DOCSLIB.ORG

Technical Report Rajapalot Property Mineral Resource Estimate NI 43-101 Technical Report Mawson Gold Limited

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Technical Report Rajapalot Property Mineral Resource Estimate NI 43-101 Technical Report Mawson Gold Limited AMC Consultants Pty Ltd ABN 58 008 129 164 Level 29, 140 William Street Melbourne Vic 3000 Australia T +61 3 8601 3300 E [email protected] W amcconsultants.com Technical Report Rajapalot Property Mineral Resource Estimate NI 43-101 Technical Report Mawson Gold Limited Location Ylitornio – Rovaniemi, Finland In accordance with the requirements of National Instrument 43-101 “Standards of Disclosure for Mineral Projects” of the Canadian Securities Administrators Qualified Persons: R Webster B.App.Sc. MAusIMM, M.AIG K Forrester CEng, MIChemE, MAusIMM AMC Project 120026 Effective date 14 September 2020 Unearth a smarter way Rajapalot Property Mineral Resource Estimate NI 43-101 Technical Report Mawson Gold Limited 120026 1 Summary 1.1 Introduction AMC Consultants Pty Ltd (AMC) was commissioned by Mawson Gold Ltd (Mawson) to report the results of a Mineral Resource estimate for the Rajapalot Gold-Cobalt Project (property located in Lapland, Finland). This Mineral Resource has been reported according to the Canadian Institute of Mining and Metallurgy (CIM) Definition Standards (2014) and the report is written in accordance with the requirements of National Instrument 43-101 (NI 43-101) “Standards of Disclosure for Mineral Projects” of the Canadian Securities Administrators. This report is an update to the December 2018 report. A site visit was carried out in October 2018 by Rod Webster Principal Geologist who is acting as the Qualified Person (QP) for reporting of the Mineral Resource estimate. The information, conclusions, opinions, and estimates contained herein are based on: • Information available to AMC at the time of preparation of this report. • Assumptions, conditions, and qualifications as set forth in this report. • Data, reports, and other information supplied by Mawson. 1.2 Tenements On 30 April 2010, Mawson entered into an agreement with AREVA Finland (AREVA) whereby the Company acquired 100% of AREVA’ s mineral properties and exploration database in exchange for €1 million (M). The Rompas-Rajapalot property (Property) consists of three granted exploration permits in legal force with an additional two exploration permits which are under standard bi-or tri-annual renewals. Also, the Property includes nine (9) exploration permit applications and one reservation. 1.3 Location and ownership The Property is centred roughly at coordinates 3,408,600E by 7,373,000N of the Finnish national coordinate system (KKJ), Zone 3. It is located approximately 35 kilometres (km) west-southwest of the city of Rovaniemi in southern Lapland, Finland. Access by road from Rovaniemi is via highway E75 south-westerly for 24 km to the junction of highway 930, just past the town of Muurola. The topography is gently rolling to almost flat, heavily glaciated and inundated with numerous post-glacial lakes, till, eskers, lacustrine and fluvial deposits. The climate is classified as subarctic with an average temperature of +0.2°C. 1.4 Geology and mineralization The Property lies within the Karelia tectonic province in a Paleoproterozoic supracrustal sequence known as the Peräpohja belt (PB). This is comprised of quartzites, mafic sills and volcanics and volcaniclastics, carbonate rocks, black shales, mica schists and greywackes unconformably overlying Archean rocks of the Pudasjärvi Complex (PuC). Granitoid intrusions ranging from 2.05 to 1.78 Ga occur throughout the project. 1.5 Exploration and drilling All core recoveries were excellent and averaged close to 100% in fresh rock. Photographing and logging were conducted in Mawson’s Rovaniemi facilities and in those of the Geological Survey of amcconsultants.com ii Rajapalot Property Mineral Resource Estimate NI 43-101 Technical Report Mawson Gold Limited 120026 Finland (GTK). Core intervals, averaging 1 m for mineralized samples and 2 m for barren samples, were cut in half at the GTK core facilities in Rovaniemi. Drill core orientation was completed on PAL drillholes with the bottom of hole marked with a continuous line. This line on the remaining half core was retained for verification and reference purposes. 1.6 Assay data Samples were prepared at Kempele and analyzed for gold at Raahe where the PAL1000 technique was used. This involves grinding the sample in steel pots with abrasive media in the presence of cyanide, followed by measuring the gold in solution with flame AAS equipment. Fire assay techniques follow ALS laboratory standard procedures. Where fire assay techniques have been used as the primary or verification method for gold analysis, these samples have been submitted to ALS preparation facilities either in Piteå or Sodankylä. Whilst on site from the 8 and 9 October 2018 the QP carried out the following: • Compared some laboratory assay certificates with the assay database and found no errors. • Observed the geological logging and sampling of the core. • Reviewed the core against core logs for a number of drillholes. • Observed the drilling, logging, sampling, subsampling and core cutting operations. • Visited the project area. The QP considers the drillhole data is suitable for estimation and reporting Mineral Resource estimates. Based on quality control and quality assurance results the QP is satisfied about the adequacy of the sample preparation, security and analytical procedures. The procedures follow industry best-practice guidelines and are reviewed frequently. 1.7 Mineral processing and metallurgical testing To date a single campaign of mineral processing and metallurgical testing has been completed (SGS Minerals UK; Gopalakrishnan 2014), with a second, more comprehensive program underway. The first work was preliminary in nature and limited to the recovery of gold on material sourced from the Palokas deposit. The early testwork programme was conducted prior to the broader discovery of the Raja deposit as well as the inclusion of cobalt as a potentially economic metal. Gravity release analysis tests reported by SGS included recoveries of between 26% and 48%. Further, cyanidation of the gravity tails demonstrated the recovery of leachable gold not recovered during gravity concentration. The combined gravity concentration and cyanidation test resulted in an overall gold recovery of between 95%. There was good reconciliation between the gold grades as calculated from testing assays and the expected grades provided by Mawson. Further metallurgical test work is currently underway, with Mawson a participant of Finland’s BATCircle consortium, a program designed to value-add to the Finnish battery metals circular economy. BATCircle was founded under the leadership of Aalto University to coordinate research on the battery metal circular economy from exploration to recycling. BATCircle includes 22 companies, four universities, two research institutes, and two cities. 1.8 Mineral Resource estimate A Mineral Resource was estimated using a block model and ordinary kriging to estimate the gold and cobalt block grades. amcconsultants.com iii Rajapalot Property Mineral Resource Estimate NI 43-101 Technical Report Mawson Gold Limited 120026 Based on pit optimization the Inferred Mineral Resources, estimated for the three deposits is shown in Table 1.1. The cut-offs used within the optimized pits and below the pits, based on AuEq cut-offs (where AuEq =Au (g/t) + Co/1,430 (ppm)) are: • 1.1 g/t AuEq below the optimal pits, potentially to be accessed by underground methods (termed UG). • 0.3 g/t AuEq for the deposits within their optimal pit (termed pit). Table 1.1 Inferred Mineral Resource estimate as of 14 September 2020 Cut-off Tonnes Au AuEq Au Co AuEq Zone Co (ppm) (AuEq) (kt) (g/t) (g/t) (koz) (Tonnes) (kOz) Raja Pit 0.3 3,055 2.5 474 2.8 247 1,448 279 Raja UG 1.1 641 1.6 1293 2.5 33 829 52 Raja total 3,696 2.4 616 2.8 280 2,277 331 Palokas Pit 0.3 3,218 1.8 531 2.1 182 1,709 221 Palokas UG 1.1 1,729 2.3 572 2.7 128 989 151 Palokas total 4,947 2.0 545 2.3 311 2,698 371 Rumajärvi Pit 0.3 289 0.8 397 1.1 7 115 10 Rumajärvi UG 1.1 35 1.2 476 1.6 1 17 2 Rumajärvi total 324 0.8 406 1.2 9 131 12 Total Pit 0.3 6,562 2.1 499 2.4 437 3,273 510 Total UG 1.1 2,405 2.1 763 2.6 163 1,834 204 Total 8,967 2.1 570 2.5 600 5,107 715 Notes: • CIM Definition Standards (2014) were used for Mineral Resource classification. • Totals may not compute exactly due to rounding. • AuEq=Au+Co/1,430 based on assumed prices of Co $17.28/lb and Au $1,694/oz. • Drilling results to 1 July 2020. • Mineral Resources that are not Mineral Reserves do not have demonstrated economic viability. Pit optimization was carried out for Raja and Palokas deposits using Whittle software to define the areas that could be mined by open pit methods compared to underground methods and demonstrate reasonable prospects for eventual economic extraction. The Mineral Resource estimate cut-offs were based on these parameters also. The parameters used in the pit optimization are as follows: • Gold price – US$1,694/oz • Cobalt price – US$17.28/lb • Processing cost of US$12.00/t • Processing recovery gold of 97% • Processing recovery cobalt of 80% • G&A costs of US$2.35/t • Selling cost US$0.75/t oz Au • Royalty 0.15% of revenue • Processing rate 1 Mtpa • Mining cost at the surface was $1.50/t • Mining cost increased by $0.02 per 5 m bench • Model has been regularized to an SMU of 5 m x 5 m x 2.5 m to account for dilution • Discount rate 8% • Overall slope angle of 50° amcconsultants.com iv Rajapalot Property Mineral Resource Estimate NI 43-101 Technical Report Mawson Gold Limited 120026 • No allowance for capital was included • The additional cost for mining ore is US$0.60/t Note the chosen prices for gold and cobalt are by reference to the CIBC Mining Group Analyst Consensus Commodity Price Forecast.
Load more

Recommended publications
  • Toponymic Guidelines (Pdf)
    UNITED NATIONS GROUP OF EXPERTS ON GEOGRAPHICAL NAMES 22nd session, New York, 20-29 April 2004 Item 17 of the provisional agenda TOPONYMIC GUIDELINES FOR MAP EDITORS AND OTHER EDITORS FINLAND Fourth, revised edition 2004* (v. 4.11, April 2021**) * Prepared by Sirkka Paikkala (Research Institute for the Languages of Finland) in collaboration with the Na- tional Land Survey of Finland (Teemu Leskinen) and the Geographical Society of Finland (Kerkko Hakulinen). The 22nd session of UNGEGN in 2004, WP 49. The first edition of this paper, Toponymic Guidelines for International Cartography - Finland, submitted by Mr. A. Rostvik, Norden Division, was presented to the Ninth session of UNGEGN 1981 (WP 37). The second version, Toponymic guidelines for cartography: Finland, prepared by the Onomastic Division of the Finnish Research Centre for Domestic Languages in collabo- ration with the Swedish Language Division and the National Board of Survey, was presented to the 4th UN Conference on the Standardization of Geographical Names in 1982 (E/CONF.74/L.41). The second edition, Toponymic Guidelines for Map an Other Editors, pre- paired by the Finnish Research Centre for Domestic Languages together with National Land Survey, was presented to the 17th session of UNGEGNUnited in 1994 (WP 63). The third edi- tion (revised version), prepared by Sirkka Paikkala in collaboration with the National Land Sur- vey of Finland and the Geographical Society of Finland, was presented to the 7th UN Conference on the Standardization of Geographical Names (New York, 13-22 January 1998, E/CONF.91/L. 17) ** Editions 4.1 - 4.6 updated by Sirkka Paikkala (Institute for the Languages of Finland) and Teemu Leskinen (National Land Survey of Finland).
    [Show full text]
  • Metsähallituksen Vesien Kaupallisen Kalastuksen Lupa-Alueet Vuosina 2020-2024
    METSÄHALLITUKSEN VESIEN KAUPALLISEN KALASTUKSEN LUPA-ALUEET VUOSINA 2020-2024 TILLSTÅNDSOMRÅDEN FÖR KOMMERSIELLT FISKE I FORSTSTYRELSENS VATTENOMRÅDEN FÖR ÅRET 2020-2024 Alue: Ylä-Lappi, område: Övre Lappland Nimi, namn Kunta, kommun Eräsuunnittelija Enontekiö, Inari, Jarmo Huhtamella Utsjoki Alue: Itä-Lappi, område: Östra Lappland Nimi, namn Kunta, kommun Eräsuunnittelija Lokka Sodankylä Markku Vierelä Porttipahta Sodankylä Markku Vierelä Vajunen ja Kurittu Sodankylä Markku Vierelä Enijärvi Kemijärvi Markku Vierelä Misijärvi Kemijärvi Markku Vierelä Karhujärvi Kemijärvi-Posio Markku Vierelä Moitajärvi Kemijärvi Markku Vierelä Kalliojärvi Kemijärvi Markku Vierelä Unarijärvi Sodankylä Markku Vierelä Vaalajärvi Sodankylä Markku Vierelä Alue: Länsi-Lappi, område: Västra Lappland Nimi, namn Kunta, kommun 2003 Simojärvi-Ranuan seutu Näskäjärvi Ranua Markku Vierelä Paattinkijärvi Ranua Markku Vierelä Penämöjärvi Ranua Markku Vierelä Simojärvi Ranua Markku Vierelä 2004 Norva-Vanttaus Iso-Herajärvi Rovaniemi Markku Vierelä Iso-Kaihuajärvi Rovaniemi Markku Vierelä Norvajärvi Rovaniemi Markku Vierelä Pietarijärvi Rovaniemi Markku Vierelä Sinettäjärvi Rovaniemi Markku Vierelä Ulkujärvi Rovaniemi Markku Vierelä Vanttausjärvi Rovaniemi Markku Vierelä 2006 Perunka-Naarma Ala-Naarmajärvi Rovaniemi Markku Vierelä Ala-Nampajärvi Rovaniemi Markku Vierelä Keskijärvi Rovaniemi Markku Vierelä Köyryjärvi Rovaniemi Markku Vierelä Perunkajärvi Rovaniemi Markku Vierelä Purnujärvi Rovaniemi Markku Vierelä Pyhäjärvi Rovaniemi Markku Vierelä Repojärvi Rovaniemi Markku
    [Show full text]
  • The Emigration from the Tornio Valley (Tornedalen)
    Swedish American Genealogist Volume 26 | Number 2 Article 5 6-1-2006 The miE gration from the Tornio Valley Sture Torikka Follow this and additional works at: https://digitalcommons.augustana.edu/swensonsag Part of the Genealogy Commons, and the Scandinavian Studies Commons Recommended Citation Torikka, Sture (2006) "The miE gration from the Tornio Valley," Swedish American Genealogist: Vol. 26 : No. 2 , Article 5. Available at: https://digitalcommons.augustana.edu/swensonsag/vol26/iss2/5 This Article is brought to you for free and open access by the Swenson Swedish Immigration Research Center at Augustana Digital Commons. It has been accepted for inclusion in Swedish American Genealogist by an authorized editor of Augustana Digital Commons. For more information, please contact [email protected]. The emigration from the Tornio Valley (Tornedalen) People left Sweden from all parts of the country, even the far north BY STURE TORIKKA The emigration to North America Stranded sailors of Norrbotten have for centuries from Norrbotten, in northern-most It happened sometimes: some people walked or skied to northern Norway Sweden, started in earnest during traveled to and fro and found it dif- in times of poverty. They had open the latter half of the 1870s. In the ficult to settle in one place. As early harbors without ice there, which Tornio River Valley (Tornedalen/ as 1858 the sailor Peter Tumber arri- made life easier than at home. When Tornionlaakso) the emigration per- ved in the port of New York, where the copper works started at Kåfjord haps did not start in earnest until the he mustered out and stayed when his in Northern Norway in the 1820s this 1880s.
    [Show full text]
  • Condition and Growth of Scots Pine Seedlings Under Strong and Weak Pollution in Kola Peninsula
    BALTIC FORESTRY CONDITION AND GROWTH OF SCOTS PINE SEEDLINGS /.../ A. FEDORKOV ET AL. Condition and Growth of Scots Pine Seedlings under Strong and Weak Pollution in Kola Peninsula ALEKSEY FEDORKOV*1, JUHA KAITERA2 AND RISTO JALKANEN3 1* Institute of Biology, Komi Science Center, Russian Academy of Sciences, Kommunisticheskaya st., 28, Syktyvkar, 167982, Russia; [email protected], tel. +7 8212 24 50 03 2Finnish Forest Research Institute, Muhos Research Unit, Kirkkosaarentie 7, FI 91500 Muhos, Finland; 3Finnish Forest Research Institute, Rovaniemi Research Unit, P. O. Box 16, FI 96301 Rovaniemi, Finland Fedorkov, A., Kaitera, J. and Jalkanen, R. 2007. Condition and Growth of Scots Pine Seedlings under Strong and Weak Pollution in Kola Peninsula. Baltic Forestry, 13 (2): 179183. Abstract Anthropogenic stress has affected forest trees for decades and will continue to do so in the foreseeable future. The Scots pine tree condition was evaluated and tree height was measured at age twelve in provenance field trial established on two sites under strong and weak pollution levels in Kola Peninsula, NW Russia. The seedlings of three Finnish origins (Muonio, Ylitornio and Suomussalmi) were used for establishment of the trial. Based on needle, bud and stem observations, the evaluation of the condition was performed. Surprisingly the condition was better and trees were slightly taller on the strongly than weakly polluted site with significant differences among some provenances from northern Finland. The trees had a significantly higher condition (p<0.05) in the northernmost provenance (Muonio) than in the more southern ones (Ylitornio and Suomussalmi) under weak pollution. On the strongly polluted site, the differences between provenances were insignificant.
    [Show full text]
  • Research Highlights
    [CLIENT] IsaaksdotterIsaacson1803 LEW160651 7 December 2018 Research Highlights GOALS Locate the birth records for three of the eleven children of Isaak Mickelsson and Magdalena Johansdotter (Carlsson) born 15 December 1796: Brita Isaaksdotter, Magdalena Isaaksdotter, and Mickel Isaaksson. (Their birth dates were listed in household records, which will significantly narrow searches for these records. However, locations for those births have yet to be determined. All available records should be used to identify locations for these events, and then applicable record collections searched.) Research the ancestry of Isaak Mickelsson born 2 August 1795 in Helsingby, in Hietaniemi Parish, Västerbotten County, Sweden. His parents are Mickel Johansson and Catharina Johansdotter who lived on Heicka farm. Research the ancestry of Magdalena Johansdotter born 12 December 1796 in Nuotioranta, Hietaniemi Parish, Västerbotten County, Sweden. Her parents were Johan Metsavainio (sic) and Caisa Nilsdotter. Research two recommendations from the January 12, 2017 Project, with the objective of determining who Maria is and where she belongs in the family: Determine who the father was of the young girl named Maria in the 1859 household of Erik Isaaksson and Anna Greta Isaaksdotter. Gather more information about the 1837 marriage of Johan Johansson and Brita Caisa, as listed in Johan’s 1845 household record. This may help explain the birth of the young girl named Maria who appeared later with Anna Gretta Isaaksdotter. If you get to this third objective, I have received additional information that may or may not be of benefit in the research of Maria. We have recently received some research notes written by my wife’s mother about 1970.
    [Show full text]
  • Seudullinen Varhaiskasvatussuunnitelma 2019
    Kolari Ylitornio Pello Tornio Kemi Keminmaa Tervola Simo Sivistyslautakunta 24.4.2019 §46 1 Nimi: Seudullinen varhaiskasvatussuunnitelma 2019 Kunta: Kolari Ylitornio Pello Tornio Kemi Keminmaa Tervola Simo Hyväksymispäivämäärä: Hyväksytty sivistyslautakunnassa 24 / 4 2019 § 46 2 3 1. Paikallinen varhaiskasvatussuunnitelma; laadinta, arviointi ja kehittäminen Varhaiskasvatuksen järjestäjien tulee laatia ja hyväksyä valtakunnallisten varhaiskasvatussuunnitelman perusteiden pohjalta paikalliset varhaiskasvatussuunnitelmat. Varhaiskasvatussuunnitelman laatimisvelvoite koskee myös kunnan hankkimaa avointa varhaiskasvatustoimintaa ja kunnan valvomaa yksityistä lasten päiväkotitoimintaa tai yksityistä perhepäivähoitoa. Paikalliset varhaiskasvatussuunnitelmat ovat velvoittavia ja niitä tulee arvioida ja kehittää. Paikallinen varhaiskasvatussuunnitelma voidaan laatia kaikkia toimintamuotoja koskevaksi (päiväkotitoiminta, perhepäivähoito ja avoin varhaiskasvatustoiminta) tai kullekin toimintamuodolle erikseen. Varhaiskasvatuksen järjestäjät voivat sopia järjestäjärajat ylittävästä yhteistyöstä varhaiskasvatussuunnitelmaa laadittaessa, arvioitaessa ja kehitettäessä. Varhaiskasvatussuunnitelma laaditaan siten, että se määrittelee, ohjaa ja tukee varhaiskasvatuksen järjestämistä paikallisesti. Suunnitelmaa laadittaessa tulee ottaa huomioon paikalliset erityispiirteet, mahdolliset pedagogiset painotukset, lasten tarpeet sekä varhaiskasvatusta koskevan arviointitiedon ja kehittämistyön tulokset. Paikalliset suunnitelmat voivat tarkentaa valtakunnallisia
    [Show full text]
  • Preliminary Surficial Geological Interpretation and Transport Estimation in the Rumajärvi Boulder Field, in Eastern Ylitornio, Finland
    Geological Survey of Finland M149R2014 5.12.2014 Rovaniemi Preliminary surficial geological interpretation and transport estimation in the Rumajärvi boulder field, in eastern Ylitornio, Finland Pertti Sarala Preliminary interpretation of Quaternary geology and till geochemistry in eastern Rovaniemi GEOLOGICAL SURVEY OF FINLAND DOCUMENTATION PAGE Date / Rec. no. 5th December 2014 Authors Type of report Pertti Sarala Commissioned by Geological Survey of Finland Title of report Preliminary surficial geological interpretation and transport estimation in the Rumajärvi boulder field, in eastern Ylitornio, Finland Abstract In this report, surficial (Quaternary) geology and geomorphology of the Rumajärvi-Rajapalot area in eastern Ylitornio – western Rovaniemi with an emphasis on the estimation of boulder transport distance are presented. The study is based on the digital elevation model, Lidar data, field observations, boulder observations, drill holes’ soil thickness data, surficial geological map and literature. Several geomorphological subareas can be distinguished in the study area including active ice formations like ribbed moraines and streamlined features (drumlinoids and fluted surface) and other formations i.e. cover mo- raines and large glaciofluvial deposits/subglacial erosion channels. In the Rumajärvi-Rajapalot area ribbed mo- raine morphology is dominant geomorphological feature. The hummocky type ridges are typically oriented per- pendicular to west - east or north-west – south-east oriented ice-flow direction. The ridges are also covered by the blanket of large, angular boulders. The thickness of glacial overburden seems to be relatively shallow (2-5 m) in the Rumajärvi area and from there to east. To the north from Rumajärvi exist large area of very thin soil cover or in many places the soil is absent.
    [Show full text]
  • Pre-Quaternary Rocks of the Ylitornio Map-Sheet Area
    Suomen geologinen kartta Geological map of Finland 1 : 100 000 Kallioperäkarttojen selitykset Lehti 2613 Explanation to the maps of Sheet 2613 Pre-Quaternary rocks Vesa Perttunen Ylitornion kartta-alueen kallioperä Summary: Pre-Quaternary rocks of the Ylitornio map-sheet area Geologian tutkimuskeskus Geological Survey of Finland Espoo 2006 SuomEn GEoloGinEn kartta - GEoloGical map oF Finland 1 : 100 000 kallioperäkarttojen selitykset, lehti 2613 Explanation to the maps of pre-Quaternary rocks, sheet 2613 Vesa Perttunen Ylitornion karttalehden kallioperä Summary: Pre-Quaternary rocks of the Ylitornio map-sheet area Geologian tutkimuskeskus – Geological Survey of Finland Espoo 2006 Perttunen,V.2006. Ylitornionkartta-alueen kallioperä. Summary:Pre-Quaternary rocksof the Ylitornio map-sheetarea. Suomengeologinen kartta1:100000.kallio- peräkarttojen selitykset,lehti2613.36 sivua,18kuvaa ja2taulukkoa. Ylitornionkarttalehtialuesijaitsee hiemannapapiirin eteläpuolellatornionjoen varressa.kallioperäjakaantuukahteengeologiseen yksikköön:peräpohjanliuskealu- eeseen jakeski-lapin granitoidikompleksiin. näiden yksiköiden välinen kontakti- vyöhyke on tektoninen. karttalehden kaakkoisosassaon hyvin säilyneitäpaleoprotero- tsooiseen peräpohjanliuskealueeseenkuuluviakivilajeja,jotkaovatsedimenttisyntyi- siäjavulkaanisiamuodostumiasekäniitäleikkaaviasyväkiviä.keski-lapin granitoi- dikompleksiin kuuluu syväkiviäsekävahvastimetamorfoituneitagneissejä. peräpohjanliuskealueen pintasyntyisetkivilajitjakaantuvatkivalon ryhmään jasen päälläolevaanpaakkolanryhmään.
    [Show full text]
  • KLL Länsi-Pohja 2019
    KLL Länsi-Pohja 2019 P4 Pojat 4.lk 2 km V Sija Nimi Seura Loppuaika Ero 1. Juuso Korpi Ylitornio 8.08 2. Samuel Männikkö Tervola 8.09 0.01 2. Onni Hirsivaara Tornio 8.09 0.01 4. Niko Vestenius Kemi 8.16 0.08 5. Akseli Lamsijärvi Ylitornio 8.32 0.24 6. Niklas Järvenpää Kemi 8.39 0.31 7. Joel Karppinen Simo 8.45 0.37 7. Lassi Marttala Tornio 8.45 0.37 9. Anton Keskikallio Kemi 8.49 0.41 10. Emil Männikkö Tervola 8.55 0.47 11. Oliver Alatolonen Keminmaa 9.03 0.55 12. Ante Peltola Tervola 9.11 1.03 13. Olli Marttinen Keminmaa 9.28 1.20 14. Topias Uusimäki Ylitornio 9.30 1.22 15. Noel Ronkainen Keminmaa 9.42 1.34 16. Hannes Yliniva Ylitornio 10.37 2.29 17. Veeti Posti Simo 10.50 2.42 T4 Tytöt 4.lk 2 km V Sija Nimi Seura Loppuaika Ero 1. Lotta Rossi Simo 7.28 2. Silja Pekuri Kemi 7.44 0.16 3. Lotta Ukonaho Keminmaa 9.02 1.34 4. Enni Kulju Tornio 9.03 1.35 5. Helmi Niskala Tornio 9.13 1.45 6. Anni Karisaari Kemi 9.14 1.46 7. Ella Rajala Tervola 9.30 2.02 8. Venla Karjalainen Kemi 9.45 2.17 9. Eevi Hokkanen Tornio 9.49 2.21 10. Anni-Maija Keskimaunu Keminmaa 10.02 2.34 11. Saaga Anttila Keminmaa 10.07 2.39 12. Eedit Enbuske Simo 10.55 3.27 13. Peppiina Jansson Ylitornio 12.03 4.35 14.
    [Show full text]
  • Geochemical and U-Pb and Sm-Nd Isotopic Constraints on the Evolution of the Paleoproterozoic Ylitornio Nappe Complex, Northern Fennoscandia
    Bulletin of the Geological Society of Finland, Vol. 91, 2019, pp 75–100, https://doi.org/10.17741/bgsf/91.1.003 Geochemical and U-Pb and Sm-Nd isotopic constraints on the evolution of the Paleoproterozoic Ylitornio nappe complex, northern Fennoscandia Raimo Lahtinen1*, Hannu Huhma1, Laura S. Lauri2 and Mohammad Sayab1 1 Geological Survey of Finland, P.O. Box 96, FI-02151 Espoo, Finland 2 Geological Survey of Finland, P.O. Box 77, FI-96101 Rovaniemi,, Finland Abstract The Ylitornio area in northern Finland is a typical example of a poorly outcropping, multiply deformed, complex Precambrian terrain. U–Pb, Sm-Nd and geochemical data from metavolcanic, metasedimentary and plutonic rocks combined with structural data define the lithodemic units and tectonostratigraphy of the area. The Mellajoki, Martimo, Hosiojoki, Kierovaara and Uusivirka suites form the Yli- tornio nappe complex. Although main thrust stacking had occurred between 1.92– 1.89 Ga, later reverse faulting probably continued until 1.78 Ga. The Väystäjä bimodal volcanic rocks (2.09–2.05 Ga) from the Martimo suite are plume-related EMORB-OIB rocks formed during a continent breakup. The Kaskimaa greywacke of the Martimo suite is inferred to represent sedimentation in a deepening rift basin in the continental margin. The coeval Hosiojoki felsic rocks with A-type affinity and the Kierovaara suite granites (2.00–1.98 Ga) represent dry melting of a dominantly 2.1–2.05 Ga contaminated mafic underplate, and hydrous melting of both the mafic underplate and a refractory lower crust of Archean age, respectively. The older rocks of the Uusivirka suite are early-collisional (1.92–1.91 Ga) and derived from poorly mixed local sources, whereas younger psammite-pelite associations (Ristivuoma) are syn-collisional (1.91– 1.89 Ga) and derive from multiply recycled and thoroughly mixed sources.
    [Show full text]
  • Regional Socio-Economic Disparities in Finland
    Stefan Fina, Bastian Heider, Maija Mattila, Pauli Rautiainen, Mikko-Waltteri Sihvola, Kaisa Vatanen Unequal Finland Regional socio-economic disparities in Finland FRIEDRICH-EBERT-STIFTUNG – POLITICS FOR EUROPE Europe needs social democracy! Why do we need Europe? Can we demonstrate to European citizens the opportu- nities offered by social politics and a strong social democracy in Europe? This is the aim of the new Friedrich-Ebert-Stiftung project “Politics for Europe”. It shows that European integration can be done in a democratic, economic and socially balanced way and with a reliable foreign policy. The following issues will be particularly important: – Democratic Europe – Social and ecological transformation – Economic and social policy in Europe – Foreign and security policy in Europe We focus on these issues in our events and publications. We provide impetus and offer advice to decision-makers from politics and trade unions. Our aim is to drive the debate on the future of Europe forward and to develop specific proposals to shape central policy areas. With this publication series we want to engage you in the debate on the “Politics for Europe”! About this publication On the outset and in international comparison, Finland has developed one of the wealthiest and most generous welfare states in the world and with low levels of income inequality and high social mobility. A deeper look reveals deepening re- gional disparities, leading to the observation that in fact there are four Finlands. Following Finland's post-war industrialisation, the rate of urbanisation and rural depopulation have been rapid, however the country's demographic change and stagnating unemployment rate have increased regional inequalities and put in- creasing pressure on municipalities.
    [Show full text]
  • Kutsuntakuulutus 2021
    Puolustusvoimat 1 ( 2) Lapin aluetoimisto Kutsuntakuulutus Asevelvollisuuslain (1438/2007) ja Valtioneuvoston asetuksen asevelvollisuudesta (1443/2007) nojalla toimitetaan vuonna 2003 syntyneiden sekä muiden alempana mainittujen asevelvollisten kutsunnat Lapin aluetoimiston alueella vuonna 2021 seuraavassa jä~estyksessä: SUKUNIMEN AL- AIKA TOIMITUSPAIKKA KUNTA KUKIRJAIMET Päivä Pvm Kuukausi Kello Utsjoki Aaa-Oöö TI 17. Elokuu 12.00 Kunnanvirasto, Luossalie 1. Utsjoki Inari Aaa-Oöö KE 18. Elokuu 10.00 Kunnanvirasto, Piiskuntie 2, Ivalo Sodankylll Aaa-Oöö TO 19. Elokuu 10.00 Kunnanvirasto, Jäämerentie 1, Sodankylä Savukoski ja Aaa-Oöö PE 20. Elokuu 10.00 Kunnanvirasto, Kauppakuja 2 A 1, Savukoski Pelkosen niemi Pello Aaa-Ooo KE 25. Elokuu 10.00 Seurakuntatalo, Lapintie 3, Pello Enontekiö Aaa-Ooo TI 31 . Elokuu 12.00 Kunnanvirasto, Ounastle 165, Enontekiö Muonio Aaa-Oöö KE 1. Syyskuu 10.00 Ammattiopisto Lappia, Koulutie 8, Muonio Klttlla Aaa-Oöö TO 2. Syyskuu 10.00 Kunnanvirasto, Valtatie 15, Kittllll Kolarl Aaa-Oöö PE 3. Syyskuu 10.00 Kunnanvirasto, lsopalonlle 2, Kolarl Posio Aaa-Oöö TI 12. Lokakuu 10.00 Seurakuntatalo, Sysitie 7, Posio Salla Aaa-Oöö KE 13. Lokakuu 10.00 Seurakuntatalo, Tennontle 7, Salla Kemijärvi Aaa-Oöö TO 14. Lokakuu 10.00 Kulttuurlkeskus, Hletanlemenkatu 5, Kemllärvl Ylitornio Aaa-Ooo TI 26. Lokakuu 10.00 Kunnanvirasto, Alkkulanraittl 55, Ylitornio Tornio Aaa-Lep KE 27. Lokakuu 09.00 Peräpohjolan opisto, Joentalo, Klvlrannantie 13-15 Tornio Leq-Oöö TO 28. Lokakuu 09.00 Peräpohjolan opisto, Joentalo, Klvlrannantie 13-15 Rovaniemi Aaa-lmp MA 1. Marraskuu 09.00 Rovaniemen varuskunta, Someroharju Rovaniemi lmq.Man TI 2. Marraskuu 09.00 Rovaniemen varuskunta, Someroharju Rovaniemi Mao-Rom KE 3.
    [Show full text]