Sunday, 18 December 2011
Sunday, 4 December 2011
Wednesday, 19 October 2011
St. Gerasimos church, Lausanne
the couple Kalogeropoulos of Kefalonia who financed the building of the church
Thursday, 22 September 2011
Thursday, 1 September 2011
East Malartic Porphyry Swarm high grades
22-66 high grade intersections (over 1 oz)
16. 13 / 2 ‘
2.45 / 7 ‘
6.64 / 5 ‘
1.28 / 9 ‘
1.25 / 5 ‘
1.26 / 15 ‘
1.11 / 3 ‘
2.58 / 5.5 ‘
1.50 / 2.5 ‘
2.10 / 2.5 ‘
1.74 / 2.5 ‘
1.17 / 2.5 ‘
4.03 / 3 ‘
East Malartic chert grade
EAST MALARTIC : CHERT ZONE ON 22 LEVEL
Drill intersections
Section chert zone in hole grade in oz / ton
--------- ------------------ ----------------------
47 + 50 E chert next to Cadillac Fault
15 ‘ 0.166 22-49 stope
48 + 00 55 ‘ 0.104 “
48 + 50 50 ‘ 0.139 “
49 + 00 45 ‘ 0.093 “
49 + 50 25 ‘ 0.116 with VG “
50 + 00 25 ‘ 0.138 “
50 + 50 25 ‘ 0.090 “
51 + 00 20 ‘ 0.170 not developed
51 + 00 + 40 degrees up 8' 0.110
51 + 00 + 40 degrees up 8' 0.110
51 + 50 20 ‘ 0.137 further east
52 + 00 X-cut
52 + 50 20 ‘ 0.170
53 + 00 20 ‘ 0.160
53 + 50 12.5 ‘ 0.118
54 + 00 10 ‘ 0.070
55 + 00 12.5 ‘ 0.158 with VG
55 + 00 + 30 degrees up 12 ' 0.160
55 + 00 + 30 degrees up 12 ' 0.160
56 + 00 10 ‘ 0.090
56 + 00 15 ‘ 0.140
57 + 00 east wall 20 ‘ 0.110
West wall 15 ‘ 0.125
Strike length : 950 ft. (285 m)
22-49 grade : 469 samples with average grade of 0.306
However, 22-49 channels, mucks average 0.095
Wednesday, 31 August 2011
Mikra Asia
Biggest Ancient Theatre: Ephesos
Biggest Ancient stadium : Aphrodisias
Has about 70 % of ancient Greek / Roman theatres
More churches than mosques
Most mosques are converted Greek churches
Most citizens are originally Christians, forcefully converted to Muslims
Biggest Ancient stadium : Aphrodisias
Has about 70 % of ancient Greek / Roman theatres
More churches than mosques
Most mosques are converted Greek churches
Most citizens are originally Christians, forcefully converted to Muslims
Monday, 29 August 2011
East Malartic Porphyry Swarm zone on 22 level
PORPHYRY SWARM ZONE – 22 LEVEL ( investigated in 1977-78)
22-66 DRILL INTERSECTIONS all values in oz / t
Flat holes
VG VG,VG VG,VG VG
.48 – 1.25 - .11 - .23 – .20 – .18 – .19 – 16.13 – .31 – .13 – .25 – .11 -
VG,VG VG
.17 – .08 – .07 – .04 – .10 – .25 – .03 – .17 – .10 –
.08 - .07 – .02 – 1.11- .08 – .08- .08 – .07 – .07 – .29 –
VG VG,VG,VG VG
.49 – 2.10 – 1.74 – .10 – .13 – .12 – .09 – .10
Average uncut = 0.702
Up holes
VG
2.48– 2.35 – .07- .08 – .08 – .15 – .12 – .10 – .08 – .11 – .05 – .09
VG VG VG
– .09 – .38 – .16 – .09 – .07 – .05 – .17 – .10 --.21 – .07 – .09 – .09
Average uncut = 0.297
Down holes
VG,VG,VG VG VG
.16 – .12 – .05 – .05 – .08 – .71 - .05 – .04 – .01 – .41 – .03 – .03 – .25 –
VG,VG
.01 – 4.03 – .01 – .02 – 1.74 – .02 - .10
VG VG VG,VG,VG
– .02 - .10 -1.17 – .50 – .17 – .14 – .28 – 2.58 – .10 – .12 – .09 – 1.50 - .08
Average uncut = 0.472
Average chemical composition of 4 samples (Kerrich, 1983)
%
SiO2 65.83
TiO2 0.5
Al2O3 15.16
Fe2O3 3.17
MgO 1.16
CaO 2.91
K2O 1.41
Na2O 7.07
P2O3 0.2
ppm
Au 0.16
Cr 29
Ni 15
Sr 1108
Ba 1372
Zn 42
Cu 12
Rb 29
Y 8
Zr 209
Nb 13
Average chemical composition of 4 samples (Kerrich, 1983)
%
SiO2 65.83
TiO2 0.5
Al2O3 15.16
Fe2O3 3.17
MgO 1.16
CaO 2.91
K2O 1.41
Na2O 7.07
P2O3 0.2
ppm
Au 0.16
Cr 29
Ni 15
Sr 1108
Ba 1372
Zn 42
Cu 12
Rb 29
Y 8
Zr 209
Nb 13
Wednesday, 17 August 2011
Tuesday, 16 August 2011
Monday, 15 August 2011
Tuesday, 9 August 2011
Drillhole CON- 8, Contact Lake, 1981
SUMMARY
0 - 183.4 m : fresh conglomerate
U at 117m : 134 & 164 cps
183.4 - 258.0 : Altered conglomerate
U at 189.1 : 100 cps
U at 192.7 : 120 cps
U at 193.2 : 80 - 130 cps
U at 200.5 : 150 cps
U at 235.1 : 140 cps
U at 236.4 : 100 cps
U at 236.7 : 130 cps
258.0 - 295.0 : fresh conglomerate
295 - 401.5 : Altered conglomerate
U at 330.5 : 146 cps
U at 358.1 : 120 cps
Au at 385.0 : 22.3 g/t
401.5 m : end of hole
apparently, the Unconformity was not more than 10 m away...
Samples for radiometric dating by Scintrex : 1,200 m.y.
0 - 183.4 m : fresh conglomerate
U at 117m : 134 & 164 cps
183.4 - 258.0 : Altered conglomerate
U at 189.1 : 100 cps
U at 192.7 : 120 cps
U at 193.2 : 80 - 130 cps
U at 200.5 : 150 cps
U at 235.1 : 140 cps
U at 236.4 : 100 cps
U at 236.7 : 130 cps
258.0 - 295.0 : fresh conglomerate
295 - 401.5 : Altered conglomerate
U at 330.5 : 146 cps
U at 358.1 : 120 cps
Au at 385.0 : 22.3 g/t
401.5 m : end of hole
apparently, the Unconformity was not more than 10 m away...
Samples for radiometric dating by Scintrex : 1,200 m.y.
Cutler Lake Uranium
Formerly known as Contact lake, Uranium City area, Sask.
Thin comb quartz veins with occasional pitchblende
Rock is altered by hematite & silica
Fresh lower Martin Group conglomerate
Gypsumville 4 km meteor effects
SURFACE EXPOSURES
Three exposures of fractured limestone just outside crater rim
breccia
boulder of explosive breccia
Photomicrographs
breccia
meltrock
meltrock
UMBRELLA TEXTURE
Boulders with rounded top
upside down of "umbrella" texture with
white clay in concave cavity
Another boulder with rounded top and concave directly underneath
"Expulsion cavities" in dolomite: probably formed by carbon dioxide
gas exploding like a missile inside the rock
probable shatter cones in dolomite
Definite shatter cones in dolomite
Monday, 8 August 2011
East Malartic Porphyry Swarm ore
lots of quartz veining
visible gold circled
several generations of quartz veins
yellow line separates porphyry on bottom from
sheared basalt above.
Note that quartz does not continue into basalt
East Malartic chert gold
chert below painted line. Dip at 55 degrees
chert above painted line
white quartz pods in chert
Average chemical composition of 22 samples (Kerrich, 1983)
%
SiO2 64.87
TiO2 0.4
Al2O3 12.55
Fe2O3 4.5
MgO 2.32
CaO 3.47
K2O 3.91
Na2O 3.95
P2O5 0.13
ppm
Au 12.88
Cr 157
Ni 66
Sr 656
Ba 605
Zn 37
Cu 20
Rb 67
Y 12
Zr 117
Nb 17
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