,UMR PURU...... 11' '1 AC (LENDL."lG SEC1LJi\J).
Bureau of Mineral Resources, Geology & Geophysics
Record 1991/28
CATALOGUE OF FIELD COMPILATION SHEETS OF LATE PALAEOZOIC IGNIMBRITES AND ASSOCIATED ROCKS IN T1IE BURDEKIN FALLS DAM - "CONWAY" AREA (GLENDON AND ADJACENT PARTS OF RAVENSWOOD, STRATHALBYN, HARVEST HOl\lE, AND COLLINSVILLE 1:100000 SHEET AREAS), NORTHEASTERN QUEENSLAND
Record 1991/28
CATALOGUE OF FIELD COMPILATION SHEETS OF LATE PALAEOZOIC IGNIMBRITES AND ASSOCIATED ROCKS IN THE BURDEKIN FALLS DAM - "CONWAY" AREA (GLENDON AND ADJACENT PARTS OF RAVENSWOOD, STRATHALBYN, HARVEST HOME, AND COLLINSVILLE 1:100 000 SHEET AREAS), NORTHEASTERN QUEENSLAND
B.S. Oversby% D.E. Mackenzie% J. McPhie 2, S.R. Law 3 , and D. Wyborn i
Bureau of Mineral Resources, Minerals and Land Use Program 2 University of Tasmania, Centre for Ore Deposit and Exploration Studies 3 United Reefs NL, Kilkeven, Queensland 1
Copyright (c) Commonwealth of Australia, 1991
Persons purchasing copies of this Record may reproduce any part of it for their own use or for that of their staff, but not for any other purpose except with the written permission of the Executive Director, BMR.
111 111 I I I I 2
@Commonwealth of Australia, 1991
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INTRODUCTION The geological maps which are reproduced here at approximately 1:100 000 scale have been compiled directly from basic field data and supplementary airphoto interpretation which were recorded on overlays to 1:28 000 (nominal)-scale colour airphotographs taken in April, 1988. The fieldwork on which these maps are based was undertaken as part of a joint Bureau of Mineral Resources and Queensland Department of Resource Industries investigation aimed at elucidating the regional setting of epithermal-type gold mineralisation in the area of the northern Drummond Basin. The mapping was a continuation of systematic mapping undertaken previously by the-then Geological Survey of Queensland in the Mount Coolon and Byerwen 1:100 000 Sheet areas to the south of "Conway" (HUTTON, L. J., GRIMES, K. G., LAW, S. R., McLENNAN, T. P. T., & BELCHER, R., in press - Geological mapping in the Mount Coolon 1:250 000 Sheet area, 1986. Geological Survey of Queensland Record 1987/59). The work was designed to complement specialist gold mineralisation studies being undertaken concurrently in the southern part of the area (EWERS, G., 1989 - Recognising sinters in epithermal gold deposits. BMR Research
Newsletter 11, 5-6; EWERS, G., 1990 - Epithermal sinters: a low-cost exploration tool. BMR Research Newsletter 12, unpaginated supplement, second page; EWERS, G. R., WOOD, D. G., TEDDER, I. J., WHITE, N. C., & HOFFMAN, C. F., 1990 - Epithermal gold prospects in the Conway area, northern Drummond Basin, Queensland. Pacific Rim 90 Congress Proceedings, II, 357 - 362; EWERS, G. R., 1990 - The isotopic recognition of sinters in epithermal gold deposits (abstract). BMR Record 1990/95, 17-18; EWERS, G. R., 1991 - Oxygen isotopes and the recognition of siliceous sinters in epithermal ore deposits. Economic Geology, 86, 173-178). Reconnaissance traverses by Oversby in 1987 were followed in 1988 by systematic studies by all personnel. Preliminary results were presented by: LAW, S., MACKENZIE, D., McPHIE, J., OVERSBY, B., WELLMAN, P., & WYBORN, D., 1989 - Geological setting of gold mineralisation in the northern Drummond Basin: significance of the Bulgonunna Volcanics (abstract). NQ Gold '89 Conference Proceedings, 47-50); and EWERS, G., MACKENZIE, D., McPHIE, J., OVERSBY, B., WYBORN, D., & LAW, S., 1989 - New mapping extends Drummond Basin gold potential. BMR Research Newsletter 10, 1-4. All but Law also spent time in the field in 1989, with special attention being given to resolving problems introduced by isotopic dates obtained after the 1988 season. Revised interpretations arising from this final fieldwork phase of the research have also been presented briefly, in conjunction with some major conclusions of the specialist mineralisation studies, by: OVERSBY, B. S., EWERS, G. R., MACKENZIE, D. E., McPHIE, J., WYBORN, D., LAW, S., & BLACK, L. P., 1990 - Volcanic setting of epithermal
1
gold mineralisation in the northern Drummond Basin, Queensland. Geological Society of Australia Abstracts 25, 36; McPHIE, J., BLACK, L. P., LAW, S. R., MACKENZIE, D. E., OVERSBY, B.S., & WYBORN, D., 1990 - Distribution, character and setting of mineralised Palaeozoic volcanic sequences, Burdekin Falls region, northeastern Queensland. Pacific Rim 90 Congress Proceedings, II, 465-471; BLACK, L., MACKENZIE, D., OVERSBY, B., & McPHIE, J., 1990 Setting of epithermal gold mineralisation in the northern Drummond Basin further refined. BMR
Research Newsletter 12, 14-15; and EWERS, G., MACKENZIE, D., OVERSBY, B., & WYBORN, D., 1991 - Regional oxygen-isotope patterns - implications for epithermal gold explorration. BMR Research Newsletter 14, 1-2. The most recent zircon U-Pb isotopic data to have become available (L. P. BLACK, personal communication) strongly suggest that all of the Carboniferous extrusive rocks previously assigned to either a lower "Cv" sequence or an upper Bulgonunna Volcanics "proper" sequence accumulated during the same Late Carboniferous time interval, and to some degree originally interfingered laterally; these units are probably better regarded as volcanic facies associations than as traditional lithostratigraphic entities. Many of the granitoids in the study area also appear to have been emplaced during the same time interval. Even though some Carboniferous granitoids can be demonstrated from field evidence to antedate the extrusive activity, there do not seem to be any which are of Early Carboniferous age. On the field compilation sheets, and in the key to rock units given below, different symbols separated by an oblique stroke (/) relate to what are known or inferred to be the same unit. The convention appears on compilation sheets in those areas where equivalence has been demonstrated, or most strongly inferred. At this stage, no serious attempt has been made to achieve uniformity of map unit symbol styles throughout the study area. Different styles were developed semi-independently in the four minimally overlapping areas of mapping responsibility (as indicated on the compilation sheets). The stylistic variability emphasises what appear to be some real stratigraphic differences between the areas, differences which presumably reflect original contrasts in local to semi-regional volcanic and/or volcano-tectonic environments. Some multiplicity of symbols applied to Mesozoic and Cainozoic units has also been inherited from mismatches between previously-published maps (e.g. Charters Towers, Sheet SF 55-2, and Bowen, Sheet SF 55-3, First Edition 1:250 000 Geological Series; Bureau of Mineral Resources, 1969 and 1971 respectively).
2
RAVENS- 147°00' WOOD (8257) ^20 ° 30 1^
11-7° 30 1
STRATHALBYN^(8357)
BOQI E (8457) COLLINS(8456)
21 °00 1^
SCARTWATER (8255)
MOUNT^BYERWEN COOLON (8355) ^(8455) Previous13 mapped bj SQ
Fist Location OF Burdekin Falls Dam - "Conwaj" area, and keij to 1:100 000 Sheets
KEY TO STRATIGRAPHIC UNITS In the rock unit descriptions below, the following terminological convention regarding clast/crystal/phenocryst contents (volume %, mostly estimated visually) of pyroclastic rocks (including ignimbrites), lavas, and intrusive rocks is used as appropriate: 0
=
clast-/crystal-/phenocryst-free m.. aphyric
^very^.,^-/^,, >0 to 1% = -/ 1% to 5%
^II
=
^-/^II
4
N
-poor a very sparsely porphyritic -poor a sparsely porphyritic
5% to 10% = moderately ti^-/ it -/^t,^-poor -,7: moderately sparsely porphyritic 10% to 25% = moderately ti^-/ II -/^II^-rich7.---- moderately abundantly porphyritic 25% to 50% = i,^-/^ii -/^ii -rich:-.._ abundantly porphyritic 50%+ = very^ti^-/^ii -/ ., -rich a very abundantly porphyritic Nomenclature of pyroclastic rocks is taken from Le MAITRE, R.W. (editor), 1989 - A Classification of Igneous Rocks and Glossary of Terms. Blackwell Scientific Publications. Nomenclature of intrusive igneous rocks is based on STRECKEISEN, A.L., 1973 - Classification and nomenclature recommended by the JUGS Subcommission on the Systematics of Igneous Rocks. Geotimes 18, 26-30; it is essentially the same as that of Le MAITRE (1989). Suffixes applied to several units on the compilation sheets indicate, as and where appropriate: (h) = hornfelsed; (a) = intensely altered (indicated additionally by stippling); (bx) = brecciated. * denotes reserved, but not formalised, name.
EXTRUSIVE AND SEDIMENTARY ROCKS
QUA'1ERNARY (HOLOCENE)
Qha : active alluvium
4
Qa : rarely active to inactive alluvium, commonly dissected
TERTIARY and QUATERNARY (w) : deep weathering profile
(r) : residual soil CzlCzs : soil and colluvium, locally includes some inactive alluvium
TERTIARY T/Ts = Suttor Formation / Tu : undivided epiclastic commonly clayey quartz sandstones, quartz-clast and polymictic pebbly to cobbly conglomerates; minor tuffaceous(?) mudstones
and siltstones; commonly ferruginised; locally unlithified Td : as TITsgu, intensely ferruginised to lateritised Tb : moderately porphyritic pyroxene-olivine basalt
MESOZOIC to TERTIARY
Mz : quartz sandstone, locally pebbly
LOWER PERMIAN
Plc = Collinsville Coal Measures: undivided; mostly epiclastic rocks, locally calcareous Plz = Lizzie Creek Volcanies : undivided; mostly basaltic to andesitic pyroclastic and epiclastic, and mixed pyroclastic-epiclastic, rocks
5
UPPER CARBONIFEROUS Bulgonunna Volcanics ("proper") association (northwest)
Cbi : undivided medium to dark grey clast-poor to moderately clast-rich 2mm to 4mm-crystalrich rhyolitic to rhyodacitic ignimbrite (Limey Dam area); buff clast-rich crystal-poor to moderatelyly crystal-rich rhyolitic ignimbrite ("Glenroy" area); grey to brown clast -poor moderately crystal-rich to crystal-rich (quartz up to 7mm) rhyolitic ignimbrite (extreme western area) Cb: very dark grey clast-poor to moderately clast-rich moderately crystal-rich to crystal-rich hornblende-biotite rhyolitic ignimbrite Cbn : very dark grey clast-free to clast-poor moderately lmm to 2mm-crystal-poor to moderately crystal-rich (%quartz » %feldspar) rhyolitic ignimbrite Cbm : dark bluish-grey to very dark grey 2mm to 4mm-crystal-rich to very crystal-rich (%quartz > %feldspar) rhyolitic ignimbrite Cbl = Locharwood* rhyolite : medium purplish- to -pinkish-grey clast-free to clast-poor moderately 2mm to 3mm-crystal-rich (%quartz < %[pink] felspar) rhyolitic ignimbrite with characteristic orangey-pink to reddish-brown fiamme up to 1.5cm x 7cm Cbg = Collins Creek* rhyolite : very dark grey to bluish- or greenish-grey clast-free to clastpoor very crystal-rich (%quartz [up to 8mm] > %feldspar) rhyolitic ignimbrite with conspicuous biotite Cbs : epiclastic quartz-lithic sandstone, quartz-clast to polymictic conglomerate, and siltstone; minor epiclastic lithic sandstone
6
Bulgonunna Volcanics ("proper") association (northeast) Cbv : undivided feldspar crystal-bearing and/or feldspar-phyric rhyolitic ignimbrites and/or
lavas Cbith : rhyolitic lava; may be intrusive locally Cbs : stratified crystal- and locally pumice-rich mixed pyroclastic-epiclastic tuffaceous
mudstone, sandstone, and conglomerate Cbi : undivided rhyolitic ignimbrites Cb8 purple moderately 2mm to 3mm-crystal-rich rhyolitic ignimbrite :
Cb 6 : purplish-buff clast-poor moderately 2mm to 3mm-crystal-rich (quartz absent) rhyolitic ignimbrite Cb 5 : pale green 1 mm-crystal-poor rhyolitic ignimbrite Cb 4 : dark blue 4mm to 5mm-crystal-rich rhyolitic ignimbrite Cb 3 : purplish-buff and pink moderately clast-rich lmm to 2mm-crystal-poor rhyolitic ignimbrite CbL = Locharwood* rhyolite : medium grey to pink and buff locally moderately clast-rich moderately 3mm to 5mm-crystal-rich rhyolitic ignimbrite with orangey-pink neutrallyweathering fiamme Cb i = Collins Creek* rhyolite : dark bluish-grey 4mm to 5mm-crystal-rich (mm quartz > mm feldspar) rhyolitic ignimbrite
7
Bulgonunna Volcanics ("proper") association (central-west)
Cby = Arundel* rhyolite, main (upper) interval : medium-grey to purplish-grey clast-poor moderately lmm to 3mm-crystal-rich to crystal-rich (%quartz > %feld,spar) rhyolitic ignimbrite with positively-weathering medium to large fiamme
Cby i = Arundel* rhyolite, subsidiary (lower) interval : medium-grey to buff moderately clastrich to clast-rich moderately lmm to 2mm-crystal-poor to moderately crystal-rich rhyolitic ignimbritels
Bulgonunna Volcanics ff_p_m_e_n association (southwest) Cbl, : rhyolitic lava; may be intrusive locally Cb Mb = Locharwood* rhyolite, main (ung) interval : medium grey to medium buff very clast-
poor moderately 0.5mm to 3mm-crystal-rich rhyolitic ignimbrite with medium orangey-red feldspars and neutrally-weathering small fiamme
Cb Illa = Locharwood* rhyolite, subsidiary (lower) interval : very pale grey commonly "chalky" rhyolitic ignimbrite Cb tIb = Pyramid* rhyolite, main (upper) interval : medium purple or pale red to purplish-brown locally clast-rich moderately 0.5mm to 3mm-crystal-rich to crystal-rich rhyolitic ignimbrite with negatively-weathering fiamme
Cb Ha = Pyramid* rhyolite, subsidiary flower) interval : very pale greenish-grey to pale buff commonly "chalky" rhyolitic ignimbrite Cbs : fine to very coarse epiclastic conglomerate
8
Bulgonunna Volcanics C' proper") association (southeast) Cub,: undivided rhyolitic lavas with ash tuffs to agglomerates and breccias Cub a = Bobby Dazzler* rhyolite : pale grey to buff clast-rich and 0.5mm to 2.5mm-crystal-rich rhyolitic ignimbrite with biotite and very poorly developed fiamme Cubi 1 •• buff moderately lithic-rich to lithic-rich moderately crystal-rich (%quartz «
%feldspar) rhyolitic(?) ignimbrite with biotite
Smedley* volcanic association (northwest)
Cv : undivided quartz-poor rhyolitic to dacitic ignimbrites, andesitic rocks, and stratified lithicrich pyroclastic and mixed pyroclastic-epiclastic(?) rocks Cvx : undivided andesitic lavas, ignimbrites(?), and coarse to very coarse pyroclastic breccias Cve : very dark-grey to black clast-poor moderately very small-crystal-poor dacitic ignimbrite; moderately abundantly porphyritic pyroxene dacitic lava, lithic- and vitric-bearing mediumash crystal tuff with accretionary lapilli Cvd = "dam ignimbrite" : medium to dark grey and purplish-grey clast-poor to moderately
clast-rich moderately lmm to 3mm-crystal-rich (quartz absent to « %feldspar) dacitic ignimbrite with hornblende and minor biotite and common medium to large porphyritic fiamme Cvc : dark grey to very dark grey clast-free to very clast-poor moderately lmm-crystal-poor (%quartz > %feldspar) rhyolitic ignimbrite Cvb : pale to medium brownish-grey to dark grey clast-free to very clast -poor crystal-rich to
very crystal-rich (%quartz » %feldspar) rhyolitic ignimbrite
Cva : dark bluish-green clast-free to moderately clast-rich 2mm to 3mm-crystal-rich (%quartz <% feldspar) dacitic ignimbrite
9
Cvs : epiclastic polymictic pebble to cobble conglomerate and quartz-lithic sandstone Smedley* volcanic association (northeast)
Cv : undivided quartz-poor rhyolitic to dacitic ignimbrites, andesitic rocks, and massive to stratified lithic-rich pyroclastic, mixed pyroclastic-epiclastic, and epiclastic(?) rocks Cvi : undivided ignimbrites; probably includes "dam ignimbrite" Cvi 4 : very dark bluish-grey moderately 2mm to 3mm-crystal-rich dacitic ignimbrite with diffuse attenuated fiamme Cvi3 : very dark bluish-grey clast-rich 2mm to 3mm-crystal-rich (%quartz < %feldspar) dacitic ignimbrite with porphyritic fiamme Cvi2 : medium brownish-grey 2mm to 3mm-crystal-rich (%quartz > %feldspar) rhyolitic ignimbrite with biotite Cvi i : dark bluish-green clast-free to moderately clast-rich 2mm to 3mm-crystal-rich (%quartz < %feldspar) dacitic ignimbrite Cvs : polymictic epiclastic(?) cobble conglomerate; minor fine- to coarse-ash tuff
Smedley* volcanic association (southwest)
Cvt : undivided stratified lithic to lithic-vitric-crystal fine-ash tuffs to fine agglomerates and breccias rhyoliticidacitic ignimbrites Cvl JCvl dlCvl a : rhyoliticidaciticlandesitic lavas; may be intrusive locally
10
Smedley* volcanic association (southeast)
Cvi : undivided rhyolitic and/or dacitic ignimbrites
Smedley* volcanic association ? (southeast)
Cv: undivided rhyolitic and dacitic ignimbrites CVi fiCVi fiCVi fq : dark grey very clast-poor 0.5mm to 2mm-crystal-rich to very crystal-rich
(quartz absent to « %feldspar) rhyolitic(?) to dacitic ignimbrite without fiamme I as moderately clast-rich to clast-rich and locally pale green I as CVif, %quartz < %feldspar
Clilf,
Cv (I) : dark grey moderately clast-rich to clast-rich crystal-rich (quartz absent to « %feldspar) dacitic ignimbrite with hornblende
MID- to UPPER CARBONIFEROUS? Cr : buff to dark grey flow-laminated sparsely porphyritic rhyofitic lava; minor fine- to coarse-ash quartz-feldspar, quartz-feldspar-lithic, and feldspar-lithic tuff; may be intrusive locally
Csv : undivided pale grey to greenish-grey or buff quartz-feldspar-rich fine- to coarse-ash tuffs, clast -poor to moderately clast-rich moderately crystal-rich rhyolitic ignirnbrites, tuffaceous(?) quartz-feldspar sandstones Cs : undivided pale greenish-grey to grey or buff locally lithic-pebble epiclastic(?) quartz to quartz-feldspar sandstones; minor epiclastic quartz-pebble conglomerates Cld : dark brown to greenish-grey or grey moderately porphyritic pyroxene(?)-hornblende andesitic to basaltic lava (?)
11
LOWER to MID(?)-CARBONIFEROUS Star of Hope Formation
Cis : undivided purple, purplish-grey, chocolate-brown, and reddish-brown locally pebbly epiclastic feldspar-lithic to lithic siltstones to sandstones, epiclastic granule- to pebbleconglomerates, epiclastic mudstones, dacitic to andesitic lavas with breccias and rare ash tuffs, clast-rich and crystal-poor rhyolitic ignimbrites and lavas; rare to sporadic fine to coarse lithic- and/or quartz-feldspar ash tuffs with local accretionary lapilli Cls i : dark bluish-grey to brownish-grey clast-rich moderately crystal-poor to crystal-rich (%qyartz < %feldspar) rhyodacitic to dacitic(?) ignimbrite
Clc = Scartwater Formation : undivided grey, greenish-grey, and brown epiclastic quartzfeldspar to quartzfeldspar-lithic sandstones to conglomerates with siltstones and mudstones;
rare clast-rich rhyolitic ignimbrites and lensoidal algal limestones
UPPER DEVONIAN to LOWER CARBONIFEROUS St Anns Formation
DCa : undivided buff to medium greenish-brown fine to very coarse epiclastic lithic and feldspar-lithic sandstones, pale to medium green to greenish-brown micaceous (muscovite) epiclastic siltstones and mudstones, medium to dark grey, commonly laminated and locally algal, silty to medium-sandy limestones DCa.:buff rhyolitic ignimbrite
12
Stones Creek* formation DCv : undivided rhyolitic to andesitic lavas, breccias, agglomerates(?), and ignimbrites, with
brown to purple epiclastic and/or mixed pyroclastic-epiclastic feldspar- and feldspar-lithic to lithic sandstonesltuffaceous sandstones to fine conglomeratesltuffaceous conglomerates; subsidiary siltstonesltuffaceous siltstones; rare algal(?) limestones and jasper DCv s/DCv (s) : undivided, mostly epiclastic and mixed pyroclastic-epiclastic, rocks DCvi- : undivided mostly rhyolitic to rhyodacitic, lavas and ignimbrites
DCvSD C v .1 : undivided, mostly dacitic, ignimbrites DCv ii : quartz-free to quartz-poor rhyolitic(?) to rhyodacitic ignimbrite DCv ii : quartz-free to quartz-poor rhyolitic to rhyodacitic lava
DCv di : dacitic ignimbrite DCv alDCv 00 : undivided, mostly andesitic, lavas and pyroclastic rocks DCv 03) basaltic lava :
UPPER DEVONIAN Dum = Mount Wyatt Formation : undivided epiclastic feldspar-lithic to lithic-feldspar sandstones and fissile mudstones; subsidiary epiclastic conglomerates
MIDDLE DEVONIAN
13
Dk = Ukalunda Beds : undivided fissile to cleaved(?) epiclastic mudstones and quartz-feldspar to feldspar-lithic-quartz sandstones; subsidiary epiclastic conglomerates, limestones, and
cherts; quartz stringers and veins characteristic locally in the northeast
CAMBRIAN and/or ORDOVICIAN Seventy Mile Range Group
COs : undivided medium to dark-grey fine to coarse epiclastic(?) quartz-feldspar (to arkosic) sandstones; minor quartz-feldspar ash tuffs and rhyolitic rocks of uncertain origin's COw = Mount Windsor Volcanics : intensely fractured and altered sparsely porphyritic
rhyolitic rocks of uncertain origin's; minor pyroclastic and/or epiclastic quartz-feldspar coarse-ash tuff/sandstone; rare andesitic lava(?)
LOWER PALAEOZOIC? C0c = Cape River Metamorphics : undivided micaceous quartz-feldspar schists to gneisses with quartzites
PALAEOZOIC Pzv : unassigned extrusive rocks
14
INTRUSIVE ROCKS
UPPER PALAEOZOIC to MESOZOIC(?) q : vein quartz mg : undivided aplites and micro granites to microgranodiorites(?) mg i/po : quartz-feldspar-phyric microgranite to very fine-grained granite mg2 : feldspar-phyric microgranite to leucocratic and mesocratic microgranodiorite(?) Pltr = Mount Wickham Rhyolite : commonly flow-banded and sporadically autobrecciated sparsely quartz-feldspar-phyric rhyolite rh/f : undivided rhyolites to dacites(?); may be extrusive locally (in the Mount Coolon area, most occurrences of the same rocks were annotated Cub rh) rh i : quartz-feldspar-phyric rhyolite; may be extrusive locally rh 2 : feldspar-phyric rhyolite to dacite(?); may be extrusive locally rh3 : aphyric rhyolite to dacite(?); may be extrusive locally ad/Cx : undivided dacites to andesites; may be extrusive locally t : undivided trachytes mdi : porphyritic melanocratic microgranodiorite(?) to microdiorite mgd: porphyritic hornblende-biotite micro granodiorite to diorite agg/Cut : intrusive rhyolitic ash tuff agglomerate, and/or breccia
15
LOWER PERMIAN
Pig: granodiorite
CARBONIFEROUS and/or PERMIAN
CPg b = Bluegrass Creek* granite : biotite granite CPg : pink fine-grained moderately porphyritic biotite granite CPgd : biotite-hornblende to hornblende-biotite granodiorite CPd: dark grey fine- to medium-grained porphyritic pyroxene?-hornblende diorite to gabbro CPi/Cgm/m/do : undivided mafic rocks; may be extrusive locally
CARBONIFEROUS
Cgp : pink to red abundantly porphyritic biotite micro granite to very fine-grained granite Cga : pink to red aphyric "aplitic" biotite micro granite to very fine-grained granite
UPPER CARBONIFEROUS POST-VOLCANIC
Cug b = Bells Creek* granodiorite : fine- to medium-grained hornblende-biotite granodiorite to tonalite Cug/Cug. : undivided and unassigned granites to granodiorites Cug p .: quartz-feldspar-phyric micro granite to very fine-grained granite (in the Mount Coolon area, many occurrences of the same rocks were annotated Cub)
16
Cug ing : aphyric to sparsely porphyritic "aplitic" microgranite to very fine-grained granite Cug i : buff or pale grey to pink medium-grained biotite granite Cug2:grey to pink fine-grained hornblende-biotite granite Cug3:grey fine-grained (acicular) hornblende-biotite granite Cug 4 : bluish-grey medium-grained hornblende-biotite granite Cug slCugh : fine- to coarse-grained hornblende granite Cur : white, buff, pale grey, and medium grey sparsely to moderately quartz-feldspar-phyric rhyolite; commonly with variable but pervasive sericitic alteration and locally, abundant pyrite
PRE-VOLCANIC Clg : undivided granites to granodiorites Clgc : pink coarse-grained granite Clg p .: quartz-feldspar-phyric micro granite to to very fine-grained granite Clg ra = Roscow* granite, granite phase : fine- to medium-grained hornblende-biotite granite Clg r = Roscow* granite, granodiorite phase : fine- to medium-grained hornblende-biotite granodiorite and quartz monzodiorite Clg p = Percy Douglas* granodiorite : fine- to medium-grained hornblende-biotite granite to granodiorite Clg n = Nostone Creek* granodiorite : fine- to medium-grained hornblende-biotite granite to granodiorite and quartz monzodiorite
17
Clg. = Sunbeam* granodiorite /Clgm : fine-grained melanocratic granite to granodiorite Clg i = Joe de Little* granite : fine- to medium-grained hornblende-biotite granite to granodiorite Clg mgh = House and Kitchen* granite /Clg ing : aphyric to sparsely porphyritic "aplitic" microgranite to very fine-grained granite I as Clg mgh but geographically separate
CARBONIFEROUS?
Cgs = Stuart Pocket* granite : pink coarse-grained biotite granite; invariably intensely altered(may be Lower Palaeozoic)
LOWER PALAEOZOIC Ravenswood Granodiorite Compl e x 0Dr : medium grey to pinkish-grey biotite-hornblende to hornblende-biotite granite(?) to granodiorite ODa : pink to pale grey abundantly miarolitic and locally porphyritic biotite granite
18
/
5trati~rQphic
/
Hi9h-on.9le fault
X X
(including intrusive) cont:.aet
Anticlinal axial trace S~nGlinQI axial trace
Where location of contacts, faults, and axial traces is approximate, line is clashed; when "permonentl~" concealed, dotte.d; where inferred or doubtful, ~ueried. Where 9eolo~ical bound(lr~ is of uncertain nature, prefe.rre.d option (contact or fault) is ~ueried.
, II
---<;"0
Strike and dip of strata (/ocall!j includes eu!:4)(itic foliation of i,9nimbritesbelow)
.oK
Vertical strata.
~IO
L
Horizontal strata.
Generalised dip. commonl~ from airphoto interpre.ta.tion
~
Strike and dip of eutaxitic foliation of i9nimbrite
X
VerticClI eutaxibc foliation
~
Strike. and dip of flOW bandin9 of lava and intrusive rocks
J;!?
Ve.rticol flow bands
Ao ).
4"
~t.nualise.d strike and dip of contorted flow bonds Strike. and dip of tectonic foliation
Ala
J
+
D~ke.,
wil:h dip where known (otherwise essentiall~ vertical)
Whae location of d~kes is approximate, concealed, or inferred or doubtful. is dashe.d, .lotted, and queried re.sped:ive.l~.
s~mbol
//
Trend lines
'-,...':<'
Joints
~
Unc.ome.nt
"
81501210
~Rb-5r
JOI32ots
airphoto interprc:.tal:.ion
1 J
Location of geochronolosical sample; With refc.re.nce number, datins method. and 119e. in m"dlions of ~/Ulrs Location
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