地質図幅説明書

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6 Ⅺ Ⅺ Ⅺ Ⅺ Ⅺ Ⅺ Ⅺ Ⅺ Ⅺ Résumé

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10 km m

11 ,m

12

13 flatlava

14 ,m

15 NWSWNW NE NWNE

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17 m

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19 NE

20 ,m cm.mmmm

21 flatlavaplatylava flat-lava

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24 cm m cm

25 m m

26 ,m

27 km m m,.m

28 mm km

29 m m

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31 mm km mmm m m

32 m m m m,m

33 m,m,m,,m flatlava

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35 ,m,m,m Schneekoppe,m Sonnblick Zngspitze,m

36 ,m.,m..,m m m

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38 m

39 cm m,m m m

40 ,m,m

41 ,m,m m m cm m cm cm

42 cm

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44 cm cmcm m 塡

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46 cm

47 Ⅺ Ⅺ Ⅺ N WNE cm..cm m NW

48 WE NWNESWm mangtaggtcu Pb.Zn.Cu cmmm Ⅺ km m Ⅺ Ⅺ m C

49 Ⅺ,mm C,m C Ⅺ

50 m m No.No m No.No

51 No.No.No Ⅺ m

52 km

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54 Vol No Vol VolNo No No No

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56 EXPLANATORYTEXT OFTHE GEOLOGICALMAPOFJAPAN Scale ASAHIDAKE Abashiri By MoriakiKōnoyaTakehiroKobayashi CheoulWooKimandShinpeiKawachi GeologicalSurveyofHokkaidō Résumé TheareaofAsahidakesheetmapissituatedinlatitude NandlongitudeE.,andislocatedin thedaisetsunationalparkandbelongstokamikawatownhiga shikawatownbieitownandshintokutowninhokkaidōthe Daisetsuvolcanicgroupisincludedinthissheetmapandthe neighbouringdaisetzusheetmap Topography TopographicallytheareaisdividedintotheDaisetsuvolcanic groupandtheirbasementswhicharedistributedintheeastern andwesternpartsthebasementintheeasternpartismainly composedoftheslateandbasemanyraggedmountainranges peralleltothestructureoftheslatethewesternbasement composedmainlyofthepropyliteshowssteepmountainthe Daisetsuvolcanoesarecomprisetopographicallythebroadrelati velyflatplainscomposedofbasallavaflowsdomeshapedmounta inssuchashakuundakeandtomuraushimadeofveryviscous

57 lavasandtypicalstratifiedvolcanoessuchasasahidake InadditionlowflatplaneisdevelopedalongtheIshikaririver inthenortheasternpart Geology ThegeologyofthisareaiscomposedlargelyofPreTertiary HidakaGroupMiocenevolcanicrocksandsedimentsandmany lavaflowsofthedaisetsuvolcanicgroupwhichcovertheabove mentionedformationsinadditionquaternarysedimentsare alsopresent PreTertiaryformationisrepresentedbytheslateofthelo werhidakaformationbelongingtothehidakagroup TheMioceneformationscomprisetheKaunnaipropyliteand YanbetappuFormationTheKaunnaipropylitewhichisexten sivelydistributedinthewesternpartoftheareaisakindof compositeigneousbodybeingcomposedofrhyoliticandbasaltic propylitesinsomeplacesbothholocrystallinefaciesandgreen tuffareassociatedwiththem TheYanbetappuFormationislargelycomposedoflatered palegreenweldedtuffsandiscoveredbynormaldepositscompo sedofthesandstonsintheupperhorizon ThePlioceneFormationsincludetheTomuraushiweldedtuff andtheuniishikarilavasthetomutaushiweldedtuffcompo sedofrhyoliticweldedtuffcoveredbytuffaceoussandstoneis welldevelopedinthisareaaswellasintheadjoiningareaofthe sheetmapoftheupperstreamofthetokachirivertheuni Ishikarilavacomposedofthehyperstheneaugiteandesiteisde velopedintheeasternpartofthearea Theothervolcanicrockscomprisethelavaflowsrelatedto theformationofthedaisetsuvolcanicgroupandcanbegrouped intothefollowingstages ThestageoftheformationofthebasementoftheDai setsuvolcanicgroup

58 ThestageoftheformationoftheOlderDaisetsuVolcano ThestageoftheformationoftheYoungerDaisetsuVo lcano ThestageoftheformationoftheAsahidakevolcano OfthesethestagebelongstothePleoPleistoceneandthest agebelongstotheholocenethelavasofthe stageinclude thebieilowerlavakoganegaharalowerlavanumanoharalava MidoridakelowerlavaKaundakelavaPonchūbetsulavaKogane gaharalavachūbetsudakelavaandtakanegaharalavaallof whicharetwopyroxeneandesitessomtimeswishwelldeveloped platyjointtheyarecharacterizedbytheirextensivedistri butionformingflatlavaplatformsandareofthesocalledflat lavatype The stageincludestheolderdaisetsulavausiroasahidake lavahakuundakelavatomuraushi stlaveandndlavaall ofwhichbelongtothehornblendehyperstheneaugiteandesites withcoarsegrainedphenocrysts ThestagevolcanicsisrepresentedbytheSounkyowelded tuffhyperstheneaugiteandesiticincompositionitsgeologicage isthelatepleistocene InadditionthefirstterracedepositstheHakuyōdairaforma tionandthethirdterracedepositsallofwhicharepleistocene orholoceneinagearedevelopedinthelowlandalongtheishi kaririver GlacialandPeriglacialTopography CirquesduetotheglacialerossionaredevelopedintheKo ganegaharakaundakechūbetsudakeandtakanegaharaandthe iraltitudeishigherthan,mabovethesealevel Periglacialtopographyincludespolygonalsoilsstriationsoils andstonepavementsallofwhicharealsodistributedintheal tiude Economicgeology

59 Anepithermaldepositofcopperleadandzincisfoundinthe midstreamofthekaunnairiveranexplitationwastried oncebutthedepositwasabandonedowingtoitspoorquality Theminingofsulfurwhichwastheimportantnonmetalicdepo sitsinthecraterofasahidakebeendiscontinued Hotspringsareabondantinthisdistrictandmanyof themareusedforbathingsuchastenninkyōyūkomanbetsu andkogenspashotspringswhichissuefromtheupstreams ofyambetappuandtomuraushirivershavenotbeenutilized EspeciallyalongtheupstreamofTomuraushiriverhotsprings higher aredistributedforthedistanceofaboutkmand muchsteamiscomingout

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