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Gold/Mining/Energy : Gold and Silver Juniors, Mid-tiers and Producers -- Ignore unavailable to you. Want to Upgrade?


To: TheBusDriver who wrote (26873)12/2/2006 8:57:02 AM
From: loantech  Read Replies (1) | Respond to of 78404
 
Back to 47 cents or so so getting fairly positive or closer to break even.



To: TheBusDriver who wrote (26873)1/11/2007 12:23:38 PM
From: loantech  Read Replies (2) | Respond to of 78404
 
Tinka samples five m of 763 g/t Ag at Colquipucro

2007-01-11 10:16 ET - News Release

Mr. Andrew Carter reports

TINKA'S SURFACE CHANNEL SAMPLING EXTENDS DIMENSIONS OF LARGE SILVER SYSTEM AT COLQUIPUCRO PROJECT IN PERU, INCLUDING 5M AVERAGING 763 G/T AG

Tinka Resources Ltd. has provided further results of surface channel samples taken from the company's 100-per-cent-owned 2,079-hectare Colquipucro property located within the richly mineralized Zn-Pb-Ag belt of central Peru.>>>>>

new.stockwatch.com

Uh similar to this maybe?:

NEWS RELEASE November 26, 2004
EXPLORATION IDENTIFIES HIGHLY MINERALIZED ZONE AT LUMINARIA, PERU
Vancouver, Canada – Tinka Resources Limited (TSXv - TK; Frankfurt – TLD; Pinksheets-TKRFF).
Mr. Andrew Carter, President, is pleased to report that the Company has completed the first phase exploration program on the Company's 3,500 hectare Luminaria Project. The project is located in the Huaraz mining district, department of Ancash, Peru.A field crew has been on site for four weeks undertaking a comprehensive soil, pitting and channel sampling program on the Rurimarac Hill area. Twenty-five pits were dug to an average depth of two metres and channel sampled. In addition, 133 soil samples were collected on a grid system. A highly anomalous area of gold mineralization has been confirmed from this work in the northern zone of Rurimarac Hill, with further channel sampling currently being carried out to fully define its extent. The anomalous gold values are associated mainly with pyrite, arsenopyrite and grey quartz occuring in the Chimu Formation, and in also white quartzite with narrow shale and coal horizons in contact with strongly altered
diorite. One hundred and thirty-three soil samples were taken every 20 metres, at an average depth of 30 cm, along
220 metre long east-west lines, spaced 100 metres apart, over a total north-south distance of 1,200 metres. Gold values range from 0.02 g/t gold to 1.86 g/t gold, and these values are complemented by anomalous copper, lead and arsenic. Soil sampling suggests that the mineralized area is faulted-off along the west edge of the grid system but remains open in all other directions. Twenty five pits were dug within the zone of interest to a maximum depth of 4 metres and are located within an area of about 270 metres by 100 metres. The pits intersected the Chimu formation and bottomed in strongly
altered porphyry intruding the overlying quartzites. Vertical channel samples in the pits ranged from 1.2 g/t gold
to 24.6 g/t gold with an average of 7 g/t gold over 2 metres.>>>