Cream Minerals Ltd. (TSX-V ?CMA?) (?Cream?) is pleased to
report that its first test hole, RAD 07 ? 01, on its Wine ? Radar Lake
property, 60 km southeast of Flin Flon, Manitoba, assayed 1.30% Nickel,
2.27% Copper, 0.319 g/t Gold, 0.132% Platinum and 0.270 g/t Palladium over
66.8 feet core length at a dip of????
?49 degrees (true width is estimated to be 43.6 feet).??
The hole was drilled to test and confirm an earlier
hole DDH EEL ? 346, drilled in 1987 by Hudson Bay Exploration and Development
Co. Ltd., which assayed 0.85% Nickel and 1.42% Copper over 54.0 feet at a dip
of ?45 degrees (Refer to Cream News Release dated February 6, 2006).? Assays over the mineralized section of the
RAD 07-01 drill hole are tabled below:?
Assay Results for RAD 07-01:
Sample
#
|
From
(Ft)
|
To
(Ft)
|
Width
(Ft)
|
Au
(ppb)
|
Cu
(%)
|
Ni
(%)
|
Pt
(ppb)
|
Pd
(ppb)
|
860603
|
182.6
|
184.8
|
2.2
|
80
|
0.41
|
0.42
|
0
|
65
|
860604
|
184.8
|
186.4
|
1.6
|
80
|
0.13
|
0.08
|
30
|
70
|
860605
|
186.4
|
189.4
|
3.0
|
110
|
0.40
|
1.01
|
45
|
250
|
860606
|
189.4
|
192.2
|
2.8
|
50
|
0.65
|
1.25
|
25
|
55
|
860607
|
192.2
|
193.9
|
1.7
|
890
|
2.89
|
0.00
|
40
|
55
|
860608
|
193.9
|
195.0
|
1.1
|
1750
|
18.10
|
0.52
|
60
|
150
|
860609
|
195.0
|
198.3
|
3.3
|
390
|
0.62
|
1.62
|
130
|
180
|
860610
|
198.3
|
200.9
|
2.6
|
150
|
2.68
|
1.92
|
35
|
330
|
860611
|
200.9
|
203.7
|
2.8
|
30
|
0.33
|
2.48
|
45
|
530
|
860612
|
203.7
|
207.0
|
3.3
|
280
|
3.48
|
1.73
|
350
|
510
|
860613
|
207.0
|
209.0
|
2.0
|
70
|
0.72
|
2.67
|
510
|
250
|
860614
|
209.0
|
212.6
|
3.6
|
390
|
7.76
|
1.44
|
270
|
570
|
860615
|
212.6
|
213.9
|
1.3
|
70
|
0.18
|
0.13
|
20
|
40
|
860616
|
213.9
|
215.6
|
1.7
|
1170
|
3.02
|
0.35
|
340
|
230
|
860617
|
215.6
|
217.3
|
1.7
|
40
|
0.16
|
0.03
|
20
|
10
|
860618
|
217.3
|
220.5
|
3.2
|
150
|
1.99
|
1.46
|
60
|
320
|
860619
|
220.5
|
224.7
|
4.2
|
30
|
0.05
|
0.11
|
15
|
10
|
860620
|
224.7
|
227.0
|
2.3
|
240
|
5.60
|
1.25
|
210
|
150
|
860621
|
227.0
|
230.1
|
3.1
|
560
|
3.77
|
1.46
|
45
|
180
|
860622
|
230.1
|
233.7
|
3.6
|
65
|
1.39
|
1.36
|
110
|
120
|
860623
|
233.7
|
237.0
|
3.3
|
1610
|
1.33
|
2.07
|
260
|
250
|
860624
|
237.0
|
240.1
|
3.1
|
110
|
1.27
|
2.28
|
270
|
400
|
860625
|
240.1
|
242.9
|
2.8
|
230
|
3.25
|
2.24
|
330
|
710
|
860626
|
242.9
|
246.2
|
3.3
|
55
|
0.20
|
0.15
|
15
|
35
|
860627
|
246.2
|
249.4
|
3.2
|
340
|
3.72
|
2.04
|
20
|
760
|
TOTAL
|
182.6
|
249.4
|
66.8
|
319
|
2.27
|
1.30
|
132
|
270
|
RAD 07 ? 01 Drill Logs:
From
(Ft)
|
To
(Ft)
|
Lithological
Description
|
Sample
#
|
From
(Ft)
|
To
(Ft)
|
Width
(Ft)
|
164.50
|
265.00
|
RHYOLITE
|
|
|
|
|
|
|
Light
gray, fine-grained, weakly foliated.?
Mineralized 182.6? to 249.4? disseminated to near solid sulphide pyrrhotite and
chalcopyrite? (184.8 ? 186.4 ?
gabbro)
|
|
|
|
|
|
|
|
|
|
1% chalcopyrite, 90% pyrite
|
860602
|
172.5
|
173.3
|
0.8
|
|
|
|
|
|
|
|
|
|
1% chalcopyrite, 10% pyrrhotite
|
860603
|
182.6
|
184.8
|
2.2
|
|
|
2% chalcopyrite??????????????????????????
|
860604
|
184.8
|
186.4
|
1.6
|
|
|
2% chalcopyrite, 20% pyrrhotite
|
860605
|
186.4
|
189.4
|
3.0
|
|
|
2% chalcopyrite, 10% pyrrhotite
|
860606
|
189.4
|
192.2
|
2.8
|
|
|
8% chalcopyrite, 10% pyrrhotite
|
860607
|
192.2
|
193.9
|
1.7
|
|
|
60% chalcopyrite, 5% pyrrhotite
|
860608
|
193.9
|
195.0
|
1.1
|
|
|
1% chalcopyrite, 25% pyrrhotite
|
860609
|
195.0
|
198.3
|
3.3
|
|
|
6% chalcopyrite, 50% pyrrhotite
|
860610
|
198.3
|
200.9
|
2.6
|
|
|
1% chalcopyrite, 80% pyrrhotite
|
860611
|
200.9
|
203.7
|
2.8
|
|
|
8% chalcopyrite, 25% pyrrhotite
|
860612
|
203.7
|
207.0
|
3.3
|
|
|
5% chalcopyrite, 75% pyrrhotite
|
860613
|
207.0
|
209.0
|
2.0
|
|
|
25% chalcopyrite, 25% pyrrhotite
|
860614
|
209.0
|
212.6
|
3.6
|
|
|
1% chalcopyrite, 1% pyrrhotite
|
860615
|
212.6
|
213.9
|
1.3
|
|
|
6% chalcopyrite, 4% pyrrhotite
|
860616
|
213.9
|
215.6
|
1.7
|
|
|
tr chalcopyrite, tr pyrrhotite
|
860617
|
215.6
|
217.3
|
1.7
|
|
|
5% chalcopyrite, 15% pyrrhotite
|
860618
|
217.3
|
220.5
|
3.2
|
|
|
tr chalcopyrite, tr pyrrhotite
|
860619
|
220.5
|
224.7
|
4.2
|
|
|
6% chalcopyrite, 6% pyrrhotite
|
860620
|
224.7
|
227.0
|
2.3
|
|
|
6% chalcopyrite, 6% pyrrhotite
|
860621
|
227.0
|
230.1
|
3.1
|
|
|
5% chalcopyrite, 15% pyrrhotite
|
860622
|
230.1
|
233.7
|
3.6
|
|
|
5% chalcopyrite, 20% pyrrhotite
|
860623
|
233.7
|
237.0
|
3.3
|
|
|
10% chalcopyrite, 60% pyrrhotite
|
860624
|
237.0
|
240.1
|
3.1
|
|
|
10% chalcopyrite, 80% pyrrhotite
|
860625
|
240.1
|
242.9
|
2.8
|
|
|
1% chalcopyrite, 5% pyrrhotite
|
860626
|
242.9
|
246.2
|
3.3
|
|
|
10% chalcopyrite, 40% pyrrhotite
|
860627
|
246.2
|
249.4
|
3.2
|
|
|
|
|
|
|
66.8
|
In a report received from Mr.
Anthony J. Spooner, P.Eng., of A. J. Spooner Exploration Services Inc., Flin
Flon, MB, Qualified Person for NI 43-101, who is managing the drilling
program on the Wine Property, Mr. Spooner stated:? ?This is certainly worth chasing some more.? I hope borehole geophysics will show us
the way?.??
A second drill hole, RAD 07 ? 02 was collared at
approximately 230 feet southeast of RAD 07 ? 01.? It was drilled at ?60 degrees to a depth of 837 feet with the
hope of intersecting mineralization should the zone plunge vertically to that
point.? The favourable horizon was not
intersected in this hole; however, the main purpose of the hole was to locate
the downward plunge of the upper zone and the hole will now be used for a
down the hole Pulse EM Survey as soon as possible in order to locate the
mineralized body.?
During the drill
program, standard sampling procedures were used whereby the core was cut with
a circular diamond saw and half of the core was sent by trucking company
directly to TSL Laboratories Ltd. in Saskatoon, Saskatchewan.? The remaining half of the core was stored
in a core storage facility in Snow Lake, Manitoba.? All sample preparation was done at the laboratory by TSL staff,
who assayed the samples using a multi-acid digestion and Atomic Absorption
assay procedures.
For more information, including
about Cream and its mineral property interests, please visit Cream?s website
? www.creamminerals.com.
|