52F11NE A.49 BUCHAN BAY (EAGLE LA QOIO til»l% S»tD» Hoe.
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1 52F11NE A.49 BUCHAN BAY (EAGLE LA 0 10 * ;.«; Oi.:oLCGlC&» QOIO til»l% S»tD» Hoe.
2 S2F1INE02S6 63A.49 BUCHAN BAY (EAGLE LA 010C ftni Conclusions of.":>«.rf«.e0 1* Inirodluotlon 3, 3 f Ct I* S Iron C* A d* 4 ru Folding b* Fnultlng d 1* for *-> of ion» X 3 tu Loecttion 0 c»» potion B A S600 I 00 t*» 900 fft«t oortsh iio^t non *9ttth 1, Loo&tlon /I 3,000 tu Loofition fait
3 YOUNG, YOUNG & GROSS, LIMITED CONSULTING MINING ENGINEERS ft GEOLOGIST SUITE 1O07, 67 YONGE ST., TORONTO ho *m Gold iliii«t% 3»t&«Left* ATM* Ontario a «j a of OK this i»ouril* rh distributed on the j/wjifhsrty nnft vti-lus e.iv.1 stri.igerb filling y,?iri4 in sulphide repl«eej*eiit the Go-c^llec! J,,on6 1 Ift Ww frora the varlou eoureee of lo R co of hi:?s i-t lt>ri{?,th of is B.j>proxls»toly 100 feet, 0*146 O K«fjoJWl ovw 40 ch we open *ii ne or both 0»lc* Of * nisj>0sr» to htsvo the ehonh be d rilled at o toec worfe *h&# tte&* &o1& IB In 1» ta, th lava of In of ^>14 fotiod to d^te oeoa^ i» off srat*r cm <?f fit GOrafelnni $?:!,$ eite«tilmt this AMHurtsUi 60 wow 3 4
4 * a * Ctoor'Hyeionl report; ) A'hiauo e>on**& wore f.isjjdcje whore rock ocourroa «ra oheofcqa for they.*«ro T-OVCHSM! by tw*rbui*«tf»)» JKwao of thi?0e rotioo wiso foum to oon* te>in f*o M 1» Bi.u^i c(mo*mt r«t tone e» & m X imit ik^llhi^ of feliee* s wfio lisa tea b;f t ho ovortntrft^tti *IM> Wttred ««*oo Aictf»ho0tie«^hat I is tho ffiot tliet tjjoi^j^itej tjsi^ tftait fcfc^nrit- teltw in nna 0 true turo to :«ite of 8'ilpM$.CHs over lefip oreu»--a.f» potent irfl miwc/u* It i«j^otm- b%o«^tetfttfof! ttefc «>s»0 ^r IMI in thoeo aul >hlc!0.oonocntt^tiolte aas t* r «i<a»»aa tliat eeh *f 3 6«i 4 be t ttio }* f9t«h6 ' ««3 ««It«*y#t»ont inl. tarvty»# It tbftt th«&«r.orie@ bo drilm *f't«(f t]mi «X»lbi«ti6ii»f ^QJM it In this v«-^r they ro %?*tn as or@ pot«ikl»ia A.vl»«i( Hktt taltte ^P ton* I hoe beijii defln^a. A lur{? portion of tb«jpttfwrty to -.tthattf1^!!! iflp. VooK* are wore or le»e f^noturod awl fillo&'ttitb p r:tt ' s^rliiiis^et A nuiitiox' fit (s^isples has bot^n tciltoft -frott ftoncrt.lly vetiturned io»^ ow VidtttB* n- pjci. ^'-vc ]-ot,*irnoa V!:lucn> in tht ounooo end free gold ftoe boon foutvx in the <iu«rtb in. n noraber of i>li»eoa'(ihm» M«,^«^*l7fi»l@')# I* to fri:totiusr 3l l«4ioo way- o^bi&tn.-oi'o' vriiiob.to >e of ov rbmt40ii*. 9tio 'ojfoeo of >ftooli.aii'i^* ona a Bilftifc inoroaoo til tho w jr«t«fiwao'-of ' t>b o ' pooeimlity of it>%jioneo :%o»»eg@«i of 3L0s#*p?«i4«.-f»l«l'iisl,t A ount -of Arilltnc; on thto type of 0o)4' aodttrt'oiido i» ret* ana tho locfttion of th«$o
5 M Si & a -i* S *" '"*' 1 4 I a ;.* V>* a 8? i.-^b sj o i * o a ^ ^ 5 ^ ffi S AJ 3 «L f? J4»t sx- ^ fii Sn s >fc S O O (& 3 ^»' O r-4 ^ fo C C;.^i' * S V-, * V* O Hi HI * 1 O SS «IS I* - S «r «* o & 1 -*» o *««. Gk e<& 1 J3 S 2 E TWT I o s o J* «8 O ts «*- f w t*fc <*>««? J if» -4 *» a a 4$ S3-3} O a ^ 3D jyfc ^S^ t S 1k * a* S «J «** o» *»!5 I s o $ s «1O s o ** w o a* S3 * O w«t w o a a t a 9 * * of ti S - 0
6 4 * em, be n by inepotttion of tthe inolu$e& #9i»&? «ionp tfeo oeet *r$4«of Mi IsieM us? the now nt «>3* nor* encouraging ttem noin t-iichjlnr, or* two 1 h s; been fourvl as reeull of tho j!ioyf e worlr* -i-'ho t^nown fp-cte ooucemiiig this Hooattou ^re ^to'/b on tiho iv.?:i ioolte plon (fc*s6) &nolu<l09 in tffeis report* 'i'h Is j>lc,r th)c'.>-fi vho r*ooxonyi HoM voiuesi me^iioteio o on t cure (.T4 :-.-ono J3 ro u,v:«ju ovor 1U foo «a» Count on voluoti lio <j i n 0y,t In pared t.i> ivl-o.tf vhr* i»w vf-lw 8 veitui on»ofe foot itoi'!.h ci; is { i>!,o*:i' -4th e / loifif; pr.rt of i trs lojir-tli, *,'ho of volt* of to it In
7 i?trihe& into low ffwniapy ground wiiilo tho on i>inohei> out In tlw trenoh* i*h showing lies in ft i/ttfmctio condition uhion. pwalet for e ires?ai hundred feet off buth on4ft of tune trenob* this ohowlni; 3iay y^ti h? eom O0ot)omlo importcmoe eo the ij 00y pxflii to6» t>0eti In01u<to& in this p Ooutoredi or* tind B J.300 f *«t north, an intrueiv (V) porphyry oout&inin^ cmax>tii«fill«4 f'vniotttf'ttk H«v 3Usw f,olvl v<u,uc?e cjver a eoimidex'dbx^ er fi* i'li n«ta the vcilaon obt&incd et isftioetwt ^X»o«0 aeyoaa th» of tho urefa* vhie location Maarv a «i>»»i ^«woifitel.ft-»be' to jx-u-t of uiso ornleri ifef etiotiian uter qun iii*ii*c's*f»<i^ ^ug^r quart* aaaaaa & low vt luee* o the ttmnactry bt»i««i n OlnitMi lilts a»j vory io.i vr.lsiioo viorc obtained* vhcr ti*aiio»i U CMI aloas the ntrlko of «n irret^il^s* < u$trtfe v«sift w«ife of t &OOVPO native r.-e-m wi*o obtained tvm t lw> vein in onvity but u ohiitmol eoroeu the tf«lft etmhit 0 feet t<iritoa G trtu'.e of foj4* t!h 0ho«r etil vinrt* vein to be i/ he result oi" relief of atfe&e throaflb roeka of foront coi-ipotenoy roeiltin^ tfi e fraetttre io tlie c; t!»0 vein 6na ahe^rifeg in the oow ;» «t BLOO «N*t» ao«th Bdmarali*ati0n in
8 no
9 Lake ar o we iaftppm in of M on.\ report mipplocaonte tho limits i*@r Ofia3L of ibo lor/wr fe^turoe «nl^h.extend of t!»o.k 1'he in tb i'ollddvinf?: tf»v>x«of *» uand/» 0c id and * iron fomati<m t-oli** i'lio omoei focke are light to <les*k c- i-i\,h nitior Uftettlte iis \,,JQ lifu'klo Hot; in tiho tjrcm of the M&^ ho?'i*ono nre coii-.-.on but fclio iimiiivi4it«il piilows es^j ouly
10 * 0 * of uco in a etortjlnlnf; fxcw top** JiayipJUiXeii in the.pillows c,tj.*c not raro u ni the Gonaontrrotiori «t tint of j>ixxo.m WMO of tto-o It* etraotural d^fcojktiimitiotw* i'lie 6!3y$iul<si;?^y 'bo quflrte or o Xe!t0 thty to bo idtnorelibod b/ milphuea* I'lw lavm wjtb oo!iictoc?iiiy of a minor <!0ftree ilutelopm la f»l t» e «re thd etreee ho0 been c! ou^ovop in tho vioinlty of ti» iav^tt Ho were eeon hut tfte. GmphtboXi^ea a,ra 4>on«i4-areA to «aiterel wi,l 3;^otye%filiifeM aale«4^ «ttw» tiees^by pti* ot; JinvBC ore in t»!io aiapfellioilt eteg of ia@t»t*irptiiiki to uuboto.ntiiovo this (ibuur<i)tior* of Xoitn sixiewmfi iroti or bnftlei ohort occur in the b&slc fxo^tt nlong Dliore of iioraitick );^iy# ooooelotuixlyt tla 6 I0«ia feet in i. iciuioos, but 1*2 INMt ie M&uaXt in laoofe of thoi.o i-f.ntlw the r-iornotito contoat 10 er^lx 'but in»0 narrow bfjivi onoufjh namiokito m & prteenl to cau^ in tiso coiipnfes noo4xe«of tiding tii v;a ie fl Ciorlcn.: of uoid oiwl int«naoaifi%o Xev«e nut-3oroue Koouf<tin porphyry boaiea* Xn imppit^ theso rooka conbid«r«bxc diff io'ixty wwo snoouriter! in ore <*il cor'oiicrt-bx/ elttiroa.en^ vmy or M*y not Iieve nrfcr phenooryts'to* oit'\ixoray» tine fexaepfir >l»«nooryttt* / be qttitc frcfc:; or i oi fcl* other «Ktv0&ie«
11 only in thin #eotlon» contaat relations w i» *av$i? e««*jr artl the boot erituseitt w::^ the distribution of tha oatoroi*! ft eu-oulor or olli.i>tiopl ftiattibattan toeing tokan ae wi to* dloation of thw intr.ielve *i*\tttra looking rock* 'Jlio rhyoxitaa wera usually uorphyritiic with which rat/»aoh iaoii in fron fine* tsjo den&0» th«latter often a toyy in eon oe.ssos nt 10a t* i'jiie ei.'orty rh/oxita we«oc»n to tee ;->ohitited nni aggloiaerfttie qaivalonta of and Intereneftlntfi flo»;0 nr foubjl o» tha areae hnv boon r^ >pod«gn ie tr«a oj-j t?-tft iiorth«*t)at)t seoticm of tho igpoup* fftese roo&s pooeibly AorivM frora tuo intanaa»!i aring of ooidio flo</i;» 'i'-j«o^ c:ro llflti in oolo* nua vtrir of% 4n to 6Ss@ hi(t of or:4oito pt^fjont in part as vaialatra out i*»n)gtt3u*r a(vlom*jwh6 ic pwstebly of i.i4t@»ms4ieto composition, ff ft dnrk oolordd roefef $h fj*ag^iint»6 range in sit* to ir.\oh disi'meione Umt, in pitt0 0 it ie nora >p im.i»iy tt well.i;^,-kv;(u ;i'li0 rooks zaappaft «@ Aetoitaa ineluaa tnoaa v y os? grecm rooho ivhioh oou34 not ba is6^p«t a rnyolitna or tux- of tho outoropa aspp«4 as &.0ite»af ba 'i"he letyaa ahew uo tbe &%truaiva natmrp of tha roaka ia )'>oth tho alteration: awa tha porphyritio tarn* tura vftry fro.'., plc-.aa to px&oa' ifutraaatnis tha 4iffl0oXty in rocopj)ii?.inr the continuity of the flow» froia outcrop to out crept
12 * IQ * r^10 roefco intruoivea «K? r>o;nuft«8i wot &* «<' ** lirht in c>;lor cma t.he phteoor^efc elms? up pn euh'f*fje oven when ftl ei^tl<4» land-he thoir appear(*ao«in the i>rokon rook* Vresh) ttfmil«(ip@4 portion* give trtse ojt boitir porpli/r/ 4{tk»» fettt- iaeje of oo»%aol& tl;gt title io o ftrodntioiiel cii«si? * fh» ft?urnt'i only lr> tho so it! «to the erowter vi&ooolt/ cinft oonm^umt 4 ffi««lfy ia ^ the moro «oj4 raap tiunwroua 4ilc«J4 and till of j,$ m» JKMP* c^re fotwd in foil type -of Ite^stitt Jtavati Sl»*»» boon fjnppo4 f-,e an* fo!4&pti i--u^t'.e^'toct u.^t theoo K«F f ows Mrioe fron ond to tbe Q««rt» end* 'i'he oviaeneo tk t» on l»oreneo in t!:o «Uor«ition of the faldspar fdtoikootyfttfi with fm Inoroivcte in the 01r.cs c\i^ mimber of tj«ert«phonoor^fii^* Vheto tf..4iot)» which i3*!y ba either dike r «ill««ar mm* rrow, of feho orjtor of io*ft-of««% «a «K«0pti«n le %h«ih»rp»»yry 4iko -^bion 1 founft on elate Ho«IH109 tia 'i north *>n^ south bayonfl t?ie el.ato bottf«9l&ri«s» fhi 1-06 &»3fitJtlrMfci aidttj of vcine on tiio :>i40jx»rty* Two known ftftottplfta aj? u^iieu wf.jcit nave» parent ly raoponet a e
13 tmvition «w..u.v<cj ro pro rent «In earse of the&0 oay&ticfcit niisl pyrlto cubes ei*$ tothkhodff* h«v«i:rt» r*ieo oooure ee frooturo fililfi^e in vtirloue /*i In en?sii rooke I'ii on tt> aroperfey* fliiti stctions hav* to in fore r,iiifl. on t;>o north «m?i of the pr»p«rt r i in t-hsee roelsc? Iiuve boen obneyted to fe both, runt (ratlitnci the i'he boirooh oover ^n *h» pi*op@rt r is a j^et reach aoaas4?ebi0 & pth to ma.a frm the naribgir of utis^ocanflfttl fi.lteb.pte to tmn^i tehrottgh -..hci-e UK o).oy hnw boon Wf*eh«* omt f*x»f ttj «hoi» fin * Ho eiiibl l»»oo to fomlni 4 ia fi^enoe»n the y t*;--io;i ovorlioa the function of tuo taliloi11 stmofeu.ifix t.:. of the fcogi l*ak areui 'fheoe fdattafes are the two trou^he otrilcln^ fepjiro^imstfl^r ftortheoot Hit»tmth l* >.'he letter i e oonr.idcn-ccl >y i» W» MoorhOttW to bo o irti>rnl o/.tun&ion of tho fofnor* w* H» QJPOSB
14 * IS * ti»eit the* Bottth»0!»3t-iking eynoittio In a e?00t*fo!ml on ctfcrueturo* HIB thoory explain* th» DorttwioutU the f& ny imtruelvo porphyry lukee l«thai Alytolio to feootftottsf no f milt toft of ti ipori.\'*nee,-*?:o rtoofnir&l in ti:o ptreeg«8 were aooonnotevfft tof flhetiiptttg «.»! hou fraoturlnr* olr>i.nfo irrtioh of th» rock i»» ti» vielnifcy of roliof of t«t;rth,-.e hore P»^ UBVO Inv^lviMl fnuitlng* evld(?nce etiij/, oet*j t^o iir«f» of oitaot wtiieh miy b o«ly one of thooe hoe «iy aof inite flold oviacnot? $0 the contention* noin trenoii on i;ono 1* Ji'bia'offofit rani tu^h*norfchif*«t tm»m Along, this lino atrlkinf; porpliyry ulikoe Xridlefite MCMI etlrtietural «f««j(fift*0 ^v.-icti,''«x^ilttal tjjolr Intrasiotit j&ottt 00 f«ol weefe of lino a noi'th tronaln^ VfilUgr MporHtea aeia fumrs fvon Icjyctcj out orope fire rare in the orifcioui points m It is not i?t«x,n \vith certainty that thoj^e le e 40fliil%e»ff«l wiiofciaes' tlso ivp^wenfc offsets ie 4iM» to tbo ii«iwk>ttu intx^aolvoo i-jiifih. j;y.iy Uive inv«il0,l trie Iwwts north./est of *'he of feet running ocmth frora i4n ^ «*t ebc.ib on i»[jo ir:-.;*ij:ic?tio eoniottr asp* 10 not iserfcodi ««a faitit by fiwm ot>norv'.-.wicm* - ett ^efeion of lies in tho enplaoomont of porphyt^ aikeo u 1m t If» fault fteiefce thero ie no hfhftwnttel of!,';irj0«j» vol» 40, pt* 4* (mtovio
15 of ftmlte on the porptyrar dike <w* Claim io indirect m*l ehoi?8 up an the.&eglofrio<*3> jwp us a result of tho <110i,ribul,ion of the oufcorope, the fault ttwfaoo hue not boon aeoit it) «ny oas «fh» ijftr^hyri' fiifed In thlc onee itentlf probably oeoupiee a fault with»«rar»i«ll hor bo Bio voioanioo -hv» l»y eii-oariiig otrcda. Ciil«i»iti eoneb era wet&f ita$wni*teat t reor/otftllieed to u oonflidoroblo oxtoi»t, tb«ere no,; n ffctyrofentea fe nrrojy elbitiswi *» %tot «tkjr tiioy have been obliterotoa* tn oonteaotf the ore rcpreconted in pleoee by lai'fia areaa of a r&or*fi%e ciorlcite ocji iatio* - In pleoe0 the oeohinettion. of *%vee* and ooi;ipr-tcncy hfi«betsn «ueh e» to deteiep neither fmilte nor uometff in the rook bat roeultin^ in the pvodttetion of fracture cyctcme in definite pstttjptwji flie roiike oorft aiuittg t.'icc frnotured «yt? tbe porp^ritie type «s.n^ eppavently In* trnoivo UP well 0:i5 «ctinieive roeke are fovowftble for their developr^ont* i'he frnoturee 11 in three diveet lon«t o»e of which ie ;>re4onineint«a eeoorvi of leeeer latportane* end a third of very Minor total tyi&ntity* fhese ettnetaree ere invorinbly uit-h ^uert B uad may or nay aot earry
16 ^ ooaqq,
17 A m»i x\ O?^l _^ T I-* \ t N /A 1 /.>y '? *» <-«* *H~ & i$/ * K * Pi K ''»-..,-' L, Mm.if ok L, ik l-z I' P 0 V --, ' r, J -< MIM I '. '""i ^r t { ^, ' f*,s /' 5, '^ T Mirt. \ H 1.^jpaft g '. :-- n >/ V'---.,,-. / w :::V i/]t ''"' \ ^ &&"->, x /' A / \ ''«, ',.-' \^ $ ' /i\ W s / i \ «- * J 1 _>n \ _ ~ 1 I A^? p, p i \/T\ r J 7»uV \ ^~ o W > V Pt -- i ^ p' **, ^ r" L :"^-^ * / K \ «P. i V \ V R ^.\ /? < ^--- \s v.'u 1 \ \ V **' N >v \ '*-'- \ % N. \ If-' \.->V \<y v V^ IP, p' \ - 1 V! \ \ ' \! \ ''' * 1 V?' i A; fef«-\ fx IZ \ \..\ \ 52F11NE A.49 BUCHAN BAY CEAGLE LA
18 52F1INEC256 63A.49 BUCHAN BAY (EAGLE LA 10
19 MAGDALEhA RLD LAKE. LlhiT LAKE PROSPECT DISTRICT OF KENOKA, ONT belf POTENTIAL <4 SCALE: HOR\-Z.OM-T/M_ i 100' VERTICAL. S P. )" = \OO M V. VERTICAL. TOP. l" = )OO' TOPOGRAPHIC PROFILES AUGUST-1948 SOUTH SHEET uj or o in o 0 ftl LEO ISLAND Al-OWG WEST SHORE. 25 FT. W OF UME-H ROCK ISLAND ALONG) SHORE. SOFT E«T OF UNE.-E REMARKS THE OBJECT OF THIS SURVEY \A^AS TO CHECK THE MAGNETIC AMOMALVE^ FOR SULPHIDE. MtMERAL\ZATlOiN- THESE WERE, TRAVERSED W\TH THE SELF POTENTIAL EQUIPMENT THE LOOPS WERE. NOT CLOSED. THE- WERE. CORRECTED FOR POT THE SECTIONS AHE ARRANGED VN ORV>ER WEST TO EAST AND THE MAGNETIC INTENSITIES ARE INDICATED e>y ARROWS ON TH& PROF\LES. 52F NE0S56 63A.49 BUCHAN BAY (EAGLE LA
20 LEGEND POST ALGOMAN D AL6OMAN PORPHYRY VEINS DIKES AMD SILLS^ FELDSPAR PORPHYRY ~p, QTZ.-FtuOSPAR. PORPWXRV -P, QTZ. PORPHYRY - P* " i KEEWATIN POR.PHVB.\ FLOWS SCHIST - "3CS FLOWS L- IRON FORMATION AND QAMDE > CHERT BASIC FLC»*S, AMPHieOUlTlC FUOWS -A SY MBOLS GEOLOGICAL CONTACT OE-F\NEO GEOLOGICAL COtHTACT OUTLINE OF SWATV\?S OR SWAMP OR AWD STRIKE OF T>lP AND STRIKE OF Pii-LOW LAVAS SULPHIDE VMNE.RAUXA-TIOM OR VOSSX&LE, FAULT TUFF MAGDALEMftRLD LAKE. LIMITED LAKt PROSPECT DISTRICT OF KENORA, OHT. GEOLOGY SCALE - I = 00 AUGUST O \OO -2 OO eoo 800 IOOO FT- A/--2/
21 z 8 uj y 5 MAGDALENA RED LAKE MINES. LIMITED ELAGUt- LAKE, PROSPECT DiSTRiCT OF KEWORA, ONT. SELF POTENTIAL A TOPOGRAPHIC PROFILES SCA\_E. - VE.RTICAU S P. _ l VE.R.T1CAU TOP. - \ \00 \OO M-V. \OO AUGUST-194 & NORTH SHEET
1.- L a m e j o r o p c ió n e s c l o na r e l d i s co ( s e e x p li c a r á d es p u é s ).
PROCEDIMIENTO DE RECUPERACION Y COPIAS DE SEGURIDAD DEL CORTAFUEGOS LINUX P ar a p od e r re c u p e ra r nu e s t r o c o rt a f u e go s an t e un d es a s t r e ( r ot u r a d e l di s c o o d e l a
C o a t i a n P u b l i c D e b tm a n a g e m e n t a n d C h a l l e n g e s o f M a k e t D e v e l o p m e n t Z a g e bo 8 t h A p i l 2 0 1 1 h t t pdd w w wp i j fp h D p u b l i c2 d e b td S t
B rn m e d s rlig e b e h o v... 3 k o n o m i... 6. S s k e n d e tils k u d o g k o n o m is k frip la d s... 7 F o r ld re b e ta lin g...
V e lf rd s s e k re ta ria te t S a g s n r. 1 4 3 4 1 5 B re v id. 9 9 3 9 7 4 R e f. S O T H D ir. tlf. 4 6 3 1 4 0 0 9 s o fie t@ ro s k ild e.d k G o d k e n d e ls e s k rite rie r fo r p riv a tin
EM EA. D is trib u te d D e n ia l O f S e rv ic e
EM EA S e c u rity D e p lo y m e n t F o ru m D e n ia l o f S e rv ic e U p d a te P e te r P ro v a rt C o n s u ltin g S E p p ro v a rt@ c is c o.c o m 1 A g e n d a T h re a t U p d a te IO S Es
SCO TT G LEA SO N D EM O Z G EB R E-
SCO TT G LEA SO N D EM O Z G EB R E- EG Z IA B H ER e d it o r s N ) LICA TIO N S A N D M ETH O D S t DVD N CLUDED C o n t e n Ls Pr e fa c e x v G l o b a l N a v i g a t i o n Sa t e llit e S y s t e
B a rn e y W a r f. U r b a n S tu d ie s, V o l. 3 2, N o. 2, 1 9 9 5 3 6 1 ±3 7 8
U r b a n S tu d ie s, V o l. 3 2, N o. 2, 1 9 9 5 3 6 1 ±3 7 8 T e le c o m m u n ic a t io n s a n d th e C h a n g in g G e o g r a p h ie s o f K n o w le d g e T r a n s m is s io n in th e L a te
w ith In fla m m a to r y B o w e l D ise a se. G a s tro in te s tin a l C lin ic, 2-8 -2, K a s h iw a z a, A g e o C ity, S a ita m a 3 6 2 -
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