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Cross Lake Minerals: Sheraton Timmins Project - Wide Zinc Mineralization Intersected.


VANCOUVER, BRITISH COLUMBIA--(BUSINESS WIRE)--July 16, 1998-- Cross Lake Min.(VSE See DOS/VSE.

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.) Cross Lake Minerals Ltd. (the "Company") is pleased to report that 120 metres (394 feet) of 1.03 percent zinc and 11.6 g/t silver, with a true thickness of approximately 100 metres (328 feet), was intersected from 506.0 to 626.0 metres in Hole CLS (Common Language Specification) The structure and syntax of .NET and CLI programming languages. See .NET.  98-59. This hole was recently completed as part of the Company's on-going extensive exploration program on its 100 percent held Sheraton-Timmins Property located near Timmins, Ontario This article is about city in Ontario, Canada. For other uses, see Timmins (disambiguation).
Timmins, with a population of 42,997 (2006), is a city in northeastern Ontario, Canada on the Mattagami River. At 2,961.
. Included in this 120 metre section were higher grade, narrower intervals, which are shown in the table below. This wide zone of sulphide mineralization Mineralization
The process by which the body uses minerals to build bone structure.

Mentioned in: Rickets

mineralization,
n the bioprecipitation of an inorganic substance.
, containing sphalerite sphalerite (sfăl`ərīt, sfā`–), mineral composed of zinc sulfide, usually containing some iron and a little cadmium. It occurs in crystals of the isometric system but more generally in cleavable, compact masses.  (zinc), chalcopyrite (copper) and banded pyrite pyrite (pī`rīt) or iron pyrites (pīrī`tēz, pə–, pī`rīts), pale brass-yellow mineral, the bisulfide of iron, FeS2. , is hosted in felsic fel·sic  
adj.
Containing a group of light-colored silicate minerals that occur in igneous rocks.



[fel(dspar) + s(ilica) + -ic.
 volcanic breccias and tuffs which indicate a favourable setting for volcanogenic vol·ca·no·gen·ic  
adj.
Of volcanic origin.
 massive sulphide (VMS (1) (Virtual Memory System) A multiuser, multitasking, virtual memory operating system for the VAX series from Digital. VMS applications run on any VAX from the MicroVAX to the largest unit. See OpenVMS. ) base metal deposits. This zone is twice the thickness as any previously encountered in the drilling to date.

Hole CLS 98-59 was collared 580 metres south of Hole CLS 97-16 and drilled to a total depth of 671 metres in order to intersect the Cross Lake Zone at depth. The importance of this hole is not only the presence of rhyolite rhyolite, fine-grained light-colored acidic volcanic rock. Rhyolite is chemically the equivalent of granite, and is thus composed primarily of quartz and orthoclase feldspar with subordinate amounts of plagioclase feldspar, biotite mica, amphiboles, and pyroxenes.  and rhyolite breccias which hosts the widening mineralized min·er·al·ize  
v. min·er·al·ized, min·er·al·iz·ing, min·er·al·iz·es

v.tr.
1. To convert to a mineral substance; petrify.

2. To transform a metal into a mineral by oxidation.

3.
 zone but also the presence of copper mineralization which is increasing near the base of the sulphide intersection signifying a phase change from predominantly zinc to copper. Down-hole large loop Pulse EM surveys are being completed in Hole CLS 98-59 and also in adjacent Holes CLS 98-28, 98-39 and 98-53. Results from these surveys will guide the next phase of deep drilling.

Significant intersections from Hole CLS 98-59 include:


Hole        Intersection  Length   Zinc  Copper  Silver  Gold
Number        (metres)   (metres) (p.c.) (p.c.)  (g/t)  (g/t)

CLS 98-59   438.6-440.0     1.4    0.27     -     1.8    11.4
            506.0-626.0   120.0    1.03     -    11.6      -
Including   516.5-519.5     3.0    2.14     -    13.8      -
            534.5-539.0     4.5    2.88     -     4.6      -
            551.0-558.5     7.5    1.94     -    16.5      -
            573.5-578.0     4.5    2.18     -    16.9      -
            602.0-605.0     3.0    2.61     -     5.7      -
            624.5-626.0     1.5    2.78    0.64  25.4      -





Holes CLS 98-57, 58 and 60 were step-out geological holes, located from 1.0 to 2.0 kilometres southwest of Hole CLS 97-16 in the Cross Lake Zone. Of significance was the intersection of black chlorite chlorite

Widespread group of layer silicate minerals composed of hydrous aluminum silicates, usually of magnesium and iron. The name, from the Greek for “green,” refers to chlorite's typical colour.
 and chalcopyrite in Hole CLS 98-58 which correlates with the results of follow-up Pulse EM and Mise-a-la-Masse surveys. These surveys identify a strong conductor (possible copper) passing below the hole and plunging to the west. Copper mineralization has now been traced for 200 metres along strike in the area of these holes, confirming that a series of vents occur along the 5 km Cross Lake IP trend. Hole CLS 98-61, collared 400 metres southwest of CLS 98-58, intersected a granite dyke and was terminated.

Significant intersections are as follows:


Hole        Intersection  Length   Zinc  Copper  Silver  Gold
Number        (metres)   (metres) (p.c.) (p.c.)  (g/t)  (g/t)

CLS 98-57   552.5-554.0     1.5    1.03     -    25.0      -
            578.0-585.5     7.5    1.01     -    38.2      -
            599.0-603.5     4.5    1.27     -    41.9      -

CLS 98-58   246.5-248.0     1.5      -     1.25   3.0      -
            264.5-267.5     3.0      -     1.38   4.8      -

CLS 98-60    71.0- 72.5     1.5      -     1.00   1.6      -
             95.0- 96.5     1.5      -     1.11   5.8      -
            137.0-138.5     1.5      -     1.91   6.8     1.2
            158.0-159.5     1.5      -     1.36   3.4      -
            164.0-165.5     1.5      -     1.20   3.6      -
            314.2-314.7     0.5    6.30     -     3.0      -





Cross Lake is continuing to conduct extensive geophysical surveys consisting of large loop Pulse EM, Mise-a-la-Masse and Induced Polarization (IP)/Magnetic surveys to guide the drilling program. A recent soil geochemical survey has identified targets to the northeast of the Cross Lake Zone which correspond with IP anomalies outlined earlier. As a result of the successful geochemical survey, this program will be expanded to cover areas located to the southwest of the Cross Lake Zone. Additional IP/mag surveys will be carried out to cover the area south of Area E (see map entitled "Exploration Target Areas & Drill Hole Locations", available by fax upon request). Recent Pulse EM and Mise-a-la-Masse surveys have already identified conductive targets within Areas A & E. In approximately three weeks, once results from the current work programs are received and interpreted, primary targets will be identified and drilling will continue.

ON BEHALF OF THE BOARD OF DIRECTORS CROSS LAKE MINERALS LTD.

Henry G. Ewanchuk, Chairman, President and Chief Executive Officer

The Vancouver Stock Exchange Vancouver Stock Exchange (VSE)

A securities and options exchange in Vancouver, British Columbia, (Canada), specializing in venture capital companies.


Vancouver Stock Exchange

See Canadian Venture Exchange (CDNX).
 has not reviewed and does not accept responsibility for the adequacy or accuracy of this release.

   CONTACT: Cross Lake Minerals Ltd.
             Michele Jones, 604/ 688-5448
             or
             Cross Lake Minerals Ltd.
             Kristina Kalmet, 604/ 688-5448
             http://www.crosslakeminerals.com


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Copyright 1998, Gale Group. All rights reserved. Gale Group is a Thomson Corporation Company.

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Publication:Business Wire
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Geographic Code:1CONT
Date:Jul 16, 1998
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