:',',

June 13, 1990frank A. TrusdellP.O. Box 551Uolcano, Hi. 967B5<BOB> 965-9699

fAX: <808> 965-9274

Dr. Garcia:

Enclosed you will find SOMe glass saMples. SOMe of the

Material is pristine and others are sOMewhat less so. The Material

which is less so was included because this is all the glass that

exists for these units. If the analyses COMe out O.K. please let Me

know and I'll start cataloguing theM otherwise if they are poor no

sense waste energy.

Secondly Arnold has not been in the office so My success with

getting the tilt plots is predictable.

ASAP.

I'll try to get the plots

My talk went over well at HUO!

interested in the story.

TOM W. was present and seeMed

What is the status of the pond contract after the current one

ends?

Lastly in the pursuit of glasses to be Microprobed I need a

suite of vials equal to the size the saMples were sent in, SOMe

are sMaller, and others that are 2-3x as large. It seeMS that

that

MOSt

of the dikes have pristine glass and SOMe lava flow units.

Take it easy and eagerly awaiting the probe results!

List of Glass SaMples provided by frank Trusdell frOM SOH i

SaMPle D D.e.Jrlb "B.p~

1 2138 195

2 225 208

3 2167 199

2325 217

~5 2009 180

6 225 208

7 2325 217

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U.S. Geological SurveyHawaiian Volcano Observatory

P.O. Box 51Hawaii National Park, HI 96718

Hello Terry:

Enclosed find a suite of secondary and alteration Mineralogy froM

the SOH holes. SOMe of these are suitable for fluid inclusion

work and it is up to you to Make that deterMination. Most of the

saMples are tiny and I wonder if you will be able to use the XRD?

In SOMe cases you May have to use the Microprobe. In reality

there are no Massive deposits of secondary Minerals. In any

given box secondary Minerals constitute «1% of the Material.

We have tentatively identified SOMe of the Minerals but this

is through optical Methods (binocular Microscope, not thin-

section). Therefore our calls Maybe wrong. We hope that you can

identify these for us so the logging can be done accurately and

efficiently. Lastly, SOH-4 is the Most diverse as far as

secondary Mineralogy is concerned and I tried to included that

diversity in this suite of saMples.

Please call if you have any questions. Could you forward Me

SOMe references and/or literature on secondary and alteration

Mineralogy for Me to read? I aM a novice in this area and have

lots to learn.

Aloha,

jY'~k HOLE

I I

here.0fuzzy

pollen0fine-

Mordenite,0fine-gralned

probablerock

with corners,Source rock

zeolite,Source

identified and used for fluid inclusion work.COr1MENTS0Calcite? Anhydrite?, Vug filling phase found inassociation with white fuzzy zeolite(Mordenite). Source rock fine-grainedhyaloclastite. 'White fuzzyThoMpsonite.hyaloclastite.'Zeolite, unknown dOMegrain like. AnalciMe?grained hyaloclastite.'AnalciMe? Vug filling, COMMonAssociated with sMectite and whitezeolites. Source A'a.'Heulandite? Fracture fill Mineral, only one0seen here. LiMe green in color. Source A'a.'Quartz crystal for flUid inclusion work. Vug0fill, associated with pyrite. Found in vOldsbetween pillows and hyaloclastite.'Zeollte or Anhydrite? Fracture fill, elongateCneedles. Source volcaniclastics.'White fracture fill Mineral-aMorphous silica?0Source hyaloclastite.'White, clear, crystalline zeolite, tabular-0prisMatic. Not quartz. Source hyaloclastite.'Anhydrite. Window-pane texture, SMall flakes0in vugs 5-12 MM long. Associated with greenclay (SMectite). Source phh.'Chlorite/SMectite? Green clay associated with 0above saMple of anhydrite. Source phh.'Calcite. Found in contact region between a0dike and country rock in dike breccia.Associated with fine layer of quartz xtals.'Calcite. Found in fracture in dike along with 0pyrite and quartz.'Mordenite/ThoMpsonite?? White fuzzy zeolite0found lining the vesicles in a'a.

681 6467'

271 2788'

SaMples to beBOX DEPTH359 3117'

356 3093'

359 3119'

271 2788'

487 4671'

597 5691'

598 5694'

580 5533'

604 5758.5'

580 5533'

495 4763'

282 2890.5'

4

4

4

4

4

4

4

4

4-

4

( I

I"

t~ 359

EI~DLE BOX

I~ 359

-z.. I 4

fill associated with0Source hyaloclastite.'

Vug fill associated with0Source pillow and

cor1r1ErHS0SMall white prisMatic, tabular xtals wlthstrlations; fracture flil. Associated withsMectite, calcite, quartz. Sourcehyaloclastite. •AnalCiMe? Faceted dOMes. Associated wlth0ThoMpsonite/Mordeni t e. Vug f ill. SourceHyaloclast i te. •AnalciMe? Faceted dOMes. Vug fill in picritic0phh. •AnalciMe? Large facets, vug fill picritic0flow. Maybe saMe as above.'Pyrrhotite? Pyrite? Associated with Epidote0her in vial. Vug filling phase associated withepidote, quartz, calcite. Source hyaloclastitein between pillows.'Quartz crystals. Vug fill associated with0sMectite and pyrrhotite. Source hyaloclastite.·Epidote. Vug Fill associated with sMectite(?},0quartz, pyrrhotite. Sourcepillow/hyaloclastite. I

Anhydrite? Window pane and striations on xta10faces. Vug fill associated with quartz,emec t i t e , pyrite.'Pyrite(?) FractureSMectite and quartz.Quartz crystals.SMectite and pyrite.hyaloclastite. 'Chlorite. Hydrated/altered pillow rind.Green radiating habit, Mica-like xtals, 0unknown. Vug fill in pillow/hyaloclastite.'SMectite/chlorite. associated with quartz.0Found at dike and hyaloclastite contact.'Oxydized Pyrite? Fracture fill associated with0green clay. Source dike.'Quartz crystals. Vug fill associated with0green botrydal clay? Source dike.'Green clay described above.

3117'

DEPTH3117 '

2788'

2788'

5499'

6477'

6447'

6477'

6467'

5690.5'5594'

6550'

5520'

6548'

6616'

6620'

271

271

682

283

690

576

597578

682

682

283

681

690

4

4

4

4

z..3 4

'V'f 4

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?4- 1

:zJ'-,z-;~

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L=t­

tV(1

~I 2 283 6620'

~~ 4 516 4937.5

~~ 558 5125'

AnhydrIte(?}. Fracture f i Ll in dike rock,0assoc1ated wlth pyrlte.'AMorphous s11ica? and SMectite? 2 Minerals0sequentially deposited in a vug. Source a'a. I

Anhydr-r t e c ? }. Vug fill. Source found within0thick pillow rind.

... '"

s-c)17 -If,;:::..

?>y Dc-y 75 -

~) btty; {IS- -..

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q 12 ~/'1;J;Af . Q"O

" ,

PROJECT BIMONIHLY REPORfBRANCH OF IGNEOUS AND GEOTIIERMAL PROCESSES

Project Title:Project Number:Project Chief:

Kilauea's Hydrothermal System9980-51

Jim Kauahikaua From: 1 Jan 93 To:28 Feb 93

I.Project activities and progress1) Geothermics Special Issue on Kilauea: The introduction, geology, andgeophysics papers were cleaned up and submitted to Geothermics. Cathy Janikis writing up the geochemistry paper to go with this set. I am adding a fewsections to the last paper meant to be a synthesis.2) Rainfall/groundwater isotope study with Steve Ingebritsen and MarthaScholl, WRD: We retrieved rain samplers on the Ainapo trail by helicopter andrescued one from active lava flows on the Kalapana trail near the coast. Thesesamples will be processed and sent to Menlo Park. 3) Terry Keith worked forthree weeks with Frank Trusdell and the folks at the University of HawaiiSCientific Hole Core facility delineating the secondary mineralogy in all threedeep holes.4) A small amount of progress was made in the effort to obtain permission forin-situ sampling of the True/Mid-Pacific well in the middle east rift zone. I wasFAXed a draft waiver of liabilities which was promptly reFAXed to Ralph Mihanof the solicitor's office for review.

Il.Highltghts and noteworthy results»From Terry Keith's preliminary work:1) the hydrothermal minerals in the SOH holes exist above their usualtemperature of deposition, but within stability ranges.2) silica in SOH-4 and SOH-2 is mostly quartz. Silica is scarce in SOH-I, whichdoes not have temperatures greater than 2000C, nor any mineralogicalindication that temperatures have been higher.3) anhydrite is common in all holes, probably because of the seawater component in the fluids (most of the core is below sealevel).4) permeability appears to be generally pretty low in all cores, except for a fewthin open fractures and brecciated zones.5) the hydrothermal mineralogy of SOH-2 appears to be closer to temperatureequilibrium than SOH-4; alteration mineralogy of all three holes indicatesheating up and/or a very young system(s) which has not equilibrated.

Ill.Changes in emphasis. scope. or staffNone.

IV.PublicationsMoore, R.B., and Kauahikaua, J., 1993, Introduction to the

Special Issue, submitted to Geothermtcs.Moore, R.B., and Trusdell, F.A., 1993, The geology of Kilauea

Volcano, submitted to GeothermicsIngebrttsen, S.E., and Scholl, M.A., 1993(in press), The

hydrogeology of Kilauea Volcano. GeothermicsKauahikaua, J., 1993, Geophysical characteristics of Kilauea's

Hydrothermal Systems. submitted to Geothermics.

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(USGS TO COMPLE'l'E THE FOLLOWIllG)VENDOR: The above samples are assigned BPA Call No. 99kJPM80/ . Please

send sections and residue to the following address:

51~ /-(aulA J,,°lk t.tu"-U.S. GEOLOGICAL SURVEY

i"'. 1020 O'BRIEN DRIVEtF Co) Cf 80 577/~ MENLO PARK CA 94025-3591

. . .

ATTN: ~i{-h 8a~4r , MS- 9/0SEND INVOICES TO: u. S. GEOLOGICAL SUR Y

345 MIDDLEFIELD ROAD, MS-MENLO PARK CA 94025-3591 --

MANN PETROGRAPHICS

P.O.# QqwP/V]30J

INVOICE 200- c9Z3

Date 3),;;13m

Rout 1 Box 23 - A • Ojo Caliente, N.M. 87549 • Celestino Lucero (505) 583-2477

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~ 'WorUOJ:J-fign QudityROCK AND MINERAL THIN SECTION

Address

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u.s. GEOLOGICAL SURVEY1020 O'BRIEN DRIVEMENLO PARK CA 94025-3591

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u.s. GEOLOGICAL SUR EY345 MIODLEFIELD ROAD, MS-MENLO PARK CA 94025-3591 -----

MANN PETROGRAPHICSRout 1 Box 23· A • Ojo Caliente, N.M. 87549 • Celestino Lucero (505) 583·2477

Sin", ~ 1973

:4 worMOf:JIig1i QualityROCK AND MINERAL THIN SECTION INVOICE. ;2..00 -7 S'f

Date IO/Zz..-! '13

P.O. # 9CjwPM 3 D(PNET30 DAYS

Description PriceEach

~OD

Amount

2-9n

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A H A H G G S I T o I99~(j -57':?!'? R R 0 N N I N E C N

D C D U A A U / L0 T T T H D 1'.

T V T I I 0 SH E H C 0 0 F L EI R I 0 N N E 0N NV - - L M F

IN SECTION ORDER: G E C C D I E

AME: Jte; fJ; 8a. rt;(). yS L S.R L 0 S T LEA E E L P E D

J C S C G A 0 A SNO: TS TL R R R S P

(if any) I I A E T A'0 o s D A RN N S I

AMPLE mJMBER S ,S N REMARKS

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J901 -23456789012345

'lor adc Lt.Lona), num.Ders, see reverse

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(USGS TO COUPLETE THE FOLLOWING)VENDOR: The above samples are assigned BPA Call No. CJ9wPN305. Please

send sections and residue to the following address:

;' v- •. -,

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Table 2. Fluid-inclusion heating/freezing data for hydrothermal minerals from the SOH drill holes

Drill Sample Host Number of Melting-point Salinity Number of Range of Meanhole depth mineral melting-point temperatures (wt percent homogenization homogenization homogenizationnumber (m) temperature TmCC) NaCI equiv- temperature temperatures temperature

measurements alent) measurements ThCC) ThCC)

SOH-I1526.8 If' Anhydrite 1 -1.3 2.2 14 157 - 161 1601654.9 )0' Quartz 4 -2.0, -2.1 3.4,3.6 9 155 - 171 163

SOH-21672.7;"i; . Quartz 3 -0.3, -2.1 0.5,3.6 17 252 - 267 2581759.17'1'; " 2 -1.9, -2.0 3.2,3.4 13 270 - 282 2781791.7 ,/'. " 2 -2.2 3.7 14 285 - 289 2871928.8 ie" " 1 -1.3 2.2 13 312 - 326 3182019.8!" \ " 20 -0.5 to -9.8 0.9 to 13.7 36 279 - 321 297

SOH-41085.4 '::;! Calcite 14 0.0 0.0 16 160 -173 1681452.4",0 x' Anhydrite 0 --- --- 15 204 - 272 2541472.5 2 ! 'Z " 5 -0.1 0.2 20 201 - 236 2251605.4 J~;f Quartz 3 -0.3, -0.5 0.5,0.9 33 187 - 223 2111771.7JT} Anhydrite 1 -2.5 4.2 15 205 - 215 2101886.4 »: Calcite 15 -1.9 to -2.1 3.2 to 3.6 24 253 - 272 266

" "Quartz 9 -0.4 to -0.6 0.7 to 1.1 32 269 - 275 2711959.730 Q1

, " 14 -0.9, -3.1 to -3.3 1.6,5.1 to 5.4 17 282 - 296 2881969.90'(1</ " 7 -2.0 3.4 30 273 - 291 2841973.9 ~. 0 ,( " 4 -1.1 1.9 15 290 - 295 2931996.3-3° 0 " 12 -0.2, -1.0 0.4,1.7 40 284 - 293 288

u

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1234 fJ16 6421.5 IJliI bree gm $+++ sut1Ides fibrcus Dhases , 1:-=.1%31:14 ~4-33 lvuafillinQ p(- -),s(6-10,.?1!!!L 1~~ f177JI I.- :126 .. 577'· 6425.5 IDil core s- -IJn1IItered 121 atJar1

1264 err 6429 " . 1!1+++ TS auIf\d., Q% + ? 1121-4 eeo 6451.75 Ipill/pi! brec &++ TS unalt SJiIIOW • QZ 1

Ipif brec .-1 altered pb + gz·1.

11284 681 6462-25 s+++0

125 4 681 6466 IDIl brec s- sulfides, az. +? 1

IDillow -- i130130 40 664 6490 S+t+, TS -1314 684 6491 IplI brec &+I' '1~1

13 "' 684 6496-7.5 V\JgfllllnQ s++ IQZ + smec1iteIehIorite + ? 1313 "' 686": 6507 ?\lUg nlllnC ~- -) 8113191'" "I'll O"n anhVdrtf.81 albltlloWt~ 1 mort-_.' 113' .. 686 6510 'lUg Iinina s. gz+1 "

1364 687'~ 6516 am dike none 11171908.9,)( ch~ mlchl/sm m! dtl/5C1\ 1 ~....1364 681 6521 ,p1Ibrec:c s ...+ 1.- . '-1--. .~

11314 oea 6526 pit bl'eec s+++ .---1-.138 4 - --690 '6549 wg1illiog s+ .__ .._. ---1-. 1

691-iesoo--- '--139 4 pdloweore s-+++ "---±±. 1, -140 11.1

-.141.' .--1-. I

142 Key: _. ~ ._._+--+- 1.1~ ISamCIe: p"'powder,sC:hand !'UTlPlet:d~rystal.TS~in sedlon 1~

144 Amounts: oHrc:lOtS· - .. verY llWe etc. I '-.- ..-t---+-- 144

• Page3

-, e- - ,-,

PROJECf BIMONTHLY REPORTBRANCH OF VOLCANIC AND GEOTHERMAL PROCESSES

Project Title:Project Number.Project Chief:

Geothermal Reservoirs9980-07Manuel Nathenson

From: March 1 thru April 30, 1994

I. Project activities and progress:

Nathenson put the paper on convective heat discharge from the Wood River group ofsprings south of Crater Lake into Branch review, got the reviews back, and has to revise it forsubmission by May 6. Wrote two abstracts on Crater Lake and Hawaii geothermal issues forposters at the 1995 McKelvey Forum on Energy and the Environment. These were packagedwith several other abstracts from the Geothermal Research Program to fonn a nice group ofposters and talks featuring environmental contributions from the program.

Nathenson spent a week researching questions for DOE on data for the EnvironmentalImpact Statement Got the Water Resources District in Hawaii to retrieve recent (unpublished)scream chemistry for DOE use. All data earlier than June, 1992, are suspect because anemployee of the USGS was found to be fabricating data. Tracked obscure information on thechemistry of rain water catchment systems. Nancy Blair of the Menlo Park library wasparticularly helpful in finding a review article on the microbiology of rainwater catchmentsystems that listed a series of international conferences that are not in major libraries orstandard bibliographic data bases. Questions concerning radon in geothermal water in Hawaiirequired two letters to Paul Kruger to extract some of the data. Careful reading of hispublished work raised questions concerning some of the data manipulations.

Nathenson reviewed papers by Riehle and Kuuahikaua.

II. Highlights and noteworthy results:

Bob Mariner, in his review of the Janik, Nathenson, and Scholl paper on the chemistryof geothermal water in Hawaii. raised the issue of the appropriate silica geothermorneterequation. In the paper, we used the normal formulas; however, they actually only apply up to250°C. Temperatures for some of the deep-well samples are over 3000C. and some of thesamples are at and some above the salinity of sea water. A more complete formula is availablefor silica solubility as a function of temperature and specific volume of the fluid that can also beused to include the effect of high levels of dissolved solids. This formula is not set up for easygeothermorneter calculation, and I wrote a spread sheet to do the calculations by trial and error.Because of compensating errors, the results tum out to be only somewhat different (e.g. 318°Cversus 306°C for well KS-3 \l. ith 77AOO rng/kg total dissolved solids in the wellhead liquid).

One of the interesting results is the realization that fluid from well KS-8 actually startedas saturated steam at 350°C in the reservoir. The fluid ~s sampled at the wellhead is 12 %liquid water . The enthalpy of the total fluid corresponds to 350°C steam. However, the liquidproduced at the wellhead contains 203 mg/kg of silica and nearly negligible amounts chloride,sodium, and the other ionic species. On a total fluid basis, the silica is 24 rng/kg, and thisamount of silica can be carried in 342°C steam. At normal temperatures «300°C), steamcannot carry much silica. At high temperatures (dose to the critical point of water), steamstarts to have liquid-like characteristics and can carry significant silica. The excellent agreementbetween the enthalpy temperature and the silica temperature clearly indicates that this fluidstarted as saturated steam at 340-350°C in the reservoir.

Fo (c a ' -€...)qo.4~

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~-C(~ Cf- 3'1;9. ,51

C(O.53

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- ~"'3, ~.5rl \ "Z- (7- -e».~5

Depth(ft. )

o

GraphicLog

Rock Description

No recovery.

Point Count

10

20

30

40

50

60

70

80

90

100

p

p

p

p

p

~-

p

p

1------1 Basalt, sparsely phyric. Medium gray. 15 - 30%vesicles.

Red top. Basalt, sparsely phyric. Brown to dark gray.Vesicles, 20 - 30%.

1--__---1 Brown, dirty, glassy flow top. Basalt, sparsly phyric,med. gray. 20-30% vesicles, 2-10mm, horiz.

Sample 5-1

Red, glassy flow top. Basalt, moderately phyric, med.&,.-------....:;-,=-'--1 gray. 5-30% vesicles, 1-5mm, round.

Red flow top. Aphyric basalt, med. gray. 2 vesiclepopulations: <1mm, inclined 60-70 deg.; 3-10mm,

k..I-.--......,...,'r/""'"..I'-.-'1 equant

Glassy base.

Red flow top. Aphyric basalt, med. gray.

Red flow top, glassy base. Basalt, med.-dk. gray.>30% vesicles, 1-3mm, equant.

Glassy top. Basalt, moderatly phyric, med. gray.15-30% vesicles, <1-20mm, horiz.t--- -I

Glassy top

200 pts. 1% olivine(1mm), <1% plag(1mm).100 pts. as above.

100 pts. 3% plag, 1%olivine.

100 pts. 0% plag, 0%olivine, some plagmph.

200 pts. <1% olivine,«1% plag

300 pts. 1% olivine,«1% plag.200 pts. 3% olivine, 1%plag.

.... '

Depth Graphic Rock Description Point Count

(ft.) Log

200Basalt, aphyric, med. gray. Vesicles, 5-20%, 1-3mm,equant.

!1200 pts, «1 % oliv.,

210 p- 1«1% plag.I

Sample 22-1

220 * 1II

230 1

Reddish, rubbly contact. II

Basalt, aphyric, med. gray. Vesicularity highly variable :200 pts,«1 %oliv,

2401«1% plag.

Rubbly flow. Basalt, moderately phyric, med. - dk. gray. I

p Vesicles, 20-30%, 2-10mm, horiz. i1200 pts, 2% oliv.I(3-5mm), «1% plag.

Sample 25-1 !200 pts, 3-4% oliv.,

250 p Basalt, moderately phyric, med. - dk. gray. Vesicles, 1«1% plag, plag mph.highly variable, <5 to >30%, <1 to 25mm. i

p 1Glassy top. Basalt, aphyric, dk. gray. Vesicles, 10-20%,1100 pts, <1% oliv.,1-3mm, equant. 1<1% plag.

260I

Basalt, aphyric, med. gray. Vesicles, highly variable, i

p 10-30%, 1-10mm, bubble bands. !200 pts, «1 % oliv.,1«1% plag.I1

270 iP Basalt, aphyric, med. - dk. gray. Vesicles, 10-20%, 1

1-10mm, equant, inclined 45 deg. 1200 pts <1% oliv <1%I ' ,ip1ag.

I280 I

II

PGlassy, rubbly flow top.

II

290 IIIII

r ~.... I-- ........ • J I300 I

,''''.Depth

(ft.)

300p

310

p

GraphicLog

*

Rock Description Point Count

320

330

340

350

360

370

380

390

400

p

p

p

p

p

p

p

p

Red, glassy, rubbly surface.Ash.Aphyric basalt.

Basalt, moderatly phyric, med. - dk. gray. Vesicles,20-30%, 1-6mm, equant.

r ......""- .." . ~. :;:.<:"" -;

Basalt, moderately phyric, med-dk gray. Vesicles,15-30%, 1-6mm, equant

~--;-;:;o:---I .AshBasalt, aphyric. Vesicles, 15-25%Basalt, moderately phyric, dk gray to reddish.

:Missing contact..Basalt, aphyric. Vesicles, 15-20%. Autoliths.

Basaly, moderately phyric, gray. Vesicles, 10-30%,1-5mm, horiz.

Basalt, sparsely phyric, med gray. Vesicles, 20-30%,2-4mm, horiz.

iI1100 pts, 2% oliv, «1%Iplag to 2% plag at

Ibase.

III

I,100 pts, 2%plag, <1%I •[oliv,

IIi

CiC10TOiL S:SOH-4 3641.5-1T 004 A:SOH-4 3641.5-1T 003 A:SOH-4 J754.5-1T 003 A:SOH-4 3754.5-2T 004 A:SOH-4 3980-1T 012 S:SOH-4 3754 5-18T 004 A:SOH-4 4033.3-1T 004 A:SOH-4 4037-1T 003 A:SOH-4 4204.5-1T 004 A:SOH-4 4209.5-1T 004 A:SOH-l 5009.3-1T 004 A:SOh-4 4274.3-1T 003 A:SOH-4 4360.5-1T 003 A:SOH-4 4375-1T 012 S:SOH-4 4706-1T 004 A:SOH-4 4706-1T 004 A:SOH-4 4740.5-1T 013 S:4931.5T 003 A:SOH-4 4830-1T 003 A:SOH-4 4935.5-1T 003 A:SOH-4 4981.5-1T 004 A:SOH-4 5013-1T 004 A:SOH-4 5015-1T 004 A:SOH-4 5046-1T 004 A:SOH-4 5065.5-1T 004 A:SOH-4 5053.1-1T 004 A:SOH-4 5053.1-2T 004 A:SOH-4 5075.8-1T 004 A:SOH-4 5076.4-1T 004 A:SOH-4 5084.5-1T 004 H:SOH-4 5131-1T 003 A:SOH-4 5131-2T 004 A:SOH-4 5131.5-1T 004 A:SOH-4 5143.5-1T 003 A:SOH-4 5143.5-2T 004 A:SOH-4 5154-1T 003 A:SOH-4 5154-3T 004 A:SOH-4 5179.5-1T 004 A:SOH-4 5249.9-1T 004 A:SOH-4 5312-1T 0 i 2 =::;: SOH-4T 012 S:SOH-4 5378.1-1T 003 A:SOH-4 5351.2-1T 012 S:SOH-4 5386.5-1T Oi2 S:SOH-4 5387.5-1T 012 S:SOH-4 5422.2-1T 012 S:SOH-4 5498.5-1T 012 S.SOH-4 5511~6-1

T 012 S:SOH-4 5521-1T 012 S:SOH-4 5566.9-1T 017 S:SOH-4 5592-1T 012 S:SOH-4 5613.2-)T 012 S:SOH-4 5649-1T 012 S:SOH-4 5676.8-1

T 007 UNKNOWNS.DIRECTORYT 012 S:SOH-4 3754 5-1T 013 S:SOH-4 3754 5-2T 012 S:SOH-4 3980-1T 012 S:SOH-4 4033.3-1T 003 A:SOH-4 3754.5-18T 012 S:SOH-4 4037-1T 014 S:SOH-4 4204.5-1T 012 S:SOH-4 4209.5-1T 012 S:SOH-l 5009.3-1T 012 S:SOH-4 4274.3-1T 026 S:SOH-4 4360.5-1T 015 S:SOH-4 4375-1T 012 S:SOH-4 4375-2T 003 A:SOH-4 4375-2T 012 S:SOH-4 4740.5-1T 012 S:SOH-4 4830-1T 012 S:SOH-4 4935.5-1T 003 A:SOH-4 4931.5-1T 012 S:SOH-4 4981.5-1T 012 S:SOH-4 5013-1T 012 S:SOH-4 5015-1T 013 S:SOH-4 5046-1T 012 S:SOH-4 5065.5-1TOll S:SOH-4 5053.1-1T 012 S:SOH-4 5053.1-2T 012 S:SOH-4 5075.8-1T 013 S:SOH-4 5076.4-1T 012 S:SOH-4 5084.5-1T 012 S:SOH-4 5131-1T 013 S:SOH-4 5131-2T 012 S:SOH-4 5131.5-1T 015 S:SOH-4 5143.5-1T 013 S:SOH-4 5143.5-2TOll S:SOH-4 5154-1T 012 S:SOH-4 5154-3T 012 S:SOH-4 5179.5-1TOll S:SOH-4 5249.9-1T 012 S:SOH-4 5312-1T 012 ~:~uH-4 5347 5-1T 002 S:SOH-4 5372-1T 003 A:SOH-4 5347.5-1T 003 A:SOH-4 5378.1-1T 003 A:SOH-4 5386.5-1T 004 A:SOH-4 5387.5-1T 004 A:SOH-4 5422.2-1T 004 A:SOH-4 5498 5-1T 004 A:SOH-4 5511.6-1T 003 A:SOH-4 5521-1T 004 A:SOH-4 5566.9-1T 003 A:SOH-4 5592-1T 004 A:SOH-4 5613.2-1T 004 A:SOH-4 5649-1T 003 A:SOH-4 5676.8-1

· ..

TOll S:SOH-4 5690 1T 012 S:SOH-4 5691-1T 012 S.SOH-4 5693-1T 012 S.SOH-4 5701.5-1T 013 S:OH-4 5701.5-2T 012 S:SOH-4 5714-1T 012 ~:~uH-4 5757-1T 012 S:SOH-4 5762-1T 012 S:SOH-4 5768-1T 016 S:SOH04 5782.9-1T 009 S:SOH-4 5757-1GT 009 S:SOH-4 5762-18T 009 S:SOH-4 5768-18TOll S:SOH-4 5782.9-2T 012 S:SOH-4 5800.6-1T 012 S:SOH-4 5814.3-1T 012 S:SOH-4 5822 5-1T 004 A:SOH-4 5822.5-1T 013 S:SOH-4 5912-1T 012 S:SOH-4 5954.5-1T 013 S:SOH-4 5979.7-1T 012 S:SOH-4 5993.5-1T 012 S:SOH-4 6026 1-1T 012 S:SOH-4 6102-1T 012 S SOH-4 6183.3-1T 003 A:SOH-4 6168.3-1T 013 S.SOH-4 6242-1T 013 S:SOH-4 6285-1T 013 S:SOH-4 6290 9-1TOll S:SOH-4 6312.1-1T 013 S:SOH-4 6331 8-1T 012 S:SOH-4 6351-1T 013 S:SOH-4 6359.9-1T 003 A:SOH-4 6359.9-1T 012 S:SOH-4 6393.9-1T 013 S:SOH-4 6412.5-1T 012 S:SOH-4 6422.5-1T 012 S:SOH-4 6429.5-1T 015 S:SOH-4 6462.9-1T 012 S:SOH-4 6462.9-2T 012 S:SOH-4 6467 5-1i 012 S:SOH-4 6519.7-1T 012 S:SOH-4 6532.5-1

T 004 A:SOH-4 5690-1T 004 A:SOH-4 5691-1T 004 A:SOH-4 5693-1T 003 A:SOH-4 5701 5-1T 003 A:SOH-4 5701.5-2T 004 A:SOH-4 5714-1T 003 A:SOH-4 5757-1T 003 A:SOH-4 5762-1T 004 A:SOH-4 5768-1T 003 A:SOH-4 5782.9-1T 003 A:SOH-4 5757-18T 003 A:SOH-4 5762-1GT 003 A:SOH-4 5768-1GT 004 A:SOH-4 5782.9-2; 003 A:SOH-4 5800 6-1T 004 A:SOH-4 5814.3-1T 012 S:SOH-4 5877.5-1T 004 A:SOH-4 5877.5-1T 003 A:SOH-4 5912-1T 003 A:SOH-4 5954.5-1T 003 A:SOH-4 5979 7-1T 004 A:SOH-4 5993.5-1T 003 A:SOH-4 6026.1-1T 004 A:SOH-4 6102-1T 012 S:SOH-4 6189-1T 004 A:SOH-4 6189-1T 003 A:SOH-4 6242-1T 003 A:SOH-4 6285-1T 003 A:SOH-4 6290 9-1T 004 A:SOH-4 6315.1-1T 003 A:SOH-4 6331.8-1T 004 A:SOH-4 6351-1T 013 S:SOH-4 6368-1T 003 A:SOH-4 6368-1T 004 A:SOH-4 6393.9-1T 003 A:SOH-4 6412.5-1T 004 A:SOH-4 6422.5-1T 004 A:SOH-4 6429.5-1T 004 A:SOH-4 6462.9-1T 004 A:SOH-4 6462.9-2T 004 A:SOH-4 6467.5-1T 004 A:SOH-4 6519.7-1T 002 A:SOH-4 6532.5-1

~4B13 S:SOH-4 6562-1T 003 A:50H-4 6562-1T 003 A:50H-4 3074.1-1GT 003 A:50H-4 3406-1GT 003 A:SOH-4 3980-1GT 003 A:SOH-4 4209.5-1GT 003 A:SOH-4 5015-1GT 003 A:50H-4 5075.8-1GT 003 A:50H-4 5084.5-1GT 003 A:50H-4 5143.5-2GT 003 A:50H-4 5347.5-1GT 003 A:50H-4 5422.2-1GT 003 A:50H-4 5649-1GT 003 A:50H-4 5782.9-1GT 003 A:50H-4 5800.6-1GT 003 A:50H-4 5979.7-1GT 003 A:50H-4 6026.1-1GT 003 A:50H-4 6189-1GT 003 A:50H-4 6290.9-1GT 003 A:50H-4 6359.9-1GT 003 A:SOH-4 6462.9-2GT 003 A:50H-4 6519.7-1GT 003 A:50H-4 6532.5-1GT 003 A:50H-4 6562-1GT 003 A:SOH-l 2557-1GT 003 A:SOH-1 4555.8-1GT 003 A:SOH-1 4753.1-1GT 003 A:SOH-1 5486-1GT 003 A:SOH-2 2828-1T 004 A:SOH-2 4108.8-1T 004 A:SOH-2 4108.8-2T 004 A:80H-2 4130.5-1T 004 A:50H-2 4152.1-1T 004 A:80H-2 4152.9-1T 004 A:80H-2 4180.8-1T 004 A:80H-2 4247.5-1T 003 A:SOH-2 4268-1T 004 A:50H-2 4287-1T 004 A:50H-2 6355.8-1T 004 A:SOH-2 4358-1T 004 A:80H-2 4417-1T 004 A:SOH-2 4472.1-1T 004 A:SOH-2 4504.5-1T 004 A:SOH-2 4508.5-1T 004 A:50H-2 6355.8-1GT 003 A:SOH-2 2828-1GT 003 A:SOH-2 4152.9-1GT 003 A:80H-2 4358-1GT 012 5:50H-2 4520.3-1T 012 S:50H-2 4600-1T 013 5:S0H-2 4603-1T 012 5:50H-2 4662-1~ 012 5:50H-2 4662-2T 012 5:50H-2 4714.9-1

T 008 UNKNOWNS.DIRECTORYT 006 5:50H-4 3074.1-1GT 006 S:SOH-4 3406-1GT 006 5:50H-4 3980-1GT 006 5:50H-4 4209.5-1GT 006 5:50H-4 5015-1GT 006 5:50H-4 5075.8-1GT 006 5:50H-4 5084.5-1GT 007 5:50H-4 5143.5-2GT 008 5:50H-4 5347.5-1GT 006 5:50H-4 5422.2-1T 007 5:50H-4 5649-1GT 007 8:50H-4 5782.9-1GT 006 5:850H-4 5800.6-1GT 007 5:50H-4 5979.7-1GT 009 5:80H-4 6026.1-1GT 007 5:50H-4 6189-1GT 007 8:50H-4 6290.9-1GT 007 5:50H-4 6359.9-1GT 012 8:50H-4 6462.9-2GT 006 5:50H-4 6519.7-1GT 007 8:50H-4 6532.5-1GT 007 8:80H-4 6521-1GT 006 8:80H-1 2557-1GT 007 8:50H-1 4555.8-1GT 006 5:80H-1 4753.1-1GT 007 5:80H-1 5486-1GT 013 8:50H02 2828-1T 012 8:50H-2 4108.8-1T 012 8:50H-2 4108.8-2T 012 8:50H-2 4130.5-1T 012 5:50H-2 4152.1-1T 012 5:50H-2 4152.9-1T 012 5:50H-2 4180.8-1T 012 5:50H-2 4247.5-1T 012 5:50H-2 4268-1T 012 5:50H-2 4287-1T 015 S:SOH-2 6355.8-1T 016 5:50H-2 4358-1T 016 5:50H-2 4417-1T 015 5:50H-2 4472.1-1T 016 5:50H-2 4504.5-1T 015 5:50H-2 4508.5-1T 013 5:50H-2 6355.8-1GT 007 5:50H-2 2828-1GT 006 5:50H-2 4152.9-1GT 006 5:50H-2 4358-1GT 007 5:50H-2 6355.8T 004 A:50H-2 4520.3-1T 003 A:50H-2 4600-1T 003 A:50H-2 4603-1T 004 A:50H-2 4662-1T 004 A:50H-2 4662-2T 004 A:50H-2 4714.9-1

.... l.r/i4/q.,'CC • j

.,. ..... -

, 012 5:50H-2 4722-1; 012 8:60H-2 4787.5-1T 012 6:60H-2 4934.1-1T 013 S:60H-2 4934.1-2T 004 A:60H-2 4934.1-2TOll S:50H-2 5018.9-1T 017 S:60H-2 6794-1T 004 A:50H-2 5045.3-1T 014 5:60H-2 6782-1T 012 6:80H-2 6781.5-1T 013 8:80H-2 6763-1T 013 8:60H-2 6763-2T 013 6:50H-2 6754.4-1T 007 6:80H-2 4520.3-1GT 006 6:60H-2 4714.9-1GT 007 5:50H-2 4934.1-1GT 007 6:50H-2 4934.1-2GT 007 6:50H-2 6763-1GT 007 5:50H-2 6763-2GT 012 5:50H-2 5090-1T 013 5:50H-2 5121.6-1T 012 8:50H-2 5353.8-1T 012 5:50H-2 5487.9-1T 013 5:50H-2 5508.9-1T 012 5:50H-2 5693.9-1T 012 5:50H-2 5771.2-1

I 012 5:50H-2 5779-1T 012 5:S0H-2 5846.7-1T 007 S:50H-2 6754.4-1GT 007 5:50H-2 6763 1GT 006 5:50H-2 6781.5-1GT 006 5:50H-2 6782-1GT 012 5:50H-2 5973-1T 013 5:50H-2 6132.7-1T 007 5:50H-2 6794 IGT 006 5:50H-2 5090-1GT 007 5:50H-2 5693.9 IGT 006 5:50H-2 5846.7-1GT 013 5:50H-2 6139-1T 008 S:SOH-2 5973-1GT 004 A:SOH-2 6139-1TOll 5:S0H-2 6328-1T 012 5:50H-2 6328-2T 012 5:50H-2 6328-3T 013 5:50H-2 6339.1-1T 013 5:50H 2 6355.8-1T 003 A:50H-2 6132.7-1GT 003 A:SOH-2 6139-1GT 003 A:SOH-2 6328-3GT 003 A:SOH-2 6339.1-1GT 016 5:S0H-2 6447.2-1~ 003 A:SOH-2 6447.2-1, 003 A: SOH-2 6539.5-1

T 003 A:SOH-2 6557.5-1T 004 A:SOH-2 6562.3-1

T 004 A:50H-2 4722-1T 004 A:SOH-2 4787.5-1T 004 A:50H-2 4934.1-1T 012 S:SOH02 4955.3-1T 003 A:50H-2 4955.3-1T 027 5:50H-2 5045.3-1T 004 A:50H-2 5018.9-1T 004 A:50H-2 6794-1T 004 A:50H-2 6782-1T 004 A:50H-2 6781.5-1T 004 A:50H-2 6763-1T 003 A:SOH-2 6763-2T 003 A:50H-2 6754.4-1T 003 A:SOH-2 4520.3-1GT 003 A:50H-2 4714.9-1GT 003 A:50H-2 4934.1-1GT 003 A:SOH-2 4934.1-2GT 007 5:S0H-2 6794-1GT 003 A:50H-2 6763-2GT 003 A:SOH-2 5090-1T 004 A:50H-2 5121.6-1T 003 A:SOH-2 5353.8-1T 004 A:50H-2 5487.9-1T 003 A:50H-2 5508.9-1T 003 A:50H-2 5693.9-1T 003 A:50H-2 5771.2-1T 003 A:50H-2 5779-1T 004 A:SOH-2 5846.7-1T 003 A:50H-2 6754.4-1GT 003 A:50H-2 6763 2GT 003 A:50H-2 6781.5-1GT 003 A:50H-2 6782-1GT 004 A:50H-2 5973-1T 003 A:SOH-2 6132.7-1T 003 A:50H-2 6794 IGT 003 A:SOH-2 5090-1GT 003 A:50H-2 5693.9 IGT 003 A:50H-2 5846.7-1GT 015 S:SOH-2 6303.5-1T 003 A:50H-2 5973-1GT 003 A:SOH-2 6303.5-1T 003 A:50H-2 6328-1T 004 A:50H-2 6328-2T 004 A:50H-2 6328-3T 003 A:50H-2 6339.1-1T 007 5:50H-2 6132.7-1GT 007 5:50H-2 6139-1GT 007 5:S0H-2 6328-3GT 007 S:SOH-2 6339.1-1GT 013 5:50H-2 6437.2-1T 004 A:50H-2 6437.2-1T 012 5:50H-2 6539.5-1T 013 5:50H-2 6557.5-1T 012 S:SOH-2 6562.3-1

000T 026 S:ML28-32 3877-1T 004 A:ML28-32 3877-1T 004 A:ML28-32 3880-1T 004 A:ML28-32 3890-1T 004 A:ML28-32 3910-1T 004 A:ML28-32 3920-1T 004 A:ML28-32 3930-1T 004 A:ML28-32 3955-1T 004 A:ML28-32 4030-1T 004 A:ML28-32 4044-1T 012 S:ML28-32 4044-2TOll S:DT5-3TOll S:DT5-2TOll S:DT5-1T 012 S:8S-4TOll S:ML28-32 4060-1T 012 S:ML28-32 4071-1T 006 S:8S-4GT 006 S:Ml28-32 4044-28T 004 A:92DT-8T 004 A:DT-8T 004 A:ML28-32 4150-1T 004 A:ML28-32 4180-1T 004 A:ML28-32 4190-1

~,T 004 A:1'1L28-32 4200-1T 004 A:ML28-32 4246-1T 004 A:ML28-32 4249.5-1T 004 A:ML28-32 4249.5-2T 004 A:ML28-32 4258-1T 004 A:ML28-32 4270-3T 004 A:ML28-32 4270-4TOll S:ML28-32 4279-2T 004 A:ML28-32 4279-2T 004 A:ML28-32 4300-4T 003 A:ML28-32 4320-3T 004 A:ML28-32 4334-1T 017 S: D HOt,IELLTOll S:MLV 28-32 4400-1T 012 S:ML28-32 4842-1T Oi3 8:C:2-1TOll S:Ml28-32 4342-2T 012 S:ML28-3? 4350-3T 012 S:ML28-32 4592-1T 007 S:CZ-1GT 012 S:ML28-32 4423-1T 012 S:ML28-32 4430-1TOll S:ML28-32 4435-1T 012 S:ML28-32 4440-1TOll S:ML28-32 4450-2

M~l 011 S:ML28-32 4490-2~T 004 A:ML28-32 4490-2

T 003 A:f'lL28-32 44'i'O-2AT 004 A:ML28-32 4467-1

GIl S:ML28-32 4480-2

T 007 UNKNu~S.DIRECTORY

T 012 S:Ml28-32 3880-1T 012 S:ML28-32 3890-1T 012 S:Ml28-32 3910-1T 012 S:ML28-32 3920-1T 012 S:ML28-32 3930-1T 012 S:ML28-32 3955-1T 012 S:ML28-32 4030-1T 010 S:Ml28-32 4044-1TOll S:ML28-32 4044 1T 004 A:ML28-32 4044-2T 004 A:DT5-T 004 A:DT5-2T 004 A:DT5-1T 004 A:GS-4T 004 A:ML28-32 4060-1T 004 A:ML28-32 4071-1T 003 A:GS-4GT 011 S:92DT-8TOll S:DT-8T 012 S:ML28-32 4150-1TOll S:ML28-32 4180-1T 011 S:ML28-32 4190-1Tall S:ML28-32 4200-1T 012 S:ML28-32 4246-1TOll S:ML28-32 4249.5-1TOll S:ML28-32 4249.5-2T 012 S:ML28-32 4258-1T 012 S:ML28-32 4270-3T 012 S:ML28-32 4270-4T 012 S:ML28-32 4279-1T 004 A:ML28-32 4279-1TOll S:ML28-32 4300-4T 012 S:ML28-32 4320-3TOll S:ML28-32 4334-1T 002 5:D. H~~ELL

T 004 A:D HO~ELL

T 004 A:MLV 28-32 4400-1T 004 A:ML28-32 4342-1T 00:3 A: C2-1T 004 A:ML28-32 4342-2T 004 A:ML28-32 4350-3T 004 A:ML28-32 4592-1T 003 A:CZ-IGT 003 A:ML28-32 4423-1T 004 A:ML28-32 4430-1T 004 A:ML28-32 4435-1T 004 A:ML28-32 4440-1T 003 A:ML28-32 4450-2TOll S:ML28-32 4467-1T 008 S:ML28-32 4490-2ATOll S:ML28-32 4470-2T 004 A:ML28-32 4470-2T 004 A:ML28-32 4480-2

-:lfzz

· .TOll S:ML28-32 4489-1TOll S:ML28-32 4489-2T 012 S:SOH-l 5108.2-2TOll S:SOH-2 5902.5-1T 012 S:SOH-2 5902.5-2

012 S:SOH-2 6032.5-1TOll S:SOH-2 6046.1-2T 012 S:SOH-2 6229.5-1T 003 A:SOH-2 6229.5-1T 002 S:TEST2T 027 S:TEST4T 013 S:RUNHELLOT 013 S:SOH-2 6752.3-1TOll S:SOH-l 3066-2T 013 S:SOH-l 3113.1-1T 013 S:SOH-l 3652.1-1T 013 S:SOH-l 4720.8-3T 004 A:SOH-l 4720.8-3T 003 A:SOH-l 5289.5-1T 004 A:SOH-4 2442.5-1T 004 A:SOH-4 2849.5-1T 004 A:SOH-4 2873.5-1T 004 A:SOH-2 4469.4-1T 004 A:SOH-2 4469.4-2T 004 A:SOH-2 4663-1T 004 A:SOH-2 6543.5-1T 004 A:SOH-2 5235.6-2T 004 A:SOH-2 5235.6-3T 004 A:SOH-2 5236.8-1

004 A:SOH-2 5283-1.~ 004 A:SOH-2 5485-1

T 004 A:SOH-2 5544.6-1T 004 A:SOH-2 5627-1T 004 A:SOH-2 5818.3-1T 003 A:SOH-2 5917-1T 003 A:SOH-2 5969.9-1T 004 A:SOH2 5969.9-1T 004 A:SOH-2 5997-1T 004 A:SOH-2 6000.1-1T 003 A:SOH-2 6660-4T 003 A:SOH-2 6260.8-11- 004 A:SOH-2 6332.5-1T 004 A:SOH-2 6402.4-1T 003 A:SOH-2 6535-1

T 004 A:ML28-32 4489-1T 004 A:ML28~32 4489-2T 003 A:SOH-l 5108.2-2T 003 A:SOH-2 5902.5-1T 003 A:SOH-2 5902.5-2T 004 A:SOH-2 6032.5-1T 004 A:SOH-2 6046.1-2T 002 S:SOH-2 6625.3-1T 003 S:Ql~RTZ

T 006 S:TEST3T 013 S:SOH-6229.5-1T 004 A:SOH-2 6625.3-1T 004 A:SOH-2 6752.3-1T 004 A:SOH-l 3066-2T 004 A:SOH-l 3113.1-1T 004 A:SOH-l 3652.1-1T 003 A:SOH-6229.5-1T 013 S:SOH-l 5289.5-1T 013 S:SOH-4 2442.5-1T 013 S:SOH-4 2849.5-1T 012 S:SOH-4 2873.5-1T 013 S:SOH-2 4469.4-1T 012 S:SOH-2 4469.4-2T 013 S:SOH-2 4663-1T 012 S:SOH-2 6543.5-1T 013 S:SOH-2 5235.6-2T 013 S:SOH-2 5235.6-3T 013 S:SOH-2 5236.8-1T 013 S:SOH-2 5283-1T 013 S:SOH-2 5485-1T 013 S:SOH-2 5544.6-1T 012 S:SOH-2 5627-1T 012 S:SOH-2 5818.3-1T 013 S:SOH-2 5917-1T 012 S:SOH-2 5945.5-1T 013 S:SOH-2 5969.9-1TOil S:SOH-2 5997-1T 012 S:SOH-2 6000.1-1T 013 S:SOH-2 6660-4T 013 S:SOH-2 6260.8-1T 012 S:SOH-2 6332.5-1T 012 S:SOH-2 6402.4-1TOll S:SOH-2 6535-1T 005 S:SOH-4 3491.8-1