KAT Exploration Inc (KATX)

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.Q: Does Kat have proven Copper.....see for your self................. I believe that Kat has a sr Geo who is, and has been working on a resource est. on Kats Cabbot for the last 5-6 months. ........Has much more work been done on the Cabot property rhan previously known?....I do believe so!.....over 400.000 work has been done in 1990's dollars



















look what i did all night
http://gis.geosurv.gov.nl.ca/geofilePDFS/Batch12/012I_0250.pdf
//////////////p26///////////////////////////////////////////////////////////////////////////Anomaly No. 2 is located in the northern portion of the grid, between Lines 43+00N and 48+00N and
from approximately 39+00E to 43+00E. The anomaly consists of copper values ranging between 51
ppm and 173 ppm. A large Pulse EM anomaly underlies this soil anomaly and has been correlated with
a strike extensive graphitic schist horizon. In addition, another significant Pulse EM anomaly occurs
immediately to the west of the soil anomaly.///////////////////p26//////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////Anomaly No. 1 occurs in the southern end of the soil grid between lines 32+00N and 34+00N extending
from 42+00E to 44+00E. The anomaly consists of copper values between 51 and 540 ppm. It is felt
that this anomaly is a result of the eastward glacial dispersion of material from the Cabot Zone located
several hundred meters to the west. Numerous copper mineralized float have been identified in the
vicinity of this soil anomaly which appear to resemble the Cabot Zone style of mineralization. This
anomaly may continue further to the southwest, beyond the limit of the 1998 soil survey.///////////////////////////////////////////////////////////////////////////////////////////All nine (9) holes drilled in the 1998 program were successful in intersecting the Cabot Mineralized
Zone. Excluding the narrow intersection encountered in Hole No. CAB-98-11 (0.38% Cu over 1.60m)
and the multiple zones intersected in holes CAB-98-07 & 08, the zone averaged 0.39% Cu and 0.015%
Co over 21.6 meters. The best grade intersections over a significant width occurred in hole No.’s CAB-
98-07 and CAB-98-08 where respectively 1.90% Cu over 2.78 meters and 1.33% Cu over 3.60 meters
were obtained. Table No. 3 summarizes the grade and width intersections for each drill hole, as well as
showing both the Cu and Cu+Co-Cu equivalent grades. The Cu+Co-Cu equivalent value is based on the
price of Cu at 0.7475 $ US/pound and the price of Co at 21.00 $ US/pound. These prices were
established on June 12th , 1998 (London Spot prices).////////////////////p37///////////////////////////////////////////////////////////////// Based on diamond drill hole data and surficial mapping, the Cabot Mineralized Zone consists of a
discrete intensely choritized stringer/stockwork sulfide zone. The sulfides consists of disseminated and
stringer chalcopyrite, pyrrhotite and locally minor sphalerite. Pyrite is also locally abundant throughout
the zone and occurs predominantly as subhedral to euhedral grains, 2-10mm’s in size.///////////////////////////////////////////////////////////////////////////////////////////////////p41////////////////////////////////////////////////////////////// The magnetite content generally ranges from 10% to 70%. In localized areas
within the zone it is non-existent and the zone is dominated by intense chloritic alteration. As with the
mineralized zone, the iron formation generally exhibits sharp contacts with the host rocks. The zone was
intersected in six (6) out of the nine (9) holes drilled and occurred at a range of 3.3 meters to 57.8 meters
above the mineralized zone. The zone thickness ranged from 5.0 to 18.25 meters, with an average
thickness calculated at 7.0 meters.
The....//////////////////////////////////////////////////////////////////////////////////////////////////p42//////////////////////////////////////////////////////////////////////..... The Cabot Zone to date as been drill tested to a vertical depth of 430 meters and for a horizontal distance
of 350 meters. All holes were successful in intersecting the zone, and it has been inferred from surficial
mapping and drill hole data that the zone has a northeast plunge. Little is known to date on the angle
of this NE plunge and the zone still remains open at depth and along strike. The Cabot Zone has been......interpreted to be a feeder zone characteristic of those associated with volcanogenic massive sulfide
deposits............ ////////////////////////////////////////////////////////////////////////////////////////////////////////////p34/////////////////////////////////////////////////////////////////...below the stripped area. Hole No. CAB-97-01 intersected 0.38% Cu over 22.6 meters at a vertical
depth of 51.0 meters and Hole No. CAB-97-02 intersected 0.35% Cu over 22.0 meters at a vertical depth
of 18.0 meters.
During the period of June 01 to July 29, 1998 Noveder Inc. conducted a nine (9) hole diamond drilling
program consisting of 2382.1 meters of BQ core drilling (Figure No. 4). All of the holes were drilled
on the Cabot Zone and tested its vertical projection to depths ranging from 54 meters to 430 meters.
The drill program was largely guided by the geophysical results obtained from the winter 1998 program
and observations and location of the Cabot Zone at surface.///////////////////////////////////////////////////////////////////////////////////// other most intresting conclusions on pages 290 291 289 285 286 287 288 ////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////////// ... gis.geosurv.gov.nl.ca/geofilePDFS/Batch12/012I_0250.pdf
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