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Bergkvalitetskartan Del Av Kungsbacka Kommun, Skala 1:50 000

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Bergkvalitetskartan Del Av Kungsbacka Kommun, Skala 1:50 000 SVERIGES GEOLOGISKA UNDERSÖKNING SGU serie K 96:1 Häll (enligt SGU Ae 20) Outcrop (according to SGU Ae 20) Bergkvalitetsklass 1 Bedrock quality class 1 Bergkvalitetskartan Bergkvalitetsklass 2 Bedrock quality class 2 del av Kungsbacka kommun Bergkvalitetsklass 3 Bedrock quality class 3 Bedrock quality map Stenbrott, nedlagt Quarry, abandoned Skala 1:50 000 Stenbrott, krossberg, nedlagd täkt Quarry, aggregates, abandoned Lerum Blocksten, nedlagd täkt Öckerö Partille Bolle- Dimension stone, abandoned bygd Härryda Borås Göteborg Litologisk kontakt Mölndal Lithological contact Spröd till plastisk deformationszon, ospecifierad del av Mark Brittle to ductile deformation zone, unspecified KUNGS- BACKA Strukturell formlinje för plastisk deformation, delvis indikerad med magnetiska data Sven- Structural form lines, ductile deformation, partly indicated by magnetic data ljunga Lineament, indikerat från höjddata Lineament, indicated from topographic data Varberg Falkenberg Vatten- eller lerfylld spröd svaghetszon, indikerad från VLF-data Brittle deformation zone filled with water or clay, indicated from VLF data Hylte Provpunkt med provnummer DCL031006A Sample location and sample number 1,1 Mätpunkt för bestämning av radiumindex (rak text) och aktivitetsindex (kursiv text) 0,8 Location of radium index (plain text) and activity index (italic text) determination Mylonit M Mylonite Djup till urberget, < 2, 2–5 och >5 meter (data från SGUs brunnsarkiv) Depth to crystalline bedrock, < 2, 2–5, and >5 metres (information from SGU’s Archives on wells Starkt förskiffrad berggrund Strongly foliated rock 2008 Radiumindex är ett mått på mängden radium, som ingår i ett material. Detta index skall för byggnadsmate- rial vara mindre än 1,0 (BFS 1990:28). Radiumindex = 1,0 motsvarar ca 16 ppm uran eller 200 Bq/kg radium-226. Aktivitetsindex är ett mått på den totala gammastrålningen som avges från ett material. Beräkningen av aktivitetsindex sker med formeln mγ = CK/3000 + CRa/300 + CTh/200. CK är koncentrationen kalium-40, CRa är koncentrationen radium-226 och CTh koncentrationen torium-232, alla i enheten Bq/kg. Aktivitets- index mγ bör för byggnadsmaterial vara mindre än 2 (The Radiation Protection Authorities in Denmark, MAGNETISK ANOMALIKARTA Finland, Iceland, Norway and Sweden 2000). f g h i j 8 8 7 7 DCL032006 DCL032007 DCL032008 DCL032010 6 6 N N N N Kungsbacka 5 5 Lygnern N=30 N=40 N=40 N=40 4 4 DCL032012 DCL032014 DCL032015 DCL032017 N N N N 3 3 Åsa N=15 N=23 N=40 N=40 2 2 DCL032018 DCL032020 DCL032024 DCL032026 Frillesås N N N N 1 1 f g h i j Anomali (nT) –201 –157 –130 –113 –100 –88 –76 –67 –58 –50 –41 –33 –26 –19 –11 –4 3 10 18 25 33 40 49 58 66 76 88 99 113 129 156 200 N=40 N=21 N=40 N=40 Magnetisk anomalikarta över del av Kungsbacka kommun (skala 1:250 000). Magnetiska data är reduce- DCL032027 DCL032028 DCL032029 DCL032030 rade till epok 1965.0. Kartan visar totalfältets avvikelser från DGRF 1965.0. Kartan baseras på flygburna N N N N mätningar utförda 1974 och 1991 på 30 meters flyghöjd, med ett linjeavstånd av 200 meter och en öst–västlig flygriktning. ELEKTROMAGNETISK KARTA (VLF) N=42 N=23 N=40 N=40 f g h i j 8 8 7 7 BERGGRUNDSKARTA f g h i j 8 8 6 6 7 7 Kungsbacka 5 5 Anneberg Lygnern 6 6 Kungsbacka Stensjö 4 4 5 5 Lygnern Fjärås kyrkby 3 3 4 4 Åsa Tjolöholm 2 2 Gällinge Frillesås 3 3 1 1 f g h i j Åsa St Hornsjön 2 2 Promille Frillesås 989 924 941 951 961 968 974 980 974 980 985 989 994 997 1001 1015 1022 1030 1039 1052 1069 1095 1151 1 1 Elektromagnetisk karta (VLF) över del av Kungsbacka kommun (skala 1:250 000). Kartan visar den f g h i j relativa totalintensiteten av det sekundärt inducerade elektromagnetiska fältet, vilket ger ett mått på den relativa elektriska ledningsförmågan. Kartan baseras på flygburna mätningar utförda 1974 och 1991 på Provpunkt för teknisk analys Granit, svagt gnejsig eller ådrad, anatektisk (60) 30 meter flyghöjd, med ett linjeavstånd av 200 meter och en öst–västlig flygriktning. Sample location, technical analysis Granite, slightly gneissic or veined, anatectic (60) Spröd till plastisk deformationszon Granit, gnejsig och ådrad (71) Brittle to ductile deformation zone Granite, gneissic and veined (71) Starkt förskiffrad berggrund Ögongnejs (72) Strongly foliated rock Augen gneiss (72) 1600 suite Mylonit 1600-sviten Granodiorit, gnejsig och ådrad (73) Mylonite Granodiorite, gneissic and veined (73) Diabas (24) Tonalit, gnejsig och ådrad (74) Diabase (24) Tonalite, gneissic and veined (74) Pegmatit Äldre, mafisk intrusivbergart (76) Pegmatite Older, mafic intrusive rock (76) Granit, grovporfyrisk (Askim, RA, 50, 52) Ytbergartsgnejs, fin- till fint medelkornig, av Granite, coarse porphyritic (Askim, RA, 50, 52) vulkaniskt och sedimentärt ursprung (Horredgruppen, 83) Granit, grovporfyrisk (Stråvalla, 53) Supracrustal gneiss, fine- to medium-grained, of volcanic and sedimentary origin (Horred group, 83) Granite, coarse porphyritic (Stråvalla, 53) 1300 suite 1300-sviten Mafisk intrusivbergart associerad med 1300-graniterna (54) Mafic, intrusive rock associated with 1300-granites (54) ISSN 1652-8336 ISBN 978-91-7158-813-5 Ytterligare information finns i den separata beskrivningen som medföljer kartan. Undersökningarna av Kungsbacka och Varbergs kommuner påbörjades år 2003. Följande personer från SGU har deltagit: Mehrdad Bastani (geofysikmätningar), Hossein Shomali (geofysikmätningar, tolkning), Christina Johnsson (extrageofysiker, geofysikmätningar), Mattias Göransson (projektledning, provtagning, tolkning), Ulf Bergström (provtagning, tolkning), Fredrik Hellström (provtagning, mikroskopering), Thomas Eliasson (opakmikroskopering), Anders Hallberg (mikroskopering) och Jonny Sangskar (extrageolog, mikroskopering). MRM, Luleå har utfört de tekniska analyserna. Jan Trädgårdh, Cement och Betong Institutet (CBI), Stockholm har bedömt risker för alkalisilikareaktion (ASR). Kartan och den kortfattade beskrivningen är sammanställd av Mattias Göransson, Ulf Bergström och Hossein Shomali. Referens till kartan: Göransson, M., Bergström, U. & Shomali, H., 2008: Bergkvalitetskartan del av Kungsbacka kommun, skala 1:50 000. Sveriges geologiska undersökning K96:1. Reference to the map: Göransson, M., Bergström, U. & Shomali, H., 2008: Bedrock quality map of part of Kungsbacka municipality, scale 1:50 000. Huvudkontor/Head Office: Filialkontor/Regional Offices: Topografiskt underlag: Ur Vägkartan. Sveriges geologiska undersökning K96:1. Box 670 Geovetarcentrum 0 1 2 3 4 5 km ©Lantmäteriverket. Ärende nr M2005/2355. Besök/Visit: Villavägen 18 Guldhedsgatan 5A Kiliansgatan 10 Skolgatan 4 Box 16247 Geografiska längden är räknad från Greenwich, Gauss' projektion. SE-751 28 Uppsala, Sweden SE-413 20 Göteborg, Sweden SE-223 50 Lund, Sweden SE-930 70 Malå, Sweden SE-103 24 Stockholm, Sweden Tel: +46(0) 18 17 90 00 Tel: +46(0) 31 708 26 50 Tel: +46(0) 46 31 17 70 Tel: +46(0) 953 346 00 Tel: +46(0) 8 545 21 500 Godkänd från sekretessynpunkt för spridning. Lantmäteriet 1996-10-30 Fax: +46(0) 18 17 92 10 Fax: +46(0) 31 708 26 75 Fax: +46(0) 46 31 17 99 Fax: +46(0) 953 216 86 Fax: +46(0) 8 24 68 14 Skala 1:50 000 E-post: [email protected] E-post: [email protected] E-post: [email protected] E-post: [email protected] E-post: [email protected] URL: http://www.sgu.se SGU Serie K 96:1 © Sveriges geologiska undersökning (SGU), 2008 BERGKVALITETSKARTAN Medgivande behövs från SGU för varje form av mångfaldigande eller återgivande av denna karta. Detta innefattar inte bara kopiering utan även digitalisering eller överföring till annat medium. DEL AV KUNGSBACKA KOMMUN .
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