New drill results include:
B5MB4D059 - 10.19 metres @ 6.69% Cu, 0.48 g/t
Au, 3.2% Zn & 20 g/t Ag from 33.5 metres in supergene massive
sulphides
B5MB4D066 - 4.90 metres @ 15.94% Cu, 1.27 g/t Au & 49.4
g/t Ag from 19.3 metres.
B5MB4D074 - 35.09 metres @ 4.82% Cu, 0.38 g/t Au, 0.85% Zn
& 17.7 g/t Ag from 70.35 metres down hole in a
primary massive sulphide intersection
TORONTO,
Nov. 14, 2011 /PRNewswire/ - Gentor
Resources, Inc. ("Gentor" or the "Company") (TSX-V: GNT) &
(OTCQB: GNTO) and their Omani partner Al Fairuz Mining Company LLC
are pleased to announce continued excellent results from on-going
evaluation drilling of their Oman Block 5, Mahab 4 Cyprus-type
copper discovery. Further diamond drilling has confirmed continuity
of strong Massive Sulphide grades over 300 metres of strike,
including high-grade supergene zones below gossan exposures at the
southern end of the deposit.
These continued impressive results from infill
and extensional resource drilling by two diamond rigs at Mahab 4
are expected to allow the calculation of a maiden resource estimate
on this high grade deposit by early 2012. By the end of
October 2011, Gentor had completed 43
drillholes totalling 5,075.4 metres at Mahab 4. A recent
Laser scan DTM survey has provided accurate topographic and drill
hole collar information (see Table 2 below).
Assay results received from twelve new drill
holes up to B5MB4D074 are summarised in Table 1 below and the
drillhole intersections shown in the prospect geology plan (see
Figure 1 via the link below to Gentor's website). An additional
nine successful holes have been completed whose assay results are
awaited, and at least six more holes are planned to complete
definition of the main ore deposit shape on 50 metre sections down
to a nominal 150 metres depth below surface.
Gentor has initiated preliminary metallurgical
test work on ten representative samples of Massive Sulphide and
Stringer Zone samples from Mahab 4 at Wardell Armstrong's UK
laboratory.
Gentor plans to restart drill evaluation of the
Maqail South discovery in December
2011 following completion of this phase of the Mahab 4 drill
programme. Regional exploration continues across Blocks 5
& 6 in Oman with a reverse
circulation drilling program of some 3,000 metres planned for
November/December 2011.
Locality plans of the Oman concessions, the key prospect areas and
reported drill holes on sections are found accompanying this press
release on the Company's web site:
http://www.gentorresources.com/s/NewsReleases.asp?ReportID=490430
Gentor's President & CEO Dr. Peter Ruxton commented: "Understanding the
geological model and structural controls has allowed Gentor to
efficiently target the high-grade massive sulphide shoots at Mahab
4 and has outlined this deposit for planned early resource
definition and metallurgical testing. The shallow depth of the
Mahab 4 mineralisation suggests future potential for a
near-surface, high grade, open pittable ore body."
Results from the main massive sulphide
intercepts include:
- GRB5D047 intersecting 24.4 metres of primary MS /SMS
grading 4.68% Cu, 0.21 g/t Au, 1.68% Zn and 13.8 g/t Ag from 96.6
metres,
- B5MB4D059 intersecting 10.19 metres of supergene MS
grading 6.69% Cu, 0.48 g/t Au, 3.2% Zn and 20 g/t Ag from 33.5
metres,
- B5MB4D064 intersecting 39.5 metres of gossan/MS/SMS
grading 4.81% Cu, 0.25 g/t Au, 0.38% Zn and 16.7 g/t Ag from 13.5
metres down hole, including 16.85 metres grading 8.4% Cu, 0.25 g/t
Au, 0.52% Zn and 15.3 g/t Ag from 20.15 metres depth.
- B5MB4D066 intersecting 22.7 metres of gossan/MS/SMS
grading 3.76% Cu, 0.54 g/t Au, 0.09% Zn and 15.4 g/t Ag from 1.5
metres depth including 4.9 metres grading 15.94% Cu, 1.27 g/t Au,
0.11% Zn and 49.4 g/t Ag from 19.3 metres down hole.
- B5MB4D074 intersecting 35.09 metres of primary MS grading
4.82% Cu, 0.38 g/t Au, 0.85% Zn and 17.7 g/t Ag from 70.35 metres
down hole.
TABLE 1. Summary of Significant Intersections at Mahab
4 from June - Oct. 2011.
Hole # |
From |
To |
Intercept |
Copper |
Gold |
Silver |
Zinc |
Mineralisation |
Mahab 4 |
m |
m |
m |
% |
g/t |
g/t |
% |
|
GRB5D042 |
108.20 |
111.00 |
2.80 |
5.03 |
0.17 |
17.7 |
1.29 |
MS |
and |
119.70 |
129.90 |
10.20 |
5.25 |
0.30 |
13.8 |
1.02 |
MS |
GRB5D047 |
96.60 |
121.00 |
24.40 |
4.68 |
0.21 |
13.8 |
1.68 |
MS/SMS |
incl: |
98.75 |
116.39 |
17.64 |
6.14 |
0.26 |
18.6 |
2.24 |
MS/SMS |
incl: |
103.00 |
112.00 |
9.00 |
7.22 |
0.25 |
15.8 |
1.93 |
MS/SMS |
GRB5D048 |
57.20 |
65.00 |
7.80 |
1.24 |
0.08 |
2.1 |
0.18 |
QVS |
and |
93.00 |
103.00 |
10.00 |
1.54 |
0.07 |
1.4 |
0.18 |
QVS |
and |
113.89 |
129.00 |
15.11 |
0.49 |
0.02 |
1.1 |
0.04 |
QVS |
GRB5D052 |
90.54 |
106.89 |
16.35 |
0.72 |
0.05 |
1.4 |
0.13 |
QVS |
incl: |
90.54 |
93.88 |
3.34 |
1.18 |
0.04 |
1.3 |
0.07 |
QVS |
and incl: |
102.00 |
109.00 |
7.00 |
0.73 |
0.06 |
2.2 |
0.21 |
QVS |
GRB5D054 |
62.40 |
73.00 |
10.60 |
0.43 |
0.03 |
0.5 |
0.04 |
QVS/SMS |
incl: |
67.89 |
73.00 |
5.11 |
0.72 |
0.04 |
0.8 |
0.05 |
QVS/SMS |
B5MB4D057 |
104.15 |
107.00 |
2.85 |
0.44 |
0.04 |
5.4 |
0.14 |
QVS |
B5MB4D059 |
33.50 |
43.69 |
10.19 |
6.69 |
0.48 |
20.0 |
3.20 |
MS |
B5MB4D064 |
13.50 |
53.00 |
39.50 |
4.81 |
0.25 |
16.7 |
0.38 |
GOS/MS/SMS |
incl: |
20.15 |
37.00 |
16.85 |
8.40 |
0.25 |
15.3 |
0.52 |
MS |
B5MB4D066 |
1.50 |
24.20 |
22.70 |
3.76 |
0.54 |
15.4 |
0.09 |
GOS/MS |
incl: |
19.30 |
24.20 |
4.90 |
15.94 |
1.27 |
49.4 |
0.11 |
MS |
B5MB4D067 |
32.95 |
41.00 |
8.05 |
3.18 |
0.53 |
24.0 |
0.39 |
MS |
incl: |
33.90 |
38.70 |
4.80 |
4.59 |
0.81 |
36.3 |
0.31 |
MS |
B5MB4D074 |
70.35 |
105.44 |
35.09 |
4.82 |
0.38 |
17.7 |
0.85 |
MS |
incl: |
72.84 |
95.41 |
22.57 |
6.14 |
0.38 |
20.9 |
1.08 |
MS |
and incl: |
99.25 |
105.44 |
6.19 |
4.01 |
0.72 |
21.6 |
0.67 |
MS |
(Codes: MS = Massive Sulphide, SMS = Semi-Massive Sulphide, QVS
= Quartz Vein Stringer, GOS = Gossan)
TABLE 2. Core holes completed at Mahab 4 (June to
Oct. 2011)
Hole No |
Section |
Easting |
Northing |
Dip |
Azi |
Length
(m) |
GRB5D048 |
0 |
468775 |
2656105 |
60 |
255 |
135.15 |
GRB5D050 |
0 |
468808 |
2656115 |
60 |
255 |
145.85 |
GRB5D052 |
0 |
468677 |
2656063 |
50 |
060 |
117.40 |
GRB5D054 |
1S |
468714 |
2656035 |
50 |
075 |
84.05 |
GRB5D055 |
2S |
468734 |
2655999 |
50 |
075 |
96.00 |
B5MB4D057 |
1S |
468674 |
2656025 |
50 |
075 |
115.50 |
B5MB4D059 |
1S |
468741 |
2656040 |
49 |
065 |
55.10 |
B5MB4D061 |
2S |
468754 |
2656009 |
50 |
075 |
49.30 |
B5MB4D063 |
1S |
468795 |
2656058 |
90 |
0 |
46.50 |
B5MB4D064 |
1 |
468760 |
2656139 |
60 |
255 |
77.00 |
B5MB4D066 |
0 |
468767 |
2656104 |
60 |
255 |
64.85 |
B5MB4D067 |
0 |
468780 |
2656104 |
45 |
252 |
85.50 |
B5MB4D069 |
1.5S |
468748 |
2656024 |
50 |
075 |
52.50 |
B5MB4D070 |
1S |
468771 |
2656049 |
75 |
255 |
85.30 |
B5MB4D071 |
4.5 |
468762 |
2656316 |
60 |
255 |
141.50 |
B5MB4D072 |
1 |
468656 |
2656103 |
50 |
072 |
132.45 |
B5MB4D074 |
4.5 |
468761 |
2656314 |
60 |
277 |
126.00 |
B5MB4D075 |
2 |
468708 |
2656181 |
75 |
075 |
55.10 |
B5MB4D077 |
5.5 |
468758 |
2656362 |
60 |
255 |
79.30 |
B5MB4D079 |
2 |
468678 |
2656168 |
64 |
075 |
130.35 |
B5MB4D080 |
6 |
468752 |
2656387 |
60 |
255 |
154.60 |
B5MB4D082 |
3 |
468701 |
2656218 |
72 |
075 |
123.70 |
B5MB4D083 |
3.5 |
468763 |
2656265 |
60 |
255 |
105.20 |
DRILL RESULTS
The northern end of the deposit is discussed
first on a sectional basis followed by the southern end and central
sectional drill results (refer to Figures 1 to 6 via the above link
to Gentor's website for interpretative details).
Section 4 --GRB5D042 and GRB5D047 tested
the lateral extent of the GRB5D035 major intersection shown
in Figure 3 and previously reported in July
2011.
GRB5D042 a scissor hole from the west
intersected the Main Fault then 2.80 metres of MS grading 5.03%
Cu, 0.17 g/t Au, 1.29% Zn and 17.7 g/t Ag from 108.20 metres
and 10.20 metres of MS grading 5.25% Cu, 0.30 g/t Au, 1.02% Zn
and 13.8 g/t Ag from 119.70 metres. These zones define a narrow
width to the MS at this level.
GRB5D047 intersected 24.40 metres of
MS/SMS grading 4.68% Cu, 0.21 g/t Au, 1.68% Zn and 13.8 g/t Ag from
96.60 metres and includes 9.00 metres grading 7.22% Cu, 0.25
g/t Au, 1.93% Zn and 15.8 g/t Ag from 103.00 metres. This
confirms the high grade zone in GRB5D035 extends at depth
down dip to the east but it is cut off by an eastern fault (see
Figure 3).
Section 4.5 -- B5MB4D071 and
B5MB4D074 effectively extended the strike extent of the MS
north into Section 5 where GRB5D041 and GRB5D045 had previously
failed to intersect the deposit.
B5MB4D071 drilled parallel and 25 metres
north of GRB5D035 provided an excellent result of a similar
very strongly mineralised zone of MS, SMS and QVS from 63-128
metres including 45 metres of chalcopyrite-rich MS down to 108
metres for which final assays are not yet available. This
encouraging result showed the deposit remained open to the north -
so a second drill hole GRB5D074 from the same site was
angled towards Section 5.
B5MB4D074 also provided a strong
primary massive sulphide intersection of 35.09 metres grading
4.82% Cu, 0.38 g/t Au, 0.85% Zn and 17.7/t Ag from 70.35 metres
down hole ended at 105.44 metres with a sharp conformable
transition to strongly altered footwall V1-1 lavas. The latter part
of this intersection lies beneath the barren intersection in
GRB5D041 on Section 5 and shows the deposit is open at
depth.
Sections 5.5 and 6-- B5MB4D077 and
B5MB4D080 further tested the northern strike extension of the
deposit.
B5MB4D077 collared 50 metres north of
B5MB4D074 on Section 5.5 intersected 30cm of pyritic MS from
70.4 metres below a thin magnetite rich umber and then sedimentary
breccias above V1-1 footwall lavas. This result suggests a
distal exhalative position and indicates the deposit has thinned
rapidly to the north from B5MB4D074, or there may be some
cross structural control at the northern end of the deposit.
B5MB4D080 was collared 25 metres north of
D077 on Section 6 looking for any northern extension, but failed to
intersect a mineralised seafloor position with only thin umbers
between 85.80 metres and 90.10 metres and jasper clasts at 103
metres. This hole implies the deposit may have terminated just
north of the D077 position.
Section 2S and 1.5S -- B5MB4D055,
B5MB4D061 and B5MB4D069 tested the southern strike extensions
of the deposit located on Section 1 in the southern wadi.
All of these holes failed to intersect the Main
Fault or the mineralised package containing the Mahab 4 deposit,
therefore it is concluded that an east-east cross fault parallel to
the sections as shown in Figure 2 has cut off the deposit and may
have displaced it at depth to the east.
Section 1S - BGRB5D054, B5MB4D057,
B5MB4D059, B5MB4D063 and B5MB4D070 defined the southern strike
extent of the deposit in the southern wadi (see Figure 6).
Initial drillholes B5MB4D054 and
B5MB4D057 testing the QVS part of the system intersected
moderate to low grade copper including 10.6 metres of
QVS/SMS grading 0.43% Cu, 0.03 g/t Au from 60.4 metres in
B5MB4D054 and 2.85 metres at 0.44% Cu, 0.04 g/t Au from 104.15
metres in B5MB4D057 that is interpreted be close to the bottom
of the deposit.
However, overlying this weak mineralisation,
drillhole B5MB4D059 intersected 10.19 metres of supergene MS
grading 6.69% Cu, 0.48 g/t Au, 3.2% Zn and 20 g/t Ag from 33.5
metres adjacent to the Main Fault zone and ending at an eastern
fault (see Figure 4). This high-grade intersection represented a
break through in the evaluation of the southern end of the deposit,
because it showed that good MS can be found at shallow depth
beneath mapped gossan and above weak QVS stringer mineralisation at
depth.
B5MB4D063 designed to test any eastern
down-dip/stratigraphic extension of the B5MB4D059 MS failed
to intersect sulphide mineralisation at depth in footwall V1-1
lavas, but did hit shallow oxidised copper from 13-16 metres in
basalt indicating leakage from subsurface gossan exposure
upstream.
B5MB4D070 was designed to provide a full
intersection of the oxide-supergene MS-primary MS-QVS transitions
on Section 1S primarily for metallurgical purposes. It achieved an
excellent result with mineralisation virtually from the surface
including 6.5 metres of ferruginous gossan below wadi gravel
from 7 metres depth, a 6 metre thick zone of chalcocite
supergene enriched MS from 12.45 metres above a primary MS zone to
36.1 metres. Assay results from this zone are awaited.
Section 0 -- BGRB5D048, BGRB5D052,
B5MB4D066 and B5MB4D067 clearly defined the limits to the
deposit on this section shown in Figure 5.
GRB5D048 collared 10 metres east of the
Main Fault intersected three separate intervals of copper bearing
sub seafloor QVS mineralisation including:
7.80 metres grading 1.24% Cu, 0.08 g/t Au,
0.18% Zn and 2.1 g/t Ag from 57.20 metres,
10.00 metres grading 1.54% Cu, 0.07 g/t Au,
0.18% Zn and 1.4 g/t Ag from 93.00 metres, and
15.11 metres grading 0.49% Cu, 0.02 g/t Au,
0.04% Zn and 1.1 g/t Ag from 113.89 metres.
GRB5D052 drilled from the western
footwall intersected a 16.35 metre near true thickness zone
of QVS mineralisation from 90.54 metres which grades
0.72% Cu, 0.05 g/t Au, 0.13% Zn and 1.4 g/t Ag and includes
3.34 metres of 1.18% Cu, 0.04 g/t Au, 0.07% Zn and 1.3 g/t
Ag.
B5MB4D066 was sited 5 metres west of hole
GRB5D048 to test for MS below surficial gossan and it
intersected the mineralised sequence from Fe and Cu oxidised
hanging wall basalts to 12.5 metres then gossan to 20 metres depth
above supergene enriched MS and SMS with high grade chalcocite +
covellite down to 24 metres where the mineralised interval was
faulted out by a core parallel structure.
Assay results gave 22.7 metres
of GOS/MS/SMS grading 3.76% Cu, 0.54 g/t Au, 0.09% Zn and 15.4 g/t
Ag from 1.5 metres depth including 4.9 metres grading 15.94% Cu,
1.27 g/t Au, 0.11% Zn and 49.4 g/t Ag from 19.3 metres down hole in
the supergene zone.
B5MB4D067 was sited 10 metres to the
east of B5MB4D066 in order to provide a better idea of the
width of the MS mineralised zone and positions of the faulted
contacts. The hole successfully intersected a fault on the east
side of the mineralised zone at 28 metres and primary MS with minor
supergene enrichment to 38.65 metres then haematitic sediment to
39.25 metres above a fault into footwall basalts at 39.7 metres.
Assay results across this zone include 8.05 metres of MS grading
3.18% Cu, 0.53 g/t Au, 0.39% Zn and 24 g/t Ag from 32.95
metres.
It appears that the mineralised zones on this
section are of reasonable grade but are thinner than expected due
to considerable faulting and dyke intrusions.
Section 1 -- B5MB4D064 and B5MB4D072
tested near surface extensions of the MS as shown in Figure 4.
B5MB4D064 was designed to test for
MS below surficial gossan exposed in a trench between
drillholes D005 and D006. B5MB4D064 successfully
intersected clay-rich to haematitic gossan and jasper from 12.5
metres -20.15 metres above supergene MS to 27.5 metres then primary
chalcopyrite-rich MS to 36.8 metres grading to SMS down to 51
metres above footwall QVS to 60 metres where the Main Fault
terminated mineralisation.
This impressive intersection totalling 39.5
metres of GOS/MS/SMS in B5MB4D064 grades 4.81% Cu, 0.25 g/t
Au, 0.38% Zn and 16.7 g/t Ag from 13.5 metres down hole, including
16.85 metres grading 8.4% Cu, 0.25 g/t Au, 0.52% Zn and 15.3 g/t Ag
from 20.15 metres depth.
B5MB4D072 was a scissor hole designed to
better constrain the shape and grade of QVS below the strong MS in
B5MB4D064 and above the well mineralised GRB5D005
intersection. Unfortunately the hole intersected a
series of unmineralised structures and late dykes between ~97
metres and ~105 metres and then QVS between down to 107.34 metres
where it terminated on a cross fault. Assays are awaited but this
result minimises the effective width of the deposit on this section
as shown in Figure 4.
Section 2 -- B5MB4D075 and B5MB4D079
tested intermediate depth extensions of the MS and QVS.
B5MB4D075 was stopped at 122.10 metres
having intersected 5.7 metres of MS at 91.63 metres close to
where the hole crosses drillhole D020. It also intersected several
fault zones and breccias some of which contain minor QVS
mineralization and assays are awaited for this hole.
B5MB4D079 was stepped back to the west to
intersect the QVS zone at about 100 metres depth well below that of
hole B5MB4D075. B5MB4D079 intersected over 30 metres
of moderate QVS mineralisation from 95.25 to the end of the hole at
125.30 metres where the QVS grades into brecciated basalts with
only minor pyrite stringers. Assays are awaited for this hole.
Section 3 -- B5MB4D082 and B5MB4D086
targeted the QVS zone at 50-100 metres depth.
B5MB4D082 was set up at the same collar
site as GRB5D032 but drilled a steeper hole with the aim of
intersecting QVS mineralisation beneath the MS encountered in hole
D030. B5MB4D082 successfully intersected the Main Fault at
81.5 metres then the lowermost part of the MS to 83.6 metres
followed by QVS mineralisation with chalcopyrite down to 119
metres.
B5MB4D086 in progress is a step back hole
designed to test the position of the Main Fault, then the grade and
width of the QVS at 120 metres depth.
Section 3.5 -- B5MB4D083 was an infill
drill hole designed to test the continuity between the 30 metre
thick MS intersection of GRB5D030 and the 50 metre thick MS
of GRB5D035.
B5MB4D083 has confirmed the presence of
high-grade MS from 45.2-65.75 metres, SMS down to 72.4 metres and
16 metres QVS down to 88.5 metres. This good quality mineralised
zone awaiting sampling is slightly thinner than in D030 but appears
to be of equivalent grade on comparative logging.
Summary
Recent drilling has clearly enhanced the deposit
in terms of its size and grade. Although original attributes of the
VMS ore body can be determined, the resultant form is clearly
highly truncated by later faulting - particularly at the deposit's
southern end. In these circumstances true widths of the ore
intersections can be difficult to determine.
The deposit appears broadly constrained to a
northerly trending linear, penecontemporaneous fault and is at
least 300 metres long between Sections 1S to 5N. It comes to
surface on Section 2.5 with a well-developed gold gossan and
supergene enriched massive sulphides and plunges shallowly to the
north as shown in the long section Figure 2. In this figure, the
intersections shown are considered to represent 80-90% of the true
thickness of the deposit.
Infill drilling on five intermediate 25 metre
sections was required to determine ore shapes for ore body
modelling and provide additional core for metallurgical testing of
ore types.
The deposit is potentially open down-plunge at
depth to the north where proposed drilling is underway. To
the south, the body appears to be terminated on a cross fault but
extensions may be possible and will be evaluated by using
geophysics.
Qualified Person
The exploration results disclosed in this press
release have been reviewed, verified (including sampling,
analytical and test data) and compiled by Dr. Peter Ruxton, who is a Member of the Institute
of Materials, Minerals and Mining (I.M.M.M.), the Company's
President and Chief Executive Officer and a "qualified person" (as
such term is defined in Canadian National Instrument 43-101 as
promulgated by the Canadian Securities Administrators).
Technical Report
Additional information with respect to the
Company's Omani properties is contained in the technical report
prepared by Venmyn Rand (Pty) Ltd, dated December 31, 2010 and entitled "National
Instrument 43-101 Independent Technical Report on Block 5 and Block
6 Copper Projects, Semail Ophiolite Belt, Sultanate of Oman held by Gentor Resources, Inc." A
copy of this report can be obtained from SEDAR at
www.sedar.com.
About Gentor
Gentor is a mineral exploration company whose
projects include copper and gold properties in the Sultanate of
Oman and a
molybdenum-tungsten-silver property in East Central Idaho,
U.S. The Company's strategy is to create shareholder value by
developing highly prospective mineral properties around the globe,
with current focus in the Sultanate of Oman. In Oman, Gentor is partnered with Al Fairuz
Mining Company LLC on its Block 5 exploration tenement and Al Zuhra
Mining Company LLC on Block 6.
Cautionary Notes
Forward-Looking Information: This press release
contains forward-looking information. All statements, other than
statements of historical fact, that address activities, events or
developments that the Company believes, expects or anticipates will
or may occur in the future (including, without limitation,
statements regarding drilling and other exploration results,
potential mineral resources, potential mineralization and the
Company's exploration and development plans) are forward-looking
information. This forward-looking information reflects the current
expectations or beliefs of the Company based on information
currently available to the Company. Forward-looking information is
subject to a number of risks and uncertainties that may cause the
actual results of the Company to differ materially from those
discussed in the forward-looking information, and even if such
actual results are realized or substantially realized, there can be
no assurance that they will have the expected consequences to, or
effects on the Company. Factors that could cause actual results or
events to differ materially from current expectations include,
among other things, risks related to the exploration stage of the
Company's properties, the possibility that future exploration
results will not be consistent with the Company's expectations,
changes in world copper or gold markets and equity markets,
political developments in Oman,
uncertainties relating to the availability and costs of financing
needed in the future, the uncertainties involved in interpreting
exploration results and other geological data and the other risks
involved in the mineral exploration business. Forward-looking
information speaks only as of the date on which it is provided and,
except as may be required by applicable securities laws, the
Company disclaims any intent or obligation to update any
forward-looking information, whether as a result of new
information, future events or results or otherwise. Although the
Company believes that the assumptions inherent in the
forward-looking information are reasonable, forward-looking
information is not a guarantee of future performance and
accordingly undue reliance should not be put on such information
due to the inherent uncertainty therein.
The United States Securities and Exchange
Commission (the "SEC") permits mining companies, in their filings
with the SEC, to disclose only those mineral deposits that a
company can economically and legally extract or produce. U.S.
investors are cautioned not to assume that any disclosure of
mineralization contained in this press release is economically or
legally mineable. U.S. investors are urged to closely consider all
of the disclosures in the Company's reports filed pursuant to the
United States Securities Exchange Act of 1934 which may be secured
from the Company, or from the SEC's website at
http://www.sec.gov/edgar.html.
Neither TSX Venture Exchange nor its Regulation
Services Provider (as that term is defined in the policies of the
TSX Venture Exchange) accepts responsibility for the adequacy or
accuracy of this release.
SOURCE Gentor Resources Inc.
Image with caption: "FIGURE 1- Mahab 4 geological plan showing
drill holes, geology and mineralised intervals. (CNW Group/Gentor
Resources Inc.)". Image available at:
http://photos.newswire.ca/images/download/20111114_C5175_PHOTO_EN_6559.jpg
Image with caption: "FIGURE 2- Mahab 4 geological long section
showing drill holes, geological interpretation and mineralised
intervals. (CNW Group/Gentor Resources Inc.)". Image available at:
http://photos.newswire.ca/images/download/20111114_C5175_PHOTO_EN_6560.jpg
Image with caption: "FIGURE 3- Mahab 4, Section 4 with drill
holes, geological interpretation and mineralised intervals. (CNW
Group/Gentor Resources Inc.)". Image available at:
http://photos.newswire.ca/images/download/20111114_C5175_PHOTO_EN_6561.jpg
Image with caption: "FIGURE 4- Mahab 4 Section 1 with drill
holes, geological interpretation and mineralised intervals. (CNW
Group/Gentor Resources Inc.)". Image available at:
http://photos.newswire.ca/images/download/20111114_C5175_PHOTO_EN_6562.jpg
Image with caption: "FIGURE 5- Mahab 4, Section 0 with drill
holes, geological interpretation and mineralised intervals. (CNW
Group/Gentor Resources Inc.)". Image available at:
http://photos.newswire.ca/images/download/20111114_C5175_PHOTO_EN_6563.jpg
Image with caption: "FIGURE 6- Mahab 4, Section 1S with drill
holes, geological interpretation and mineralised intervals. (CNW
Group/Gentor Resources Inc.)". Image available at:
http://photos.newswire.ca/images/download/20111114_C5175_PHOTO_EN_6564.jpg