SI
SI
discoversearch

We've detected that you're using an ad content blocking browser plug-in or feature. Ads provide a critical source of revenue to the continued operation of Silicon Investor.  We ask that you disable ad blocking while on Silicon Investor in the best interests of our community.  If you are not using an ad blocker but are still receiving this message, make sure your browser's tracking protection is set to the 'standard' level.
Microcap & Penny Stocks : Microcap Kitchen Canadian Stocks -- Ignore unavailable to you. Want to Upgrade?


To: czechmate who wrote (12388)9/5/2013 2:55:25 PM
From: Goose94  Respond to of 49402
 
Pangolin Diamonds (PAN-V) boasts exploration legends on the ground in diamond haven Botswana

Pangolin Resources fully funded to complete its 2013 exploration and drilling plans, made headlines at its Tsabong North project in Botswana earlier this year with the discovery of two kimberlites within a few months of starting drilling — and the Toronto-based explorer’s ambitions for the future are no less impressive, with management targeting at least 15 kimberlite discoveries by year end with the hope that at least one of these will be diamondiferous.

Pangolin’s management and team leaders are equipped with over 135 years of combined diamond exploration experience in the region. Fittingly, Pangolin boasts as one of its directors Dr. Leon Daniels, a mining veteran with almost four decades of diamond exploration experience, much of it carried out in Africa.

After discovering the Klipfontein kimberlite pipe in South Africa early in his career, Dr. Daniels also discovered the Mambali kimberlite field in Zimbabwe and notably the DK4 kimberlite, which holds the distinction of being the only kimberlite in the Orapa kimberlite field not discovered by De Beers.

Dr. Daniels shows no signs of slowing down, having co-founded African Diamonds (AIM:AFD), which was subsequently acquired by Lucara Diamond (LUC-T), one of the Lundin group of companies, in 2010, for $100 million.

The Pangolin team was further strengthened in June by the addition of Manfred R. Marx, a prominent geologist who led the field team that discovered the De Beers Orapa Diamond Mine -- the second largest open pit diamond mine in the world -- as a consultant to Pangolin’s on-site exploration team. Marx has over 45 years of diamond exploration and discovery experience.

It was on Dr. Daniels’ watch, however, that Pangolin discovered two near surface kimberlites — each believed to be greater than 20 hectares — during this current calendar year at the Tsabong North project, an achievement all the more notable when tempered with the knowledge that only seven new kimberlites have been discovered in the country in the past five years. In addition, 45 mantle derived garnets inclusive of high pressure garnets were discovered in one of the drill core holes 22 metres below the surface.

Of Pangolin’s projects, 100 per cent owned Tsabong North, located approximately 100 km north of the town of Tsabong in southwestern Botswana, shows the most outwardly noticeable signs of mineralization.

The 1,545 km2 property, comprised of anomalous concentrations of kimberlite indicators, is also signposted by large geo-botanical features so apparent they are visible on google Earth. The explorer has identified more than 50 drill-ready aeromagnetic targets in the project area, several of which have surface areas exceeding 20 hectares.

Soil sampling has turned up highly anomalous concentrations of kimberlite indicators within the project area inclusive of G10 garnets. The current drill core results suggest there is more than one kimberlite source in the project area.

Certainly, the project is in the right neighbourhood -- the Tsabong North Project is situated immediately north of the diamondiferous Tsabong kimberlite field that hosts the M-1 pipe, the largest known diamondiferous kimberlite pipe in the world. That pipe has a Pangolin connection, as it was Dr. Daniels, now Pangolin's single largest shareholder, who developed the geological model of the 180 hectare M-1 pipe as part of the Falconbridge team led by Chris Jennings. Dr. Daniels’ connection with the area continues, as he was also directly involved in the discovery of several new kimberlites in the Tsabong kimberlite field.

Tsabong North, the site of current drilling, was selected for what was felt to be significant potential “because in the known Tsabong kimberlite field there are many large kimberlites,” says Dr. Daniels, and large, he points out, means more than 20 hectares, equating to a potential 25-year mine life.

The largest known kimberlite covers 180 hectares, making the size of the targets Pangolin is turning up, based on independent geo-physicists assessments of the data, all the more impressive. “The largest one they are modelling is 270 hectares,” says Dr. Daniels. “There are two other clusters of targets in that small confined area — one potentially is 175 hectares, and the other potentially is 170 hectares.”

By way of contrast, the largest mine in size in Botswana is Orapa, which covers 116 hectares, while the largest in world, Mwadui in Tanzania, covers 143 hectares.

Another of Pangolin's four project areas, the Jwaneng South site, is in a similarly good neighbourhood, located 50 km south of the mine that holds the distinction of the richest diamond mine in the world by value, De Beers’ Jwaneng mine.

The 799km2 property has already been the subject of a detailed aeromagnetic and radiometric survey, which identified multiple large aeromagnetic anomalies commonly associated with kimberlites.

In addition, a well defined geo-botanical anomaly, a thicket of tall thorn trees with deep roots with a diameter of 1.4 km — reminiscent Dr. Daniels says of the “very distinctive” anomaly that marked Orapa, so clearly pilots used to use it as a navigational beacon -- provided a target for a ground gravity survey.

The survey included findings such as the discovery of kimberlite indicator garnets in soil samples and an isolated gravity low similar to gravity lows associated with the nearby Jwaneng mine kimberlites and others in this field.

Drilling on the site is to commence in the third quarter of 2013, with “over 25 targets” already selected, according to Dr. Daniels.

The Mmadinare project, which covers an area of 1,345 km2, has similar geological terrain to that hosting the Venetia, Martins Drift and The Oaks diamond mines, and has already been the subject of aeromagnetic surveys with kimberlite indicator minerals reported on the site by DeBeers, which prospected there in the past.

On that site, replete with infrastructure, Dr. Daniels says: “We’re targeting 2 to 5 hectare high grade kimberlites, that we can put into production ourselves at low cost.”

This low cost production will come at least in part due to the fact that the near surface deposits do not require drilling. “We simply dig exploration pits similar to the pits that discovered Orapa,” says Dr. Daniels. “We can sample down 30 meters.”

The company’s Malatswae project covers an area of 1,616 km2, and has been the subject of detailed aeromagnetic surveys and extensive soil sampling data, which turned up anomalous garnets; the site’s garnet chemistry indicates an unknown kimberlite source, that is, a separate mantle source to any known kimberlite field.

Malatswae South is to have a mainly alluvial focus stemming from the Orapa kimberlite field 70 kilometres distant, one of the few major diamond-producing fields that doesn’t have any significant alluvial finds associated with it.

“Over the past 20 years I’ve been tracking some paleo rivers now covered by Kalahari Desert sands,” says Dr. Daniels, “and we’ve finally found an area that we believe will yield a deposit of diamonds. One channel is about 400 metres wide and 20 metres deep. It’s a major river system that’s very capable of transporting diamonds. There’s nothing to trap the diamonds so they keep on moving; we’ve located a place where a major dike cuts across the directional flow of the river ... and that’s the ideal position to drop down diamonds. We fully expect to find potholes there [in the riverbed].”

“This is the ideal environment to find significant potholes with very high concentration of diamonds. I’m expecting to find high quality diamonds and large diamonds at high concentrations within the alluvials.”

Near-term company plans are to continue drilling at Tsabong North and commence drilling at Jwaneng South, as well as to continue follow-ups with ground magnetics, gravity, trace element and indicator sampling in selected areas. The completion of an NI-43-101 on Jwaneng South is also a plan going forward as is advancing work on the alluvial sites.

The setting is entirely appropriate for a company with such an abundance of reputation and expertise: Botswana too has a rich and storied history in diamond mining, holding the distinction of the largest diamond-producing country in the world when calculated by value.

With its politically stable regime and transparent mineral tenure system, the stable southern African nation of Botswana is rated the number one country for mining in Africa by the Fraser Institute.

http://www.proactiveinvestors.com/companies/news/47699/pangolin-diamonds-boasts-exploration-legends-on-the-ground-in-diamond-haven-botswana-47699.html



To: czechmate who wrote (12388)10/17/2013 8:07:10 AM
From: Goose94  Read Replies (1) | Respond to of 49402
 
Dr. Willem Smuts and Dr. Leon Daniels's Pangolin Diamonds (PAN-V) drilling what could be the world's largest kimberlite at Tsabong North in Botswana. The discovery holes came several months ago but Pangolin originally thought it had two large pipes, Magi-1 and Magi-2. They now appear to be a "single intrusive complex" spanning 270 hectares. (A circular pipe of that size would be nearly two kilometres in diameter.) The find dwarfs even the mammoth kimberlites in the Fort a la Corne district of Saskatchewan. Those pipes lie beneath 150 metres of overburden and low-grade rock, but Magi is closer to surface, with kimberlite occurring at depths between 30 metres and 60 metres. Pangolin also touts two other targets that span 170 hectares apiece. What Dr. Smuts, president and CEO, and Dr. Daniels, chairman, do not have yet are diamonds, which limits the market's enthusiasm. In May, Dr. Daniels touted the recovery of high-pressure garnets recovered just above the surface of the pipe but there has been no word if the kimberlite contained any microdiamonds. Pangolin says it will drill anther seven holes into Magi to delineate the body and collect at least 100 metres of kimberlite per hole to recover "any additional indicator minerals, and any diamonds." It is not the most inspiring of work descriptions, but Dr. Smuts and Dr. Daniels are more comfortable wandering the halls of academia than prowling Howe Street.

_____________________________________________________________________________________

Pangolin Diamonds Corp. has discovered one of the largest kimberlites in the world, modelled at 270 hectares (2.7 square kilometres), at its 100-per-cent-owned Tsabong North project in Botswana.

A number of the world's largest kimberlites include:

  • Se251 in Angola, measuring 220 hectares (2.2 square kilometres);
  • MK1 in Botswana, measuring 180 hectares (1.8 square kilometres);
  • Mwadui in Tanzania, measuring 146 hectares (1.46 square kilometres).


Kimberlite discovery

The new discovery stems from Pangolin's discovery earlier this year of two kimberlites, Magi-01 and Magi-02, at its Tsabong North project.

Aeromagnetic data on those finds were submitted by Pangolin for independent review by Billy Steenkamp, of Xcalibur Airborne Geophysics of Pretoria, South Africa. Mr. Steenkamp is a qualified person under National Instrument 43-101 rules. His observations include the following:

  • The previously reported Magi kimberlites are part of a single intrusive complex with a total surface area estimated at 270 hectares (2.7 square kilometres);
  • Some of the selected intrusive kimberlite targets could be of syn- or pre-Karoo age;
  • Two new kimberlite drill targets have been identified with total intrusive areas modelled at 170 hectares (1.7 square kilometres) and 175 hectares (1.75 square kilometres).


Based on these observations, Pangolin drilled a new hole between the Magi-01 and Magi-02 kimberlites. The new hole positively intersected the same sandy tuffs recognized in the two previous drill holes, confirming that the Magi kimberlite is a single large body and not two smaller kimberlites as previously believed.

The Magi kimberlite has now been confirmed over a distance of 1,200 metres in an east-west direction. The average depth of intersection of the crater facies sediments is approximately 35 metres. The depths of intersection of the sandy tuffs vary between 55.3 and 61.5 metres.

Further work will begin shortly; seven additional holes have been laid out for core drilling to determine the final size of the Magi kimberlite. These core holes will also be used toward modelling the complex geology of the crater sediments and kimberlitic sandy tuffs in preparation for future possible larger-diameter drilling. Each hole will intersect at least 100 metres of kimberlite to recover any additional indicator minerals, and any diamonds. One hole will be drilled to a minimum depth of 250 metres of kimberlite intersection.

Detailed logging of the core indicates that the Magi kimberlite is of syn-Karoo age. This makes it older than the Cretaceous diamondiferous kimberlites of the Tsabong kimberlite field farther to the south, dated at 78 million years, but potentially similar in age to the Jwaneng kimberlites, dated at 245 million years.

Core samples from all the holes are being submitted to independent laboratories to recover any additional indicator minerals, and any diamonds. High-pressure garnets originating deep in the earth's mantle have previously been recovered from the Magi-1/1 drill core, 14 metres above the surface of the Magi kimberlite.

Dr. Leon Daniels, PhD, chairman of the board of Pangolin, stated, "The geophysical models available to Pangolin strongly suggest the potential for discovering additional very large kimberlites in the Tsabong North project area."

About the Tsabong North project

The Tsabong North project, located approximately 100 kilometres north of the town of Tsabong in southwestern Botswana, is 1,545 square kilometres in size. It comprises anomalous concentrations of kimberlite indicators and has large geo-botanical features. Pangolin has identified more than 50 drill-ready aeromagnetic targets in the project area, several of which have surface areas exceeding 20 hectares (0.2 square kilometre).

The Tsabong North project is situated on the margin of the Archaean Kaapvaal craton in a similar tectonic environment to the Orapa kimberlite field. The 45 mantle-derived garnets inclusive of the high-pressure garnets were discovered in the drill core Magi-01/01. These garnets are very similar in chemical composition to the garnets from the Letlhakane mine in the Orapa area.

Pangolin's soil sampling has produced highly anomalous concentrations of kimberlite indicators within the project area. Microprobe analyses of indicator minerals have confirmed the presence of G10 garnets, indicating the presence of a mantle conducive to the crystallization of diamonds. A number of indicators occur, including remnants of kelyphite that indicate close proximity to kimberlite. Enzyme-leach trace element results are consistent with orientation trace element results over known kimberlites near the project.

The company cautions that information regarding the Se251, MK1, Mwadui and Orapa kimberlites, and Letlhakane mine or Orapa mine, are not necessarily indicative of the kimberlite or kimberlite targets being drilled by the company. The company further cautions that there is no guarantee that the kimberlite and/or kimberlite targets being drilled by the company will return diamond results of any economic significance.

The technical disclosure in this news release has been reviewed and approved by Dr. Leon Daniels, PhD, member of AIG, chairman of the board of Pangolin, and Manfred R. Marx, BSc, diploma environmental sciences. Both are qualified persons under National Instrument 43-101 rules.