ML20147J220

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Request for Subpoena for Graham to Testify Re Contentions That Applicant Has Failed to Conduct Thorough Investigations of Hosgri Fault Sys.Certificat of Svc Encl
ML20147J220
Person / Time
Site: Diablo Canyon  Pacific Gas & Electric icon.png
Issue date: 10/16/1978
From: Fleischaker D, Kristovich S, Phillips J
AFFILIATION NOT ASSIGNED, FLEISCHAKER, D.S.
To:
References
NUDOCS 7810270294
Download: ML20147J220 (11)
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{{#Wiki_filter:. [ h gLATED COICEM-s EC p BLIC D0cOMENT 110f '~. -{, s UNITED STATES OF AMERICA . ".. M NUCLEAR REGULATORY COMMISSION . ~,,_I Before The Atomic Safety & Licensing Board'. ( ^ ~? w s,. ( / V.~- ~~_..- In The Matter Of: ) ) PACIFIC GAS & ELECTRIC COMPANY ) Dockets Nos. 50-275 OL (Diablo Canyon Nuclear Power ) 50-323 OL Plant, Units 1 & 2) ) THIS DOCUMENT CONTAINS P00R QUAllTY PAGES INTERVENORS' REQUEST TO SUBPOENA DR. STEPHAN GRAHAM Pursuant to 10CRF S2.720, the Intervenors hereby apply for a subpoena requiring the attendance and testimony of Stephan Graham at the forthcoming evidentiary hearing. Dr. Dr. Graham's testimony will relate to the following conten-tions: 1. The Applicant has failed to conduct investi- / gations of the Hosgri fault system to determine adequately (i) the length of the fault; (ii) the relationship of the fault to regional tectonic structures; and (iii) the nature, amount, and geologic history of displacements along the fault, including particularly the estimated amount of the maximum Quaternary displacement related to any one earthquake along the fault. 2. A 7.5 Magnitude earthquake is not an ade-quate value for the safe shutdown earthquake. Dr. Graham has conducted extensive field studies to determine the amount and age of offset on the San Gregorio-Hosgri fault system. The abstract from the article written by Dr. Graham and his co-author, Dr. Dickinson, reporting the conclusions relating to the field studies, states.as follows- ? f /o 276 23/

'i ? 3. i Attorneys For SCENIC SHORELINE PRESERVATION CONFERENCE, INC. SAN LUIS OBSIPO MOTHERS FOR PEACE ECOLOGY ACTION CLUB SANDRA SILVER JOHN J. FORSTER l OCTOBER 16, 1978 k

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-n-u:;c:.CC.D - ~ tu D RESUME 4 f.A y .a ~ Q Stephan Alan Grcham 2136 Greenwood Dr. g San Carlos,'CA 94070 g 3p q g 'o l General Born 4/25/50, Evansville, Indiana l 1.'.arried 5/27/72, wife-P=ela,1 child U.S. citizan, military status-1H, foreign language-Gernan Education A.B. Indiana University 1972 Geology, with Honors M.S. Stanford University 1974 Geolegy Th.D. Stanford University 1976 Geology Specialization : Sedimentary geoloEy, in particular sedi=entary tectenics 'Ibesis : Middle Tertiary paleogeography and structurni development of the Salinian block, California; Bt.D. co==ittee : W. R. Dickinson (advisor), J. C. Ingle, Jr., 3. M. Page Professional' Experience 1. 1968, 1970: Subsurface mapping, Frit: Operating Co., Pt. Branch, Ind., (su==ers) 2. 1970: X-ray diffrcetometer technicien, Indiana Univ., Bloomington, Ind., (part-time ) 3 1971-1972 : Consulting geologist for Peninsula Explcration Co., corpus Christi, Texas, (part-time) 4. 1972: Associate Instructor, Indiana University Geolegic Field Station, Cardwell, Montana, (sumer) 5 1973: Research assistant, Stanford University, Ster. cord, Ca., (cu=er ) 6. 1973 : Instructor, Stanford Geological Survey, Bridgeport, Ca., (su er) 7 1976: Research Geologist, Dcxon Production Research Co., Houston, Tevas 8. 1976 - Ecploration Geolegist, Chevron USA Inc., San Francisco, CA Awards, Assistantships, and Fellowships 1. Earth Sciences Freshman deholarship, Indiana University,1963 2. Arthur R. 1.bt: Distinguished Scholarship, Indiana University, 1968-1972 l 3 Indiana University Geologic Field Station tuition award,1969 4. Standard Oil of Texas undergraduate geology award, 1969, 1970 5 Eest student paper, Rocky Ptn. Section, Geol. Soc. Acerica,1971 6. Senior faculty scholarship award, Indiana University,1972 7 Thi Beta Kappa,1972 8. National Science Foundation Graduate Fellowship, 1972-1975 8 e D-1

~ k g 1 s Professional Societies f Geological Society of /cerica .\\ Sig=a Xi Society of Econc=ic Paleontologists and Mineralogists i Publications Graham, S. A.,1971, Occurrence of middle Cembrian islands in ceuthwest Geol. Soc. /cerica Abs. With Progrecs, Rocky Mtn. Section, }tntana: 383-384. Graham, S. A., and Suttner, L.J.,1974, Occurrence of middle Cerbrian islands in southwest hbntana: The Fbuntain Geolegist, v. 11, 71-84. Graham, S. A.,1974, Ramanent magnetization of modern tidal flat sedicents from San Francisco Eay, California: Geology, v. 2, 223-226. Graham, S. A., Dickinson, W.R., and Ingersoll, R.V.,1975, Himalayan-Bengal model for flysch dispersal in the Arpalachian-Ouachita system: Geol. Soc. A= erica Bull., v. 86, # 3, 273-286. Dickinson, W.R., and Graham, S. A.,1975, Sedicentary environments, depcsitional systems and stratigraphic cycles in current concepts of depositional systems with applications for petroleum geology; W.R. Dickinson, editor: San Joaquin Geological Society Short Cour::e, Eckersfield,1-10. Graham, S. A.,1975, Tertiary sedimentary tectonics of the centrel Salinian block of California: Geol. Soc. /cerica Abstracts with Fregrams,

v. 7, no. 7, 1089 Graham, S. A.,1976, Tertiary sedimentary tectonics of the central Salinian Ib.D. Dissertation, Stanford University, Stanford, block of California:

California, 510 p. Grahem, S.A.,1976, Teltiary stratigraphy and depositionel envirc=ents near {- Indians Ranch, Monterey County, California: The Ucogene Sy:rposium, 125-136. Pac. Sect., Soc. Econ. Paleontologists and Mineralogists, Graham, S. A.,1976, Tertiary stratigraphy and depositional envire=ents near Iser. Assoc. of Iesreleum Indians Ranch, Ituterey County, California: Ceologists Ball. (abs. ), 2181-2182. Graham, S. A.,1976, San Gregorio Fault as a ca.jor right-slip fault of the San Andreas Fault system: Geol. Soc. Icerica Abstrac's with Progrers,

v. 8, no. 6, 8 p.

Graham, S. A., Ingersoll, R. V., and Dickinson, W.R.,1976, Common nrovenanco for lithic grains in Carboniferous from Cunchita Mountains and Slack Journal of Sedimentary Petrology, v. h6, 620-632 Warrior Basin: Dickinsen, W.R., Graham, S. A., and Ingersoll, R.V., and Jordan T.E.,1970, Application of plate tectonics to petroleum geology along the Pacific margin of Iiorth icerica: /ser. Asscc. Petroleum Geologists Sull. (abs ), 2179 Grahem, S. A., and Dickinson, W.R.,1977, Apparent offsets cf enlice' geologic Geol. Sec. America features across the San Gregorio-Hosgri fault trend : Abstracts with Programs, v. 9, no. 4, 424. Graham, S. A., and Dickinson, W.R.,1978, Apparent offsets of onland geolcgic Science, v. 199, features across the. San Gregorio-Hosgri fault trend : 179-181. ( D-2

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~ Graham, S. A., and Dickinson, W.R., -1978, Apparent offsets of onland geologic features across the San Gregorio-Hosgri fault trend : Calif. Div. Mines and Geology Special Report (in press ). Grahcm, S. A.,1978, Role of the Salinian block in the evolutien of the San Andreas fault system: Amer. Assoc. Petroleum Geoleci.sts gall.,

v. 62, # 11 (in press).

Telephone [ (415) 894-0308 (office' 8 :00 AM - 4 :co PM. ) (415) 595-2036 (home ) t k l l a D-3

mnrumvv mu s mom n-u w mg -p mu um cestral strand of the San Andscas fUult I-San Crqprio-Hogri Fauh Trend ATTACmtENT G F). Although lying west of the modan ] San Andicas fault. the Pilatcito, fault Abstract. The San Gregorio-fla.sgoifarilt trend i.s a contponent of the San Andreas thus is the local structurut boundary t.e. fault system on which there may have been ahumt II.% Litometers of post-carly tween Franciscan Comrle.\\ on the north. Aliocene rightdateral strike slip. Ifso, right slip on the han Amfocas and San Gre-cast and.ranitic basement on the south-t gorio-flasgrifatdts accounts far nuost of the nuovernent between the Pacifc and west. This pre-San Gregorio f.mit n.uy North Ameriewt plates smce midslincene time. Porthermore, the maenitude of be o%ct to the north as an inferred struc-right slip on a Paleogene proto-han Andocas );ndt inferred from the present dis-tural contact separuting the north-tribution of granitis basement is reduced considerably when Neugene Recent San ernmost granitic basernent outerops at Gregoria Haagri right slip is taken into account. Bodega Head from the Franciscan-floored (?) latest Cretaceous and early The San Gregorio-Hosgri fault trend less. chance alignment of several well. Tertiary Gualala basin west of the San parallels the central California coast defined major faults seems unlikely. Fur-Andreas fault (/0). from its interse: tion with the San An-thermore,if our evidence for right slip on

2) Point Reyes section-Ben Iomond dreas fault northwest of San Francisco to the fault trend is valid, throughgoing Slount rin scetion offset (G in Fig. I).

j south of Point Sal (Fig.1). In this report continuity of the fault zone is required. Distinctive Tertiary sections. including we present on land geo!ogic evidence for The eviilence for right slip consists of unconformity bound pa:Lages of Paleo-about !!5 km of right. lateral strike blip seven pairs of o6et geologic features cene middle Miccene. anJ upper Mio-on this complex fault zone. On land and (Figs. I and 2). None of these are indi-cene-Pliocene age as well as com-i I offshore segments of the fault trend are vidually unequivocal, but taken together parable granitic basement. occur at Point wc!! def!ned by geologic mapping and they present a compelling aipument. Reyes and Ben Lomond Mountain (ll-marine surveys (I 4). Connecting links Linear geologic and paleogeographic fea-U). remain controversial, however, where tures forming piercing points on lault

3) Pigeon Point Formation-Santu Ln-inferred through shallow water in coastal planes are the most sensitive indicators cia Crctuccous offset pair (K's in Fig.1).

zones where acoustic prohling data are of strike slip (S). Certain of the olfset Upper Cretaceous deep >ea fan deposits absent or ambiguous (5-7). Neverthe-pairs listed bclow are linear features. but of the Pigeon Point Fo mation (14. /3) unfortunately none are tightly con and nn associated Cretaceous basin mar. strained. Consequently, we show prob-gin (6) are probably otTset fiom similar able offset ranges. The common denomi-features in the Santa Lucia Range (6). In nator of 115 km (Fig. 2) is our estimate of addition, preliminary studies sug;est .so right slip on the San Giegorio-liosgri that Oligo-Miocene shallow. to deep ma-fault trend. rine facies overlying the Pigeon Point k. Kr.1 Details of the o%et geologic features Formation (16) may have offset equiva. GuALALA eASIN } are presented elsewhete (3. 6). but in lents in the Santa Lucia Range (JL

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suminary they include the following.

4) Ogset of ofshore gravity ridge

,o 's

1) 7hc Bodega.Cualala fanIt-Pilar-

' Fig.1). Silver (/7) proposed that a linear a soCCoA HEAD- - citos/aldt olfret pair (asterisks in Fig.1), gravity feature oJshore from Ano Nuevo PT. RE YEs sre in-e g gg g g e

s l

/ 6f M I poigy pgygg. picrey poigy. AEo NuEvo-EsCAoERo DEN LoWoNo I SANTA LuCJA a svH OFFSET 8 3 i[ OFFSET oFrSET (SILV E R) p,gggg py g g 'M J.! PtLAROIToS AAo uvEvo PT : raut T g CCN LoYoNo u) IIS KM COMMON OFFSET uTn. H no-l PetNT suA-C AM 8RI A O p c( oFF5ET E cuALALA-go$. O l yI id.

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.a PIL Ar4CITos ,/ offset 2 v I b * "* ~ s AllrH AN / \\

panfrAg, g

F A A**CisC AN f' D OFFSET / OFFSET y F , i }, 6 { "" DIG ggf (n ALL) C D I^CI \\ {, u. ulocLNE ~~ a smi._s.- s c3 't \\ l ? 00~ Q too too Soo ') 9 \\ 000EGA stu Ku nu AVlt,.A / h C "*n.G d it E AD BEACH P^C1 Mr 's LATERAL POSITIONS OF OFFSET MICrolNTS ~ i r P,T 3, ALONG SAN GRECORIO - HOSGRI FAU LT rig. t cero. st..n or enh.rie reanires whet ;n a ryn.t.acial sense aionc the s.in onroe-4 r csted llo gn t.mit trend. Sec test f or thwudin. Fig. 2 try.ho. 0;het range eb.ut bn wu utrwt paus shown in lig. I and shwnwd in the test. SCIENL*1;. YOt.. IW, I n J ANUARY 19M oint.au?N7si.ot tholMus 3u u rop,,yht c 19DI AAAS !?9

( CO3 ,,,,,,,,,,,,,i Pfl MIOCENE I ouGoCENE i EOCENE i PALEOL l'CRETAEOUS - toc ans p.g gri,9 eoe we ee s =a f ed i Fad!C er Ans(24,Am PLAT [s SA ***

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goo e-gateatta A aun*A. asf H s $no y sco ~ ~ ~;~ ' w k j N -o h 68ovt4#1=f oas Peet0 same Ancat as.,4'.U MM. O sac ofMtR FAutT3 teCNE w!mf (W a su l Y .n, 3 Ca s ti c.A7.:*s.G av a, W.r n* i r, """ rof C9s n AL eyesA ATsvt San (,a tig.+c 12 doo ess7sx' tut at i O sA's ANDw1 AS-sass GAECcac p [ ~ SAM A904(as faWT / / \\ A. ,en-se, - As eco s Am Catt.om o trovf utst tw113 I ccessect and Ac ttvi T SAN Gatccsao pacLT w a.sr 1 no-1),.o.-e., 6 a ce uu.-.4 i s stvs =r. r:5 a= =s e e r g A. M 54, awatas ea.ut=tw so n 32 ao to 63

'o s3 gj AGE (8.8YBPt w =.

m maC"" ' o.r.c o,e es sa.w. 7,8;tl,,*$3g'g fi;. 3 (left). Northern limit of Sa:inian block af:er restoration of Neogene right slip on the 5.tn Andreas fautt alone ( A) er on the San Andren taalt plus the San Gre;ono.Hosgn ? ' was.c a .I fault trend (TI).The remaining c:Tset of granihc hosement conceounted for by Neegene /, ~.fj right s!ip rnay be a tr:cawre o(right slip on a pseto-San Andren fault. Fg. e t righn. 3 N2

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***'8 (Curve A) Time-oTset curse 6') modified to show the errect of San Greguno-Ho.ri p / 'Y right slip. (Curve fi) Relative medan of the Pm5e and North Amencan pl.acs d)L See p@. text fx siiseussion. ,,,,,,,e*u,,, so,4. x t., T1 -

  • lice incorporated in the fault zone at an ration fails to consider the extension of Point is the offset expresMon of the con-s tact between Fr:nci>enn rocks and pra-intermediate distance.

Salinian basement by !!$ km of San Cre-nitic basement of the Salinian block in

7) San Simeon opleiollre-Point Sul gorio-llo3;ri right slip north of its inter-the Santa Lucia Rrnge.

ophiolite ofset pair (double underlining section with the San Andreas f; ult (22.;

3) raint Sur Franciscan-Cambria in Fig.1). Hall (22) reported the probable 1293). The restoratica of this addition s,

Fines stub of' et pair (underfinin; in Fig. offset of a Mesozoic ophiolite and an i15 km of Neegene to Recent ri;ht >!!p to s l I). The Franciscan subduction complex overlying' Tertiary sequence from Point position B (Fig. 31 reduces by ene-thi-d of the central California ceast is general-Sal to the San Simeon area along the or perhaps two thirds the apparent right-ly a potassium fcl6 par-free metasedi-Hos;ri segment of the fault trend. slip offset of the northem limit of the Sa ' rnentary sequence (IS.19). Exceptions Displacement of the Point Sal-San linian b!cek by the supposed proto-San to this genemlization tre structural Simeon ophiolite as>ociation along the Andreas fault. FurtM nore. in the un-blocks of potassium felhpar-bearing Hos;ri >c; ment occurred 5 ta 13 million likely event that the limit of Sierran base-l praywseke-sha:e at Point Sur and C:m-years ago (2"). Other of6et indicators . Tent actu:dly lies to the conh in the sub-bria (IS.19). These two blocks apparent-demonstrate post-early Miocene and surface (30), and if Bodega llend is near ly have been off>ct by San Gre;orio-probable pou-raiddle Miceene right slip. the northern limit of Safinian ; aniti: Hos;ri ri;ht slip. Holocene movement is documented basement. then a proto-San Anaeas

6) Point Sur Miocene sandstone-for onland and o:Ishore fault se;ments fault is precluded alon; the modem San Franciscan wnree terrane ofact pair.

(2 4). Andress ruthway in centrul California. Miocene sandstone occupies a small Grunitic basement of the Satinian in any esent, the proto-San Andree.s fault > lier within the Sur fault zone >e;- block wec of the San Andreas fault is fault app.trent!y was not a transferm rnent of the San Gregario-llo3pri fault offset by a minimum of 510 km. hased on fau t analogou> to the modem San An-trend near Point Sur t3. Jul l>espite the northernmost granitic exposeres at 110 dreas fault system. Instead, proto-San immediate piosimity of gr:milie base-Jega Head (l'ig. I:, ymnitic beement Andreas faulting may brve been the geo-ment evosed in Mioecne time (5), the extends offshore to l'oint Arena (2J). the logic resolution of oblique >uhdue: ion sandstone has an ewhnhely Franci ean masimum otrset h 600 km (Fig. 3). Res. along the central Califot nia co.nt in early prosenance (3). At le..st 60 km of right tomtim of weibdocumented post lio. Tertiary time (!I). Slip is required to provide an adequate cene San Andree right shp of 303 km Right slip of the San Andreas f u! is Franehe;m sonree terrane. The offset (24-25) brm;s the northern limit of Sali. conveniently dhplayed as a time.dh-carmot esceeJ 105 km. howeser. Iv-ni.m basement back !o position A in Fig. placement p:ot on curve A in l'ig.

  • t32).

c.mse the sanAtone 'aeks voleanie eteh

3. The ditfetence between positien A The dotted modineation cf carve A pdor ty rkal of Mkwene su htones near (Fig. 3) and the noethwest limit of Sier.

to 60 imibon years ago shoe the etfect Cambria 12th Tl.e Lack of oscilap of ran basement he I een takea as a rnea. of dhregarding San Grepn io-f lod riliet betwun the Point hur Miocene sure of pielh ene "ptoto-San An-right slip in proto-San An. hen fault m- >arwl tone an.1 other o:fset paus (l'ig. 21 dreai* Hght slip (22. 2NL ()ther rerional teipsetations. Curve it in Fig. 4 show-Jeo not def eat the othet aremnent, be-esidence plates this defoemation in Pa. the relathe mosement between the l'.i-cause the Mioecne sm6 tone i in a lault leneene tune L9. 2V). Ilowever the testo. eille and North Amenean pla:es U/).

.. day period on bn/nr milk. Never. J t 3 2.1. C. CL. Jh'"'**" 5"f*8 l'""'rwy thele >>. pops of all ages display reduced 9 ~ithin the imeertainty of the curves. si movement l'etv. n the plates h.n i3. 't!Y Ross, tr.s. cept. Sure. ng/. rac.on wcW and for development when en loc.dired along the.%n Andicas g Q c,, g,g;,.,,,, 3,,,, a m, uff, ut,,93 noised on brdm m, k. d 09m. C'"' C"* ' 5 In an ettempt to deteimine the cause It proper for the last 6 nullion years. tween that time and th.: early.\\lio. IlN;,7hl#'"'- of death. ; issue sections from the af. ra. J. C. Clark nJ E.J. tir sbh. C<di/. thr. Ari. irs ,ne. mmt of the plate motion was dis. cr,.I. 3rre. krts. m r'e~s. fccted pups were examined histofegt. ibuted between the San Andreas and

p. g. A. s.b e r. ti...s. >,.e. A m. Ah ur, er,,p.,,,o a.

cally. Thin sections of skin. lung. liver 253 047't GieYorio.-llosVri fault trends. Thus ts.w. a mes. Caa. soc. Am. suit. st. 3)t1 stomach, bone, and musc!c were pre. e ptesent estension of granitic base-097h. ent of the Salinian block in large part is 8

  • y;,, "' C"/' 0"'

'#* C"*I Serr Arc. lf pared from 8-day old pups nursed wi Indm 'nitk. The Sections were stained pLtined by richt shp on f.mita of the

20. P. ti. 'Trask. lo !I. O.c. Crol. Uair. Cal / 1).

with hematonlin and co3in and examined cogene S.in nJreas fault system, as

i, $7,$(1Yi. fr.. U.S. Crut. Surr..trise, riru under the light microscope. Only the
ggested by Johnson anJ Normark (JJ).

3rud.. sten 3rr..w t19: si simt skin appeared aWmd,d.hplaying fWal scirmein.: '[ f"T~'s.tver. J. R. Curray A. O Count. in acute dermatitis. general underdevelop. S. A. GRAHAh! Crol**pc G,mte rae rier, Noorthren Cu.nr I<.mrs. 'splorettion Department, tt'estern Pouer Heyrs Red.n. C.stirnema. J. kl. t.tros.nnd ment. and t. llicle atrophy. Fuithermme, o (cgime, Chctron U.S.A. Inc.. F.. M. stoores. FJ. (GeuWest Saoerr. 5xta. &MwWkmm5k@ ,,' en,.[Am. Aswe. rer Gr"t bali !*.% 3v :x['j;L' $ ;$ %.'[ g' "'ges.,,eg. thickened and the number of hair shafts an Frarrcisco. California 941I9 ~ W. R. DicxissoN >cpartment of Gevivyy. Stanford Q, l,' Q,*l$y,; 'aYl.' N.' L$.9n*l.L;ro,.r,,,matkcdly reduced. All other organs up. Swirosium. D. W Wm er. G. Ihmiay. o peared normal. though undersized. and luirersity. Smnford. Cohfornia WJU5 Tipt. n. E6. tSo.acty of Economs l' lconcol. no evidence of infection, allergy. or.in. eigsn and Shnetal@:3. Tula 19?h. p. J67. References and Notes 37, j,5,ppe, Ucut. Sec. Am Butt, gt, 3:3i g ty;ol. complete digestI3n of milk was Ob.

28. R. W. Kin!cr. 7.. E. Pecerman. D. C.

h.,,. D. %CTVCd-

t. A. K. Coorer, U.S. Crol. 5.,rv. Oren rite Rep.

Gourned. 5turtfurJ univ. hobl. Crol. 3co, s. }39 Histological observations were also Ivn ttu li.e.65. c 97);.

2. G. F.. % er cr. Gerit. Soc. Am. 4bari. Program 8
29. For e urnple. see A. Graham. A.encent Sym.

made of mammary glands ofindm d.tms pas,um. A, E. Fritsche. H. Ter Best. Jr.. W. W.

3. H. G. Gr:ene. W. H. Lee. D. S. StsCu: lech. E.

Wornards. Eds. iSociety or Econorme Paleon. who>e pups were close to death, !n gen.

9. 324 (1977).

E. er +t.. U.S. Crol. 3.ev..stisc. ricIJ : ud. toiopsa and stincratopsu. Tu>s. (C6. p. eral, the>c glands appeared less active 125. 4 ton.ttr-sid ti97)i.

30. See the JoncJ tine in Fig. 3.

and smaller than those of. normal B 6

4. H. C. v.'agwr, U.S. Crol. 3,erv. Open (Je Rep.

33, p. j, Coney. Crut. Joc. Am. spre. rup., in mice..'.{preover. %e obsewed that Im/m timt 3/ s. A. Gr.tum 6ssertadon. $tanforJ (lnh er%

32. Stodded from the curses of Di:Linson er at do dams frequently yield less mil,.

preu . A i1976L p. Sin. 6.

nJ W. R. Okkmion. Cut,/ Div..trars and Nisen nr.J UrA Cet in ae.:orance me a Mweene.Pticsene boundary rear } rnGon 3 e.r' T.iken tegether, the>e symptoms are Crot. St.re. Res., in press.

ap i or a detade. Jewu sion =ce Grarum di. slmtlar to thOse described by Mutch and

33. T. Arm.aer and P. Molnar. Sao r/wid f.,w. Publ.
7. E. A. S.her. Crut. Jac. 4m. Abstr fragram 9.

ceiv, 7 (3)in rat Iups nursed on dams re-StA) I 1977). C,gt.w. 13.I.% (l d i Hurle g 8. J. C. Crocli, Crol. Joc. 4m. J sc. Par. U

34. J. D. Jwhnson anJ W. Norrrack. Croty... Il f

c mg a po>tgestational zine free diet. (1962h p. 61.

9. For eumrie. srs T. H. Nil en. cd T. R. Lmoni.
33. Our research was surroced in part by the Earth g 974L Th s diet 10 ads to a 50 percent decrea>e i

Jr.. /. M U.S. Crol. $cron I. M9 :IV'3L

10. C. St. Wenr.enh. Souf..rd t/w. iWL Crot.

Scienee secte. Luon.1 Saen:e Found.non in the zinc content of the milk by day IS Sci H. 3 'W 8

  • tsransut.s m im b oflacthtson, nth only mm..tmal etfects on
11. A. J. Gnosay. Catif. O*.r..itines Cral Bult.

23 May 1977;rensed 22 August 1977 2 N (1977). the other constituents. As a result. nurs. ing pups are severely depleted of plasma zinc.Two-thirds of such animals die and all exhibit retarded growth and severe Z.in e D cfic.iencv in Mur.tne Milk Underl. s dermat.. itis. Moreover, total m.lk produc-te i tion Was reduced by 50 percent in the Expression of the Let/tal Milk (/m) Mutation zine-defici:nt dams. Because of the similarity of symptoms Abstract. The inability of morsing pups tu survive em milk of mice homo:ygmes for betwcen the dletary-induced zinc dcR-Jhe recenire mutation, lethat miik (Iml. is corrchited with a red uction in :ine lerch of both unill and pup carcass. Administration of:hte to pups nursing im Imtm. dams ciency and the lethal mill syndrome. we compared the concentrutions of :inc in reduces the observed snortality and murhidity. It is sus:ge.ned that lm alters :inc the milk of Imlm and normal mice. As transportfront tuoternalbhud to milk and that its. study mayprovide usefod htforma-shown in Table 1.the rina content of the tionfor uriderstanding the rare human discan, acendermatitis enteropathica. milk of mutant mice is redue:d.a per. t cent from that of normal IL 6 mice. "ihis A rcressive mutation. desir.nated Iv. pups petsist at all stages oflactation f2). We have confirmed that newborns fos-ditference is seen throughout lactation thrd md4 (!m), was discovered among mice of the CMllL'M tlM) strain (1). tered on hn/m d.uns at mid.lacutinn or and is relleeted in the whole body zine Pops nursed on hn/m d.uns eshibit stunt-late lactation aie as severely alreeted as concentrations of S-Jay old 3uckling ani-ed growth. acute dermathis, atorecia. those nm sed from the beginmns of lacta-mah llowever, we found no such defi-and death prior to w eaning. Since normal tion. ht addition, we have found a dif-ciency in either the plasma of lactatmg !!!6 pups (1.ml.ml die when nursed on ference in susceptibility to the elfeeb of imIm d.uns or in the carcasses of..tutt Im/m milk, the detect resides in the m 'k. Insbn nulk with respect to the are of hn!m females. Since adult imhn femab s " Mmem er, hnhn pops des elop noe ma!!y pops. Newborn pups me in es et uhly cshibit noim.d concentr.dions of total if fmter.nnised on a momal dam. (;e-conunisied to death aner 3 days on hn/m body zine, it appears th.it the mutation ins olves reduced transt.in t of eine n om netic analyse 4 indicate that hn h located n n:1.. esen when subequently tt ans- ! un chiom.wome 2 and ings 58.6 centi-tened to a noontal J.im. Older pops on plasma to milk.The It% J.em m;dnmin a the othen hand has ing nursed on nor mal & concennation in the emik that n ten moigans hom the agouti tal focus. The elivets of hn/m ind( on neuhota milk foi a few d.iys. licapsently survis e a timt s highes thaft that in the pi.nimi. unt. im7Nmn p un nio 3nu C..r9 n ei o lv7x A, W in

 ?.L'i _1, UNITED STATES OF AMERICA NUCLEAR REGULATORY COMMISSION , 'e Before The Atomic Safety & Licensing Board y , y y~..- %,,. ~ In The Matter Of: ) ) PACIFIC GAS & ELECTRIC COMPANY ) Dockets Nos. 50-275 OL (Diablo Canyon Nuclear Power ) 50-323 OL Plant, Units 1 & 2) ) CERTIFICATE OF SERVICE I hereby certify that I have this 16th Day of October, 1978, served copies of the foregoing INTERVENORS' REQUEST TO SUBPOENA DR. STEVEN GRAHAM in the above captioned case upon all of the parties listed below by depositing copies thereof in the U.S. Mails, first-class, postage prepaid. Elizabeth S. Bowers, Esq. Dr. William E. Martin Chairman Battelle Memorial Institute Atomic Safety & Licensing Columbus, Ohio 43201 Board Panel U.S. Nuclear Regulatory . Tames R. Tourtellotte, Esq. Commission L. Dow Davis, Esq. Mail Drop East West 450 Richard Goddard, Esq. Washington, D.C. 20555 Lawrence Brenner, Esq. Office of Executive Mr. Glenn Bright Legal Director Atomic Safety & Licensing BETH 042 Board Panel U.S. Nuclear Regulatory U.S. Nuclear Regulatory Commission Commission Washington, D.C. 20555 Mail Drop East West 450 Washington, D.C. 20555 Mrs. Elizabeth Apfelberg 1415 Cozadero Docket & Service Section San Luis Obispo, CA 93401 Office of the Secretary U.S. Nuclear Regulatory Mr. Frederick Eissler Commission Scenic Shoreline Preserva-Washington, D.C. 20555 tion Conference, Inc. 4623 More Mesa Drive Santa Barbara, CA 93105

'l 1 2. i Sandra A. & Gordon Silver Bruce Norton., Esq. 1792 Conejo Avenue 3216 N. Third Street San Luis Obispo, CA 93401 Suite 202 Phoenix, Arizona 85012 John Phillips, Esq. Center For Law In The Mr. Yale I. Jones, Esq. Public Interest 100 Van Ness Avenue 10203 Santa Monica boulevard 19th Floor Los Angeles, CA 90067 San Francisco, CA 94102 Paul C. Valentine, Esq. Mrs. Raye Fleming 321 Lytton Avenue 1920 Mattie Road Palo Alto, CA 94302 Shell Beach, CA 93449 Janice E. Kerr, Esq. MHB Technical Associates Lawrence Q. Garcia, Esq. 366 California Avenue J. Calvin Simpson, Esq. Suite 6 California Public Utilities Palo Alto, CA 94306 Commission 5246 State Building CE.rl Neiburger 350'McAllister Street Telegram Tribune San Francisco, CA 94102 P.O. Box 112 San Luis Obispo, CA 93402 John C. Morrissey, Esq. Philip A. Crane, Esq. James O. Schuyler, Nuclear Projects Engineer Pacific Gas & Electric Company 77 Beale Street, Room 3127 San Francisco, CA 94106 Arthur C. Gehr, Esq. Snell & Wilmer 3100 Valley Center Phoenix, Arizona 85073 (AM k Yb David S. Fleischaker, Esq. 1025 Fifteenth Street, N.W. Suite 602 Washington, D.C. 20005}}

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