- Page 3 and 4: m*m !:6yAy~ru Kiiolheque mciaie du
- Page 6 and 7: SUBJECT CATEGORIES REPRINTS Y " W 1
- Page 8 and 9: The sphalsrlte deposit at Newfoundl
- Page 10 and 11: stages along frastum zones es fract
- Page 12 and 13: .ining, drilling programs and a com
- Page 14 and 15: VOlAJME I UBSTWLCT ADOsnn~NTS TDBLE
- Page 16 and 17: 3.5.2 Depositional Enviromnt 3.6 We
- Page 18 and 19: 5.13 Implications of hsoc Elenent G
- Page 20 and 21: CHAPTER 11 PRE-ORE EPIGENETIC DOLOS
- Page 22 and 23: mamn 14 SYN~IESIS OF mmsE W~STONEJ
- Page 24 and 25: able 3.1 Stretigraph10 Nmenciatvre
- Page 26 and 27: Figure 4.7 isopach map of tne middl
- Page 28 and 29: Fiwre 12.4 moss-section thmugh the
- Page 30 and 31: XX iv Plate 11.2 Spnaierite Ore Hab
- Page 32: Pirure 1.1 Location and Geologic Ma
- Page 35: Fig;rr 1.2 St~.atig~aphy of the Aut
- Page 39: Nzn is situated in a fault hlmk def
- Page 43 and 44: A CROSS-SECTION OF DOLOSTONE BODIES
- Page 45 and 46: production is 1975. Wining and expl
- Page 47 and 48: aqpects of the largar topic. The in
- Page 50 and 51: RIB FUSITXIN OF m I A N E ZINC WINE
- Page 52 and 53: zinc mncrsl~zation aa sphaleritc is
- Page 54 and 55: dol.mltieed, peritidal redinmnta of
- Page 56 and 57: !ndllnleyrr, 1911; oallrneyer and H
- Page 58 and 59: mineralizd intervals Include: (1) g
- Page 60 and 61: IRGE GROUP
- Page 62 and 63: with dolmite-chert brecslas (Knight
- Page 64 and 65: The entire formation is dolmitized
- Page 66: ~lgure 2.2 liostratigraphy of the S
- Page 69 and 70: atfizns the late Canadian age of th
- Page 71 and 72: mudstones, peloidel pramstones, sma
- Page 73: alrle Point mrmation belong to the
- Page 76 and 77: The follnvlng discussion describes
- Page 79 and 80: 3.2 suatigcaphic mntml and nevi- of
- Page 82 and 83: ST. GEORGE GROUP TABLE 33 STRATIGRA
- Page 84: plate 3.2 Middle Catashe Formation
- Page 87 and 88: diverse associated banthnnic fauna
- Page 89 and 90: 3.6.1 Litholwies Peloidal grains fo
- Page 92 and 93:
- ~hr collective presenss of peloid
- Page 94 and 95:
(I) Chsrts - t%w tmes of chert occu
- Page 96 and 97:
I% OWED WACKESTONE T" I PELOIDAL GR
- Page 98 and 99:
(2) As sea level ria* drowned the s
- Page 100 and 101:
many beds call be correlated beyond
- Page 102 and 103:
____Y.,l. ..G
- Page 105:
~ia'e 4.1 %r,athune Porntion - hini
- Page 108 and 109:
dololminltes, exeept for gruptolite
- Page 110 and 111:
(5) Cherts - chert iv comnly bssoci
- Page 113 and 114:
paztially cemnteil by chalcedony. M
- Page 115 and 116:
Yig~lrr 4.3 H~rltigeneiatlonal brec
- Page 117 and 118:
~;lssls; (4) up to 30% late silica
- Page 119:
Figure 1.4 vertical Distribution of
- Page 122 and 123:
urrwed bed. The mar Wgiiiite morkcr
- Page 124 and 125:
TABLE POINT MINE NW GRAVELS IDDH 96
- Page 126 and 127:
also precipitated f m the brines; p
- Page 128 and 129:
Internretation s~btidniblntertidal
- Page 130 and 131:
100 subtidal/ intertidal units burr
- Page 132 and 133:
follow~d by accretion of laminitas.
- Page 134 and 135:
&er. Plirck brm-wttied feci-3 in th
- Page 136 and 137:
a ag- 3 ;- % g- a II Hi- ; !- z w o
- Page 139 and 140:
srghlricant emsional relief of up t
- Page 141 and 142:
(1) Massive, finely crvstal1ir.e do
- Page 143:
plate 4.3 chert Pebble Beds above t
- Page 146 and 147:
lnneine sheet flmds over the hard c
- Page 149 and 150:
1.6.5 Depeitional Inyimmsnt " The S
- Page 151 and 152:
Fo!.matiun). The sc3inmts were depo
- Page 153:
the platform into a foredeep (Stenz
- Page 156 and 157:
This chapter describes the dtrogrsp
- Page 158:
dolomite powders were determined re
- Page 162 and 163:
~ m p l e with ~ varying Nacl r 11,
- Page 165 and 166:
*. purple tm crystals of blcmite 1
- Page 168:
Plate 5.3 Dolomites I and I1 a. Dvl
- Page 171:
llgvre 5.7. Isotr,pe and Fluid Incl
- Page 174 and 175:
' (PI. 5.3a,
- Page 176 and 177:
and Iimencslone diegenesis. Calcite
- Page 178:
a. C-site "Cm' crystals with cloudy
- Page 181 and 182:
he rtoisnimerric (51 wle % CeCO.1 d
- Page 183 and 184:
Fe AND Mn IN ZONED DOLOMITE Ill
- Page 185 and 186:
alonr faults in lower parts of the
- Page 188 and 189:
E. Xenotopic, replacement saddle da
- Page 190 and 191:
FLUID INCLUSION TEMPERATURES SADDLE
- Page 192 and 193:
Petroqraphx and Distribution - Iwrt
- Page 194:
a. "late 5.6 Fluid Inclusions in Sa
- Page 198 and 199:
la) White, tlensiucant void-filling
- Page 200 and 201:
-- Fluid Inclusions - Typical, low
- Page 202 and 203:
Cathodolminessence - Oolmita VI is
- Page 204 and 205:
enriched in 6'"O and depleted in 6'
- Page 206:
Figure 5.5 Isotopic Ueta for Late P
- Page 209:
Piguce 5.6 Paragenetic Sequence Cha
- Page 212 and 213:
li17 diagenetic stages and other ev
- Page 214 and 215:
Figure 5.1 Pluid Inclusion Saliniti
- Page 216 and 217:
186 two or mre separate fluids as s
- Page 218 and 219:
A. EARLY DOLOMITES 6. EPlGENETlC DO
- Page 220 and 221:
equation: WjR = log. (6,.~,,., + a
- Page 222 and 223:
WATERIROCK RATIO CURVES FOR VARIABL
- Page 224 and 225:
saline pore fluids at 10'C end init
- Page 226 and 227:
Port-tectonic fault-mlat.4 dolcrait
- Page 228 and 229:
hwrver, crystellired at depth long
- Page 230 and 231:
,.. 7,> rnv l~\eJilrn ~~em~orpl~ls
- Page 232 and 233:
quigranuiar crystals, which replace
- Page 234 and 235:
?O.I ~olc~~nila IV - upper catmhe c
- Page 236 and 237:
increased fluid-mck IRKLiM, cooling
- Page 238:
Plate 6.1 Colaur Phases of Sphaleri
- Page 242:
ig~~n 6.1 paregenesis of Pigenetic
- Page 245:
a. riare 6.2 Early Pyrite, Rerl and
- Page 248 and 249:
6.1 ~a.1~ Red sphlerite Petrwraph~
- Page 250 and 251:
Crystal rosettes, 5 fo 20 m in diam
- Page 252:
Pisure 5.1 Fluid Inclueion Dab from
- Page 255:
a. Gmth layers of prismatic crystal
- Page 258:
Figure 6.3 Distribution of Fluid In
- Page 261 and 262:
SPAR BRECCIA 1:iD"E:ED51'A%n YELLOW
- Page 263:
a. Plale 6.4 bate Sphalerites Mediu
- Page 266 and 267:
~.lgure 6.5 variation of Late Sphel
- Page 268 and 269:
-- Evidence of - Yellow-brawn sphal
- Page 270 and 271:
-- Fluid Inclusions - One to Lventy
- Page 272 and 273:
lrlate b.5 Mtt-Ore Sulphates, Sulph
- Page 274 and 275:
lnlficant trace olmnt abundance=. 6
- Page 276 and 277:
40.0 n * 39.0 P m N 88.0 TABLE HEAD
- Page 278 and 279:
GALENA WlTH EARLY RED SPHALERITE GA
- Page 280 and 281:
&ring oxidation ot formational flui
- Page 282 and 283:
Petrwra~h,hp and Distribution - Euh
- Page 284 and 285:
mmpling across tho nine urea is nee
- Page 286 and 287:
Ute red sphelerite is "aiatively de
- Page 288 and 289:
crystallization of sulphides sulphu
- Page 290 and 291:
thtough the sedimentary pile (~uind
- Page 292:
cd 0: mineralization in both early
- Page 296 and 297:
A ~1088-~.~0ti0n aembs the L Zone o
- Page 298 and 299:
COMPARISON OF DOLOMrrE AND DOLOSTON
- Page 300 and 301:
170 above the St. George Uncontomit
- Page 302:
Qiqura 7.2 Dlatribution of the five
- Page 305:
Figure 7.3 A pmEile of flne rock-mt
- Page 309 and 310:
fault zones (Figs. 4.6, 6.7, 1.3).
- Page 312 and 313:
e. Oligwict breccia. Catoshe Fomtio
- Page 314 and 315:
stylolites separate fragments and p
- Page 317 and 318:
TABLE 7.2 BRECCIA TYPES VARIETY OF
- Page 319 and 320:
TABLE 7.3 BODY TYPES OF ROCK-MATRIX
- Page 321 and 322:
Tile lower nrelabsr of the Armathun
- Page 323 and 324:
ceussd subsidence of the lower mbsr
- Page 325 and 326:
4) Chinw B-c& - Chimney-shaped brec
- Page 327 and 328:
247 Fracturing and ~ubsvrface karat
- Page 329 and 330:
EVOLUTION OF KARST BRECCIAS
- Page 331 and 332:
8.1 Intmhlction me formatinn of ear
- Page 334 and 335:
secondary pores in these dolastones
- Page 336 and 337:
P~(JUIE 8.2 Dlbtribation of Deep Di
- Page 338 and 339:
llared on detailed petrographic rel
- Page 341 and 342:
Strnta'nd complexes of epigenetlc,
- Page 343 and 344:
Figtllo 9.1 llpp:~ Catoshs Doloston
- Page 345:
'lrure 9.2 Rciatiollahip between Sp
- Page 349:
~iqure 9.4 ~istribution or bate Fau
- Page 352 and 353:
10.1 Relative We Rslatiships ot Str
- Page 354 and 355:
trending reverse and thrust faults
- Page 357:
Piaura 10.2 structure of ths East L
- Page 361:
~igur~: 10.4 ~istribution of ~yper
- Page 365 and 366:
'omation. Mineralized velns ore rel
- Page 368:
;I. Piate lo. I Veins and Vein-Brrs
- Page 372 and 373:
Thlee gemrations of structures, whi
- Page 374:
~igure 10.8 orientation of Veins in
- Page 377 and 378:
~~gure 10.8 r.mss-ncction of a vein
- Page 379 and 380:
fractures and hrecdos. Both Saddle
- Page 381 and 382:
tant but subordinate roles. Dolosto
- Page 383 and 384:
~lo~tone beds at "30" end "66". 357
- Page 385:
Ylgure 11.1 Evolution of Cwrsc Matr
- Page 388 and 389:
12.2 Sphalsrite Boaiea: meir Intern
- Page 391 and 392:
Flgvre 12.2 Mngitudinsl Profile of
- Page 393:
~bfe 12.1 DisLribution of Sphheieri
- Page 396:
~iyure 12.3 Detailed Zinc Grade Dis
- Page 399:
a. Platr 12.2 Sphalerite Ore Habits
- Page 402 and 403:
covity-base precipitates ere also t
- Page 404 and 405:
1741 pervaled unironly pr011s dolos
- Page 407 and 408:
13.2~. he footwall and, In places,
- Page 409 and 410:
,, ,D,ISTMUTION OF EARLY AND LATE S
- Page 411 and 412:
WLPHlDE ZCNAilON, LONG HDLE SIOPE.
- Page 413 and 414:
Steqe 2, Red Wmlerita - early red s
- Page 415 and 416:
12.4, 12.6). A two stage dcveiopmen
- Page 417 and 418:
the area. The diseontinurms nature
- Page 419 and 420:
(Iv) attd sphalerite overprint styl
- Page 421 and 422:
ulphide precipitation sa regionally
- Page 423 and 424:
pul.oua dolostanes along multiple t
- Page 425 and 426:
DEFORMATION MODEL FOR GROUND PREPAR
- Page 427 and 428:
Thus, Wann to hot ore fluids poaaib
- Page 429 and 430:
CCR 10 -40 - 50 TRANSPORT ' pH META
- Page 431 and 432:
DTEomtional events cnated fracture
- Page 433 and 434:
solution oE carbonates; (3) apparsn
- Page 435 and 436:
~igurc 13.1 Regional Distribution o
- Page 437 and 438:
contrast to the local occurrenca of
- Page 439 and 440:
13.3.1 Definition TI!= mck nmd pseu
- Page 442 and 443:
e. Cumd planar hndrries (arrou) mnt
- Page 445 and 446:
,?. 1xmal ic!bra fabrics nsmc1iAr.d
- Page 448 and 449:
. coarse spnrry dolostone matrix (g
- Page 451 and 452:
13.3.2 cqetal T-s of PeeudDbncda .1
- Page 453 and 454:
P~a~dobm~~lil Is widespread in the
- Page 455 and 456:
madium Erystalline gray &lortonc. T
- Page 457 and 458:
I FABRIC ELEMENTS OF PSEUDOBRECCIA
- Page 459 and 460:
429 fluids, are reduced in pisc fmn
- Page 461 and 462:
431 by saddle dolaoite. l'hs.grsy d
- Page 463 and 464:
igurc 13.1 Evolution of Pseudobrecc
- Page 465 and 466:
435 nf tletrea thmugh adarae gray d
- Page 467 and 468:
woluding pore-centre cements. nn (6
- Page 469 and 470:
open dur~ng the four'stage precipit
- Page 471 and 472:
1.11 paeudobrec~ia beds, Which also
- Page 474 and 475:
lw metres in diarnetm by M to 50 m
- Page 476 and 477:
19191. Flllld pmasure could have bu
- Page 478 and 479:
1.10 betwoen pseudobreccia and lime
- Page 480 and 481:
trosture conduits adjacent to react
- Page 482:
8~guro 13.5 Lalc Galmitization (YII
- Page 485 and 486:
13.8.2 Intqzetstim Ssddle doldter i
- Page 487 and 488:
saddle dolomite. Discoldant gray do
- Page 489 and 490:
,159 fracturing during fluid migrat
- Page 491 and 492:
ing coarse crystalline sphalerite a
- Page 493 and 494:
Fracturing as the sudden decrease i
- Page 495 and 496:
igration and mture of the fluids ha
- Page 497 and 498:
free of H,S and precipitate sulphid
- Page 499 and 500:
igure 14.1 schematic rross-section
- Page 501 and 502:
Figure 11.2 Fault dnd Stratigraphic
- Page 503 and 504:
the basin during R them1 peak. ~nit
- Page 505 and 506:
mring the deposition of the upper S
- Page 507 and 508:
a. MIDDLE ClTOCWl FORYATloH b. UPPE
- Page 509 and 510:
,119 extensive rtratabovnd dissolut
- Page 512 and 513:
and fracture systems fomd as anothe
- Page 514 and 515:
PTimry lithology and fracture linea
- Page 516 and 517:
Host dolostone beds in the mine ace
- Page 518 and 519:
tines and lneteorio vaterr that mig
- Page 520 and 521:
deformtion generated regionel metam
- Page 522 and 523:
hydrothermal fluids into the upper
- Page 524 and 525:
sphalerite canplexcs. These "open w
- Page 526 and 527:
v. 50, p. 371-394. AILSTEM, K.L. an
- Page 528 and 529:
Carbonate ressrvoirs as Illustrated
- Page 530 and 531:
H~mn and Energy, Repor6 86-1, p. lb
- Page 532 and 533:
nmpuFTm, P.W., 1971, Late ?err-n do
- Page 534 and 535:
Daniel's Ilarboar. western Newfound
- Page 536 and 537:
drp*ition.,?uert. Jwr. cwi. w iety,
- Page 538 and 539:
New 'fork, b33p. POLBY, N.K., SINWI
- Page 540 and 541:
CaINES, A.M., 1980, Dalmitieation K
- Page 542 and 543:
GRBNIER, R. and C A W , P.. 1988, V
- Page 544 and 545:
Scl~uol of Mines Quarterly. v. 82,
- Page 546 and 547:
HITCHON. 8.. 1969, Fluid flow in we
- Page 548 and 549:
fra~tion&l'eryatallisatlon, adcwlur
- Page 550 and 551:
Geol. bsac. of Canada. Geosclence C
- Page 552 and 553:
KNIGHT, I., lPBbb, Geology of the P
- Page 554 and 555:
WWD, L.S., 1987, Basinal doldtirati
- Page 556 and 557:
14. P. l87;196. UIVERINO, P.S., 196
- Page 558 and 559:
Spec. ~ubl: 36, p. 223-210. WORE, G
- Page 560 and 561:
5.80 tion, hotspbt tracks end miner
- Page 562 and 563:
PRUTT, B.R., 1982,. Limestone respo
- Page 564 and 565:
I A ~ smaiun, O 9- Bird. utah, p. 4
- Page 566 and 567:
Misniaaippi Islley-type zinc-lead d
- Page 568 and 569:
?:I11 SIBmY, D.P., 19S9, mlanite st
- Page 570 and 571:
'140 SlOUGP, S.S., 1982,'Praliminar
- Page 572 and 573:
yold exploration in Newloundland. I
- Page 574 and 575:
WATSON, I.M., 190, mniel's nerbour,
- Page 576 and 577:
views - dlsc~ssion. Jmr. of Sed. Pc
- Page 582 and 583:
APPENDIX C X-RAY DIFFRACTION DATA F
- Page 585 and 586:
EWlY Red 61-63.3 37 0.02 1.9-7.0 0.
- Page 587 and 588:
Early Yellow ZnS 8-1 0.5 0.1 1.0 fl
- Page 589 and 590:
Cw~tal m e Early UI1site mlmite III
- Page 591 and 592:
CNSW Twe g0nrnh Ro. % V O ~ ~ B lad
- Page 593 and 594:
mt.1 m e '--h 'Pn Ih Late calcite K
- Page 595:
;'RILL HOLE 482, SOUTH OF THE L ZON