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Gold/Mining/Energy : MARUM RESOURCES ON ALBERTA -- Ignore unavailable to you. Want to Upgrade?


To: zedex who wrote (1515)3/30/1999 11:04:00 PM
From: Jesse  Read Replies (1) | Respond to of 2514
 
Sensible thinking, Bruce, but no, alluvial diamonds are considered secondary deposits. This pyroclastic-body discovery is a primary... :>

Go back and read Rick's information about bedded deposits, as posted here a short while ago, for more info:

Message 8264960

Here's an excerpt:

"Leaving aside the issue of whether or not sub-marine volcanic cones ever existed in the Ashton area, (not likely, but we don't know for sure) the bedded deposits referred to in the recent Ashton release are almost certainly pyroclastics, i.e. "hot grainy rocks", which were dumped at or near their current location after being blown out of the vent. They certainly may have been re-sorted a bit by water action but they are essentially in the same place they were a few minutes or hours after they were blown out and fell back to the sea floor. In current cross section, they probably resemble grey or brown clay-rich "sandstones" interbedded with darker mudstones (i.e. shales). When they are less altered to clays (i.e. weathered) the kimberlitic components consisting of micas and olivine give them a medium- to dark-green colour. The tonnage potential of these bedded deposits in a place like Alberta are orders of magnitude higher than for pipe deposits and their geometry is amenable to "Alberta-style" mining, that is, gigantic scale mining operations using draglines."
=================
Time for the big time!

Regards,
-j
:>
PS,
Also, re-read this from tonight's NR:

"Major diamond deposits and resources thoughout the world are
closely associated with pyroclastics and volcaniclastics. In some
cases, such as at the DeBeer's Orapa mine in Botswana, the
grade of the volcaniclastic rocks can be many times higher than
the grade of the associated Orapa pipe material. Pyroclastics,
specifically lapilli pyroclastics, occur in and near the Ashton
pipes 125 km to the east of the Chinchaga area; are major
components in and near the Argyle diamond mine in Australia;
and are closely associated with diamond mines in Tanzania,
Botswana and South Africa."