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Clean Energy Transition Inc V.RRS


Primary Symbol: V.TRAN Alternate Symbol(s):  GCRIF

Clean Energy Transition Inc., formerly Rogue Resources Inc., is a Canada-based company. The Company is focused on opportunities to generate positive cash flow, across the energy transition. The Company includes a Quartz division focused on advancing its silica/quartz business with the Snow White Project in Ontario and the Silicon Ridge Project in Quebec. The silica in high-quality quartz can be used to make silicon metal, a key component in solar energy panels. The Snow White property is approximately 27 km northwest of the town of Massey, 105 km west of the city of Sudbury and 500 km north-northwest of Toronto. The Silicon Ridge Project is located approximately 40 km north of the City of Baie-Saint-Paul, which borders the north shore of the Saint Lawrence River in central Quebec, Canada. The property comprises eight (8) contiguous maps designated mineral claims (CDC claims), which form a rectangular block covering a total area of 462.6 ha.


TSXV:TRAN - Post by User

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Post by DoctorFouadon Mar 04, 2016 7:13am
114 Views
Post# 24620903

Example of Anzaplan Test Results : Dingo Hole Silica Project

Example of Anzaplan Test Results : Dingo Hole Silica ProjectI second LeMarcus opinion. What should matters for investors when evaluating different deposits/mining projects is the economic value of the deposit, and you just cannot judge the economic value of a deposit by simply selecting and assaying a couple of surface samples. Extensive sampling/assaying, Geological mapping, Drilling, Resource Estimate, Metallurgical Test Results of representative samples, Environemental studies, and a PEA are necessary. Any serious junior mining company company cannot skip these steps PERIOD

To illustrate my point, the following is an example of anzaplan initial metallurgical test results for a silica deposit in Australia called "Dingo Hole" owned by RUM jungle resources. 


ASX Release
23 October 2015
Dingo Hole Silica – Initial processing test work results
Background
Rum Jungle Resources Ltd (RUM) announced initial surface sampling silica
exploration results to the ASX on 20 July 2015. Subsequently, Rum Jungle
Resources engaged Dorfner Anzaplan of Germany to conduct initial processing
test work on surface samples collected from the Dingo Hole Silica project.
Approximately 100 kg of sizeable quartz rock lumps, randomly collected from
the surface at Dingo Hole, were sent to Dorfner Anzaplan in July 2015.
 
Mineralogical and metallurgical tests were conducted to identify the presence
and nature of impurities. A portion of the quartz rock fragments was
autogenously ground and sized so that further physical (flotation, magnetic
separation), chemical (acid leaching, hot chlorination) and thermal (calcination)
processing tests could be conducted in order to remove impurities. This
processing route represents the traditional processing path for the production of
High Purity Quartz (HPQ) globally. This initial phase of metallurgical processing
test work is now complete.
 
Initial Metallurgical Test Work Results
The test-work sample utilised by Dorfner Anzaplan had a relatively high level of
initial measured impurities (2,600 ppm) that included approximately 2,055 ppm
of calcium, which is significantly higher in impurities than the majority of
samples previously assayed as part of the program of surface sampling work
conducted at Dingo Hole. Analysis of Dingo Hole rock samples to date does
indicate a reasonable amount of variability in impurities.
 
On a positive note, the primary process test work reduced the measured
impurities to approximately 119 ppm, which is in the range of what could be
considered as low to medium grade HPQ. However, industrial utilisation and the
association of IOTA high purity quartz standard with such products is contingent
on the makeup of the impurities that remain after processing. In most cases,
aluminium, lithium and titanium can be problematic but in the case of Dingo
Hole, these elements seem to be manageable. However, in the case of the
Dorfner Anzaplan sample, elevated levels of calcium, magnesium, iron and
boron that remained in place after processing tests, did not meet the IOTA
standard for varying uses of HPQ. These particular impurities have a detrimental
effect on the creation of high end silica products and even lower value optical
glass and semi conductor fillers. This is primarily due to excessive bubbling that
occurs when the silica is melted to create glass. Reduction of impurities that
cause this bubbling will be a necessity.
 
Therefore, at this point, it cannot be categorically stated that a marketable HPQ
product can, or cannot, be produced from the Dingo Hole Silica project.
Accordingly, this is very early stage and more work is required but there is no
guarantee that an IOTA standard, marketable HPQ can ultimately be produced
based on processing test-work to date.

Moving Forward
RUM will now consult with local and overseas silica experts and will conduct further discussions with Dorfner Anzaplan regarding the way forward. Topics of discussion will include:

· better understanding of sample selection and preparation that may impact test-work results

· potential of alternate processing methods to remove problematic impurities including optical sorting,
different grind sizes, different flotation reagents, additional flotation stages, acid gestation times and
pyro-metallurgical processes

· the potential of starting with lower impurity feedstock in the next phase of processing test work which may enable the right impurity levels to be attained at the end

· understanding of the future use cut-off grades for certain elements in feedstock to enable IOTA
standard HPQ production

· more systematic sampling and/or drilling of the mineralised area to more fully understand the chemical distribution of the SiO2 and the impurities

·engaging the HPQ industry to understand potential uses for this quality of product which may differ
from normal standards

Furthermore, RUM, through a study of publically available information, satellite imagery and geological maps, has identified a number of other areas with the Northern Territory that may host pedogenic chalcedonic silica rock (white quartz), similar to Dingo Hole. Exploration License Applications have been submitted and some initial analysis of rock samples will be conducted to ascertain the quality of these new potential deposits and to compare with the Dingo Hole white quartz.
 
Conclusion
Whilst the initial test-work results have not met the rigid IOTA standards for HPQ, this project is at an early stage of its evolution and more systematic sampling, analytical and test work needs to be done. Moreover, the HPQ industry is small and has limited transparency, so further understanding of the markets, its participants, quality requirements and potential end uses will also be critical.
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