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The Geology of the Endeavor Mine - an update -

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1973: Discovered by EZ - bullseye mag anomaly with coincident ... 1200m siliclastic turbidites overlie limestone breccia. Tuffs and two shale rich units markers ... – PowerPoint PPT presentation

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Title: The Geology of the Endeavor Mine - an update -


1
The Geology of the Endeavor Mine- an update -
  • Peter Nicholson, Don Smith and Vanadis Mares

CBH Resources Limited
2
History
  • 1973 Discovered by EZ - bullseye mag anomaly
    with coincident Pb/As in soil
  • 1983 Production begins from Elura Mine
  • 1998 Intersection of mineralisation close to
    limestone at 1200m depth
  • 2003 Purchased by CBH Resources Ltd. and renamed
    Endeavor Mine

CBH Resources Limited
3
Production
  • At June 2005
  • Resources 17.7 MT
  • 4.9 Pb, 8.7 Zn, 69 g/t Ag
  • Reserves 11MT
  • 4.9 Pb, 7.9 Zn, 66 g/t Ag
  • Mine Production 24MT
  • At present, production is ramping up to a rate of
    1.4 MT per annum

CBH Resources Limited
4
Cobar Basin Mineralisation
  • Generally polymetallic discordant veins hosted by
    siliciclastic turbidites
  • Often in anticlines adjacent to competent
    lithologies
  • Concentration of shows within structural corridor
    on E margin
  • Transfer structures often present
  • Largest deposits adjacent to basement protrusions
    into Basin

CBH Resources Limited
5
Cobar Basin Mineralisation
The Peak
after Lawrie and Hinman 1998
500m
25640E
Rhyolite
Rhyolite
100m
  • Generally polymetallic discordant veins hosted by
    siliciclastic turbidites
  • Often located in anticlines adjacent to competent
    lithologies, e.g. limestone at Endeavor, rhyolite
    at The Peak, basic intrusive at Louth

CBH Resources Limited
6
Structural Corridor
Cobar TMI Corridor is defined by mineralisation,
coincides with magnetic, gravity and geological
fabric
CBH Resources Limited
7
Basement Protrusions
Cobar Basin Gravity Basement protrusions
indicated by gravity low anomalies and doming of
sediments
CBH Resources Limited
8
  • Cobar Basin
  • Summary

structural corridor
CBH Resources Limited
9
surface
sulphide stringers
  • Endeavor Mine
  • 7000N Cross Section
  • 1200m siliclastic turbidites overlie limestone
    breccia
  • Tuffs and two shale rich units markers
  • South plunging anticline
  • Early concordant and steep NNW faults
  • Later steep N and NNE faults cut mineralisation

upper shale
9600RL
high-grade massive sulphide
lower shale
limestone
4900E
200m
CBH Resources Limited
10
surface
  • Endeavor Mine
  • 7000N Cross Section
  • Above 900m depth within anticline axis
  • Truncates against shales
  • Offset by N and NNE faults
  • Sub vertical pipes within sheet
  • Below 900m mineralisation bifurcates into two
    concordant zones that dip down anticlinal limbs
  • Alteration
  • Siderite clots and replacement forms halo several
    tens of metres around sulphide stringers.
    Preferentially replaces siltstone/sandstone
  • Silicification and chloritisation intense in
    places

sulphide stringers
upper shale
9600RL
high-grade massive sulphide
lower shale
limestone
4900E
200m
CBH Resources Limited
11
  • Endeavor Mine
  • 7075N Cross Section

Sandstone/shale
Lower shale
PO/PY/SIPY
VEIN 6-10PbZn
MINA 1-6PbZn
20m
CBH Resources Limited
12
  • Endeavor Orebody 9400RL plan
  • Mineralisation in anticline axial plane
  • Low-grade halo of sulphide stringers
  • open along strike
  • N and NNE faults truncate

CBH Resources Limited
13
  • Endeavor Mine Schematic
  • Long Section

7000N
CBH Resources Limited
14
Metal Zonation (long section slices)
gt9.0
gt0.6
0.04-0.1
1.0-2.0
Zn
Cu
Ag
100m
Cu
  • Zinc Highest grade (8-10) in centre of pipes. Pb
    similar
  • Silver Concentrated on upper/outer margins. Up to
    1000ppm
  • Copper Up to 4 in small pods at base of pipes

CBH Resources Limited
15
Metal Zonation - Cross Section 7080N
CBH Resources Limited
16
Endeavor Mine Mineralisation Textures
  • Axial Plane Mineralisation
  • Massive textured and banded
  • Banding sub parallel to contacts
  • Often rapid transition from altered sediments
  • Concordant Mineralisation
  • Quartz-siderite veins along strike
  • Low grade material composed of discordant veins
    and concordant replacements

CBH Resources Limited
17
Mineralisation Textures
Face showing near-horizontal bedding in lower
shale unit with siltstone layers replaced by
pyrite, sphalerite galena Vein at the centre
of the photo sub parallels cleavage measures
20cm
CBH Resources Limited
18
Mineralisation Textures
20 mm
CBH Resources Limited
19
Mineralisation Textures
sphalerite
galena
sphalerite
10 mm
CBH Resources Limited
20
Endeavor Mine Exploration
  • Massive sulphide zones open up dip, down dip to
    N of current workings
  • Mineralisation near limestone contact to be
    tested from W
  • High metal prices have encouraged investigation
    into mining zones of stringer mineralisation
  • Stringer zone open along strike to N S, down
    dip on both limbs. May contain more massive
    sulphide or lower grade zones

CBH Resources Limited
21
Endeavor Mine Exploration
Massive Sulphide
sulphide open
sulphide stringers open
stringers open
sulphide stringers open
Limestone
Contact mineralisation partially defined
22
Endeavor Mine Exploration
Planned drillholes
  • Drilling planned to
  • test mineralisation
  • adjacent to the
  • limestone contact

limestone
lower shale
50m
CBH Resources Limited
23
Endeavor Geology Update - Summary
  • Mineralisation localised in zones of competency
    contrast on both regional and local scale
  • Shale-rich sequences appear to truncate axial
    plane mineralisation
  • Concordant mineralisation may be important
  • Better understanding of mineralisation controls
    and high metal prices has expanded exploration
    opportunities

CBH Resources Limited
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