au (Hollister, 1992) • Fort Knox-style Au (Bakke, 1995) • Intrinsic Au (Newberry et al., 1995) • Plutonic Au (McCoy et al., 1997) • Intrusion-related Au (Thompson et al., 1999) • Granitoid Au (Goldfarb et al., 1999) • Thermal aureole gold systems (Wall, 2005) CHARACTERISTICS • Intrusion related Au deposits in Sn-W terranes • Metals – Au, Bi, Te, W, Mo, As (Sb, Sn, Pb, Cu) • Magmas – Intermediate to felsic (wide range SiO2) – I-type (crustal input, transitional S-type) – Ilm>Mag – W-Sn-Mo association (Thompson et al., 1999) CHARACTERISTICS • Tectonic environment – Continental setting, inboard, commonly late • Age – Phanerozoic (Precambrian – Archean?) – Intrusions = mineralization • Ore – Au, Bi, Te, W, Mo, As (Sb, Sn, Pb, Cu) – Reduced (no Mag-Hem), low sulfide (Po-Py-Apy) • Style – Sheeted, breccia, stockwork, flat-vein, disseminated -
Minewater Study
National Rivers Authority (South Western-Region).__ Croftef Minewater Study Final Report CONSULTING ' ENGINEERS;. NATIONAL RIVERS AUTHORITY SOUTH WESTERN REGION SOUTH CROFTY MINEWATER STUDY FINAL REPORT KNIGHT PIESOLD & PARTNERS Kanthack House Station Road September 1994 Ashford Kent 10995\r8065\MC\P JS TN23 1PP ENVIRONMENT AGENCY 125218 r:\10995\f8065\fp.Wp5 National Rivers Authority South Crofty Minewater Study South Western Region Final Report CONTENTS Page EXECUTIVE SUMMARY -1- 1. INTRODUCTION 1-1 2. THE SOUTH CROFTY MINE 2-1 2.1 Location____________________________________________________ 2-1 ________2.2 _ Mfning J4istojy_______________________________________ ________2-1. 2.3 Geology 2-1 2.4 Mine Operation 2-2 3. HYDROLOGY 3-1 3.1 Groundwater 3-1 3.2 Surface Water 3-1 3.3 Adit Drainage 3-2 3.3.1 Dolcoath Deep and Penhale Adits 3-3 3.3.2 Shallow/Pool Adit 3-4 3.3.3 Barncoose Adit 3-5 4. MINE DEWATERING 4-1 4.1 Mine Inflows 4-1 4.2 Pumped Outflows 4-2 4.3 Relationship of Rainfall to Pumped Discharge 4-3 4.4 Regional Impact of Dewatering 4-4 4.5 Dewatered Yield 4-5 4.5.1 Void Estimates from Mine Plans 4-5 4.5.2 Void Estimate from Production Tonnages 4-6 5. MINEWATER QUALITY 5-1 5.1 Connate Water 5-2 5.2 South Crofty Discharge 5-3 5.3 Adit Water 5-4 5.4 Acidic Minewater 5-5 Knif»ht Piesold :\10995\r8065\contants.Wp5 (l) consulting enCneers National Rivers Authority South Crofty Minewater Study South Western Region Final Report CONTENTS (continued) Page 6. -
Intrusion-Related Gold Systems. a Brief Summary by Bruce Pertzel
Appendix 2 Intrusion-related Gold Systems. A brief summary by Bruce Pertzel. Intrusion‐related Gold Systems – Brief Summary The new frontier for new discoveries of significant large gold deposits ‐ Intrusive‐related gold systems [IRGS] – a Brief Summary of Characteristics and Identifiable Features (relevant to greenfields exploration) The classification of Intrusion‐related gold systems (IRGS) is a relatively recent development. Hart (2005) points out that no serious and comprehensive research of the genesis of gold deposits commenced until 1980 when the price of gold increased significantly. Baker (2003) cites the progression of classification of gold deposits related to magmatic rocks as commencing with the term porphyry gold deposits (after the usage of porphyry copper deposits) in 1992 by Hollister. This ignores the fact that Sillitoe (1979) had earlier introduced the concept of a porphyry gold deposit style. The next variation in the classification was used in 1995 by Bakker ‐ Fort Knox Style and since then the progression continued with Intrusive Gold (Newberry et al 1995); Plutonic Gold (McCoy et al, 1997); Intrusion‐related Gold (Thompson et al, 1999 and Granitoid Gold (Goldfarb et al, 1999). The generally accepted classification term is now Intrusion‐related Gold Systems (IRGS). It is reasonable to suggest that there remains an amount of confusion over the classification and many deposits might be included in such a classification without warranting such. However classifications are only convenient pigeon holes commonly used in geology and it should be remembered that each ore deposit has its own specific and unique characteristics and not all deposits exhibit all characteristics of any particular classification. -
Mr Gareth Davies Cleanearth Energy Unit 2A, Bess Park Road, Trenant Industrial Estate Wadebridge 27 October 2016 Cornwall PL27 6HB
Our Ref: APP/D0840/W/15/3097706 Mr Gareth Davies Cleanearth Energy Unit 2a, Bess Park Road, Trenant Industrial Estate Wadebridge 27 October 2016 Cornwall PL27 6HB Dear Mr Davies TOWN AND COUNTRY PLANNING ACT 1990 – SECTION 78 APPEAL MADE BY MR JAMES BOLITHO LAND AT WILTON FARM, HERODSFOOT, LISKEARD, PL14 4RD APPLICATION REF: PA14/06447 1. I am directed by the Secretary of State to say that consideration has been given to the report of Paul Griffiths BSc(Hons) BArch IHBC, who made site visits on 17 November 2015 and 17 December 2015 into your client’s appeal against the decision of Cornwall Council to refuse planning permission for a single wind turbine of max. 77m to tip, along with associated infrastructure, including an access track, and electrical housing in accordance with application ref: PA14/06447, dated 9 July 2014. 2. On 2 July 2016, this appeal was recovered for the Secretary of State's determination, in pursuance of section 79 of, and paragraph 3 of Schedule 6 to, the Town and Country Planning Act 1990, because the appeal gives rise to important issues for the application of the Wind Farm policy and the appeal is therefore being recovered because of the particular circumstances. Inspector’s recommendation and summary of the decision 3. The Inspector recommended that the appeal be allowed, and planning permission granted, subject to conditions. 4. For the reasons given below, the Secretary of State agrees with the Inspector’s conclusions, except where stated, and agrees with his recommendation. He has decided to allow the appeal. -
The Distribution of Ammonium in Granites from South-West England
Journal of the Geological Society, London, Vol. 145, 1988, pp. 37-41, 1 fig., 5 tables. Printed in Northern Ireland The distribution of ammonium in granites from South-West England A. HALL Department of Geology, Royal Holloway and Bedford New College, Egham, Surrey TW20 OEX, UK Abstract: The ammonium contents of granites, pegmatites and hydrothermally altered rocks from SW England have been measured. Ammonium levels in the granites are generally high compared with those from other regions, averaging 36ppm,and they differ markedlybetween intrusions. The pegmatites show higherammonium contents than any other igneous rocks which have yet been investigated. Ammonium contents are strongly enriched in the hydrothermally altered rocks, includ- ing greisens and kaolinized granites. There is agood correlation between the average ammonium content of the intrusions in SW England and their initial "Sr/*'Sr ratios and peraluminosity. This relationship supports the hypothesis that the ammonium in the granites is derived from a sedimentary source, either in the magmatic source region or via contamination of the magma. Introduction Results Ammonium is present as a trace constituent of granitic The granites rocks, in which it occurs in feldspars and micas substituting isomorphously for potassium (Honma & Itihara 1981). The The new analyses of Cornubian granites are given in Table amount of ammonium in granites varies from zero to over 1. They show a range of 3-179 parts per million NH:, with 100 parts per million, and it has been suggested that high the highest values being found in relatively small intrusions. concentrations may indicate the incorporation of organic- Taking the averagefor each of the major intrusions,and rich sedimentary material into the magma, either from the weighting them according to their relative areas (see Table presence of such material in rhe magmatic source region or 4), the average ammonium contentof the Cornubian granites via the assimilation of organic-rich country rocks (Urano as a whole is 36 ppm. -
Forenames Surname Relationship Status Marriedfor Gender Age YOB
Forenames Surname Relationship Status MarriedFor Gender Age YOB POB Occupation County Address Parish RegDist Hd No Absalom James YEO Head Married M 35 1876 Okehampton Devon Mason Devonshire White Horse Court Okehampton Devon Esb Missing Okehampton 3 1 Absalom John YEO Son M 5 1906 Okehampton Devon School Devonshire White Horse Court Okehampton Devon Esb Missing Okehampton 3 6 Ada YEO Sister Single F 45 1866 Devon Northam Housekeeper Devonshire Mt Dinham St Davids Exeter Exeter 8 2 Ada YEO Wife Married 17 years F 40 1871 Glamorgan Cardiff Glamorganshire 32 Fairfield Avenue Cardiff Cardiff 14 2 Ada RYDER Servant Widow F 38 1873 Malborough Devon Housemaid Devonshire Welby Tavistock Road Devonport Devonport Devonport 95 5 Ada YEO Wife Married 18 years F 35 1876 London Devonshire 12 Beach Road Hele Ilfracombe Ilfracombe Barnstaple 9 2 Ada YEO Wife Married 6 years F 33 1878 Clovelly Devon Glamorganshire 10 Bishop ST Cardiff Cardiff 15 2 Ada YEO Daughter Married 4 years F 27 1884 Kingston on Thames Surrey 76 Canbury Avenue Kingston‐On Thames Kingston on Thames Kingston 5 4 Ada YEO Daughter Single F 25 1886 London Poplar Clerk Merchant Essex 79 Kingston Road Ilford Ilford Romford 7 4 Ada YEO Daughter Single F 22 1889 London Southwark Sewing Machinist Blouses London 40 Rowfant Road Wandsworth Borough Wandsworth 4 7 Ada DUMMETT Servant Single F 18 1893 Devon Berrynarbor General Servant Domestic Devonshire Wescott Barton Marwood Barnstaple Marwood Barnstaple 740 5 Ada DAVIS Servant Single F 17 1894 Alfreton Derbyshire General Servant Domestic Derbyshire -
Streamside Meadow on the Edge of Stithians, Truro, Cornwall, TR3 7AD
Streamside Meadow On The Edge Of Stithians, Truro, Cornwall, TR3 7AD 3.81 acres of level pasture land with stream frontage on the edge of a popular village A30/Redruth 6 miles - Falmouth 7 miles - Truro 9 miles • Auction 25th September • Level Pasture with Stream Frontage • Gently South Facing • Potential For Stables (STP) • Excellent Riding Area • Edge Of Well Serviced Village • 3.81 Acres In All • For auction £25,000 to £45,000 01872 264488 | [email protected] Cornwall | Devon | Somerset | Dorset | London stags.co.uk Streamside Meadow On The Edge Of Stithians, Truro, Cornwall, TR3 7AD SITUATION SERVICES The land is situated on the south western edge of The property is watered naturally from the stream which Stithians which has an excellent range of amenities forms the southern boundary. There are currently no including a primary school rated as "good" by OFSTED. main services connected to the property. Stithians Reservoir is close by, offering a range of water sports and camping facilities. There are a network of WAYLEAVES, COVENANTS AND RIGHTS OF lanes, paths and bridleways which offer excellent WAY walking and horse riding. Nearby Falmouth and Truro The land is sold subject to and with the benefit of any offer an extensive range of shopping, health and leisure Wayleave Agreements in respect of electricity or facilities. The A30, providing direct access to Exeter and telephone equipment crossing the property, together the national motorway network, can be joined at with any restrictive covenants or public or private rights Redruth, approximately 6 miles to the north. of way. There is a restrictive covenant limiting development on the land. -
Notice Concerning Copyright Restrictions
NOTICE CONCERNING COPYRIGHT RESTRICTIONS This document may contain copyrighted materials. These materials have been made available for use in research, teaching, and private study, but may not be used for any commercial purpose. Users may not otherwise copy, reproduce, retransmit, distribute, publish, commercially exploit or otherwise transfer any material. The copyright law of the United States (Title 17, United States Code) governs the making of photocopies or other reproductions of copyrighted material. Under certain conditions specified in the law, libraries and archives are authorized to furnish a photocopy or other reproduction. One of these specific conditions is that the photocopy or reproduction is not to be "used for any purpose other than private study, scholarship, or research." If a user makes a request for, or later uses, a photocopy or reproduction for purposes in excess of "fair use," that user may be liable for copyright infringement. This institution reserves the right to refuse to accept a copying order if, in its judgment, fulfillment of the order would involve violation of copyright law. HOT DRY ROCK - A EUROPEAN PERSPECTIVE J.D. Garnish Energy Technology Support Unit AERE Harwell, Oxon, England ABSTRACT permeability but natural hydrothermal circulation in existing fractures. For the purposes of this review HDR Research into hot dry rock technology is being pursued research is defined narrowly as work directed towards the actively in several European countries. All these projects creation of a heat transfer zone in otherwise impermeable employ variations of the basic hydrofracturing approach. rock, and the extraction of useful heat by the circulation of Following proof of the concept at Los Alamos, the UK fluid through that zone. -
CORNWALL Extracted from the Database of the Milestone Society
Entries in red - require a photograph CORNWALL Extracted from the database of the Milestone Society National ID Grid Reference Road No Parish Location Position CW_BFST16 SS 26245 16619 A39 MORWENSTOW Woolley, just S of Bradworthy turn low down on verge between two turns of staggered crossroads CW_BFST17 SS 25545 15308 A39 MORWENSTOW Crimp just S of staggered crossroads, against a low Cornish hedge CW_BFST18 SS 25687 13762 A39 KILKHAMPTON N of Stursdon Cross set back against Cornish hedge CW_BFST19 SS 26016 12222 A39 KILKHAMPTON Taylors Cross, N of Kilkhampton in lay-by in front of bungalow CW_BFST20 SS 25072 10944 A39 KILKHAMPTON just S of 30mph sign in bank, in front of modern house CW_BFST21 SS 24287 09609 A39 KILKHAMPTON Barnacott, lay-by (the old road) leaning to left at 45 degrees CW_BFST22 SS 23641 08203 UC road STRATTON Bush, cutting on old road over Hunthill set into bank on climb CW_BLBM02 SX 10301 70462 A30 CARDINHAM Cardinham Downs, Blisland jct, eastbound carriageway on the verge CW_BMBL02 SX 09143 69785 UC road HELLAND Racecourse Downs, S of Norton Cottage drive on opp side on bank CW_BMBL03 SX 08838 71505 UC road HELLAND Coldrenick, on bank in front of ditch difficult to read, no paint CW_BMBL04 SX 08963 72960 UC road BLISLAND opp. Tresarrett hamlet sign against bank. Covered in ivy (2003) CW_BMCM03 SX 04657 70474 B3266 EGLOSHAYLE 100m N of Higher Lodge on bend, in bank CW_BMCM04 SX 05520 71655 B3266 ST MABYN Hellandbridge turning on the verge by sign CW_BMCM06 SX 06595 74538 B3266 ST TUDY 210 m SW of Bravery on the verge CW_BMCM06b SX 06478 74707 UC road ST TUDY Tresquare, 220m W of Bravery, on climb, S of bend and T junction on the verge CW_BMCM07 SX 0727 7592 B3266 ST TUDY on crossroads near Tregooden; 400m NE of Tregooden opp. -
ERDF Convergence Progress Report, Jun 2014 DRAFT.Pub
ERDF Convergence Progress Report June 2014 Convergence status We are now 100% through the ERDF Convergence Programme in terms of time. By the end of 2013 local partners had endorsed enough investments to fully commit the Programme and the final projects will be contracted over the coming months. Some investments will continue to be delivered until 2015. ERDF has met its spend targets for 2009, 2010, 2011, 2012 and 2013. All monetary figures are million euros ERDF Programme Programme budget €458.1m Number of investments contracted* 163 Actual spend to date €327.4m Spend target by end 2014 €378.4m Note: The Programme allocation is fixed in euros. During the life of the Programmes the sterling value of the Programme will vary with the GBP/Euro exchange rates so the figures above are given in euros for consistency. For more detailed information about all Convergence investments is available on our website. You can also find the latest Convergence updates by visiting our Media Hub. *Excludes Grant for Business Investment (GBI) projects which are yet to draw down ERDF Convergence funding. find out more… www.erdfconvergence.org.uk CONVERGENCE INVESTMENTS New Investments Apple Aviation Ltd Apple Aviation, an aircraft maintenance, repair and overhaul company, has established a base at Newquay Airport’s Aerohub. Convergence funding from the Grant for Business Investment programme will contribute to salary costs for thirteen new jobs in the business. ERDF Convergence investment: £211,641 (through the GBI SIF) Green Build Hub Located alongside the Eden Project, the Green Build Hub will be a research facility capable of demonstrating and testing the performance of innovative sustainable construction techniques and materials in a real building setting. -
The Conservation Value of Abandoned Pits and Quarries In
Contents Foreword 1 Professor Keith Atkinson The Derelict Land Advisory Group 2 Adrian Spalding Geological map of Cornwall 4 Chapter 1. Geology 5 Colin Bristow Chapter 2. The Historic Environment 29 Nicholas Johnson, Peter Herring & Adam Sharpe Chapter 3. The Nature Conservation Value Of Abandoned Pits And Quarries 47 Adrian Spalding, Jeremy Clitherow & Trevor Renals Chapter 4. The Land Use Planning Context for Abandoned Pits and Quarries 59 David Owens Chapter 5: The Waste Management Licensing Aspects 63 Ralph Seymour Chapter 6: Abandoned pits and quarries: a resource for research, education, leisure and tourism 69 John Macadam & Robin Shail Case Study 1: Burrator Quarries 81 Peter Keene Case Study 2: The Reclamation of Holman's Quarry 84 Jon Mitchell Case Study 3: Cheesewring Quarry, bolts, blackfaces and bertrandite 93 Martin Eddy Case Study 4: Prince of Wales Quarry - reuse of an abandoned slate quarry as a recreational and educational site 97 Charlie David Case Study 5: St Erth Pits - Cornwall Wildlife Trust's first geological nature reserve 101 J.D. Macadam (Cornwall RIGS Group) The Way Forward 105 Stephen Hartgroves, Dave Owens & Adrian Spalding Contributors Professor Keith Atkinson (Camborne School of Mines, University of Exeter) Colin Bristow (Camborne School of Mines, University of Exeter) Jeremy Clitherow (English Nature) Charlie David (North Cornwall District Council) Martin Eddy (Caradon Countryside Service, Caradon District Council) Peter Herring (The Historic Environment Service, Cornwall County Council) Nicholas Johnson -
Note8 on Cornish Mineral Localities
92 X.--Note8 on Cornish Mineral Localities. By 3. H. Co~Iss, F.G.S. HE following brief notes may be of some interest to students of T Cornish Mineralogy. I st.--l~Ew LocaLItIEs. Seheelite.--This occurs as a partial replacement of Wolfram at East Pool Mine, where it was first noticed by Mr. Cornelius Beringer, of Redruth, an Associate Member of this Society. Hitherto it has "only been found at Pengelly Croft, Huel Mandlin, and Levant Mine, in Cornwall, ~ and at Huel Friendship, in Devon. Montmorillonite.mThis member of the chloropal group of minerals t has recently been foucrd at Great Retallack Mine, in Perranzabuloe, Cornwall. It is associated with decomposing pyrites, but on careful separation yields the following results on analysis. Silica .............. 47"9 Peroxide of iron ........ 1"2 Alumina ............ 27" 1 Water .............. 23"0 Potash and loss .......... -8 I00'0 This agrees very closely indeed with the formula A12 Ha O~, 3SiOs + 2H20 , occupying the aluminous end of the same series in which ehloropal occupies the terruginous end. No doubt this Montmorillonite is a secondary product, .and therefore of little interest to mineralogists who care for nothing but crystallography, but it is interesting to chemical mineralogists as illustrating the con- stant tendency of the operations in nature's laboratory to produce definite chemical compounds rather than mere mixtures. Millerit~--This I have recently found in a vein traversing black silurian schist at Gerrans Bay, in Col~wall, in a cavity lined with pale * See Handbook, to the Mineralogy of Cornwall and Devon, part 2, p. 90 ; and Min.