Aurado receives drill results from Mexican properties
   Aurado Exploration Ltd                                                              AEO  Shares issued 41,308,610                                                 1999-01-14 close $0.065  Friday Jan 15 1999  Mr. William Dickie reports   Cominco Mexico, S.A. de C.V, a wholly-owned subsidiary of Cominco Limited, has completed seven  diamond drill holes totalling 1,927 metres on the Amapola, Venaditas and Piedrotas properties. These  are three of the eight properties in the joint venture. The drill program was designed to investigate  various targets defined by geophysical and geological programs.   AMAPOLA   The four holes on Amapola were mainly to test geophysical anomalies developed over a five kilometre  by three kilometre area in the northern part of the claim. It was considered that volcanic stratigraphy  favourable for volcanogenic massive sulphide type mineralization was present at shallow depths.   These four holes yielded geologically surprising results; the first being that the stratigraphic section  intersected was almost entirely in sedimentary rocks. No volcanic rocks similar to those outcropping a  few kilometres to the north were seen. Sufficient pyrite and/or pyrrhotite (4 per cent to 6 per cent) were  observed in the four holes to explain the induced polarization and magnetic anomalies.   The second surprise was to locate the presence of brecciation, alteration and anomalous lead, zinc,  silver, arsenic, tin values in the two eastern holes (AM 02, AM 03). The breccias are best developed in  AM 02 between 30 and 230 metres and in hole AM 03 between 60 and 270 metres.   Anomalous Pb, Zn, Ag values were best developed in AM 02 between 95 metres and 285 metres. The  best eight intervals, between one and six metres in length, are given in the following table. Highest  values were 2.3 per cent Pb, 1.9 per cent Zn and 122 parts per million Ag. Mineralization is associated  with galena and sphalerite in stockwork type veins and breccias. Hole AM 03 contained high As (3,100  ppm) and high Sb (233 ppm) associated with silicification between 243 and 274 metres.   It would appear from the evidence in holes AM 02 and AM 03 that these holes are in the vicinity of a  heat source. This area is characterized by higher resistivity and lower residual gravity values and should  be tested for Ag, Pb, Zn mineralization. 
 
  Pb Zn Ag Intersections in AM-02
                Thick-   Interval     ness     Pb    Zn      Ag      m          m      ppm   ppm     ppm         95.9 - 98.1   2.20   6,777  9,974    32
   128.2 -129.5   1.30  22,760 19,320   122
   134.7 -135.7   1.00  11,290  8,149    40
   136.3 -137.4   1.10  26,630    325    92
   148.0 -150.3    2.3  12,918  4,219    68
   167.9 -169.4    1.5   6,918  7,374    35
   240.0 -243.0    3.0  12,635    899    37
   279.0 -285.0    6.0   6,576    215    12 
   Analyses in Cominco Lab by ICP   with hot Aqua Regia digestion.
   VENADITAS   Two holes were situated on Venaditas to test gradient array and dipole-dipole IP anomalies with  chargeability similar to that obtained over the San Nicholas discovery. The area is underlain by  sediments and volcanics containing altered rhyolite porphyry. This environment is considered favourable  for VMS style mineralization. Hole VE 01 was also situated over a combined magnetic and gravity  anomaly.   No significant anomalous values were obtained in either hole. The gravity anomaly remains unexplained  but enough pyrite was found to explain the IP anomaly. Hole VE 01 was entirely in sediments but  VE-02 intersected in its upper part 140 metres of rhyolite, intermediate to mafic volcanics and  microdiorite.   It appears that a downfaulted block of volcanic stratigraphy is preserved on the southern part of the  Venaditas property. Consideration may be given to further drill testing of the E-W belt of anomalous  gradient array IP that straddles the volcanics.   PIEDROTAS   One hole was drilled on the property to test a dipole-dipole IP anomaly at 150 metres depth. The area  showed mafic and felsic volcanic outcrops on surface. Unfortunately, this turned out to be no more than  a "skim" of volcanics and the hole intersected a sedimentary section with 3 per cent to 6 per cent pyrite,  enough to explain the IP anomaly.   RECOMMENDED WORK ON GARABATO   Reconnaissance gravity and airborne magnetics on the eastern part of the garabato claim (one of the other  five claim groups in the joint venture) an area with coincident gravity high and a magnetic anomaly.  Follow-up gravity, magnetics and IP should be done.   (c) Copyright 1999 Canjex Publishing Ltd. canada-stockwatch.com |