22 February 2016
Harvest Minerals Limited
("Harvest Minerals" or the "Company")
Update on Arapua Fertilizer Project
Harvest Minerals Reports Completion of Geological Mapping and Ground Geophysical Survey at Maximus Prospect - Arapua Fertilizer Project
The Company is very pleased to announce the completion of a geological mapping programme and a ground geophysical survey at the Maximus Prospect, part of its Arapua Fertilizer Project. This work programme was devised to define the extent of a large area of highly mineralised phosphate and potassium rich rocks identified during an earlier auger drilling programme and assist in planning the upcoming drilling campaign.
Highlights:
· Systematic surface geological mapping was conducted over an area of approximately 10.2km2.
· Kamafugite rock, potassium oxide (K2O) rich rock, had been mapped over an area of approximately 1,691km2.
· Ground magnetic anomaly indicates a well-defined magnetic domain coincident to the kamafugite rocks trend and ground gamma-spectrometric results point to high values of Total Count, Uranium (U) and Thorium (Th) channels associated to the kamafugite rock.
· Company due to start initial air core drilling programme to validate initial auger results in February 2016.
· Initial metallurgical test work suggests grades can be improved by simple screening.
Executive Chairman, Brian McMaster, commented "Since receiving the proceeds of our recent funding in January, the team has been very busy ground mapping the extent of the potential DANF product. These excellent results indicate that once we have defined a commercial product, we would have sufficient source material to support a substantial long-life project. The team is currently preparing the ground ahead of commencing an initial air core drill programme next week to verify the original XRF results from the auger drilling. Once this has been completed, the drill programme will be expanded to estimate a JORC resource and further more detailed metallurgical test work will be carried out to define a commercial DANF product."
Background:
The Arapua Fertilizer Project is strategically located in the Brazilian Cerrado, 360 km NW from Belo Horizonte, the capital of Minas Gerais State. The project consists of seven granted exploration licenses covering a total area of 12,997.6 hectares, divided across both the Arapua and Maximus prospects.
At the Maximus prospect, the previous handheld XRF results from auger holes indicated the occurrence of kamafugite rock with K2O rich zones varying from 2m @ 5.95% K2O to 20m @ 7.96% K2O and 3.89% phosphorus pentoxide (P2O5).
Geological Mapping
The geological mapping programme has been carried out over an area of approximately 1,020 hectares at the Maximus Prospect. The mapping carried over the area identified six key geological units over the prospect area of which the kamafugitic rocks of the Patos Formation will be the target of the upcoming drill programme. A description of these six units is included at the end of this announcement.
The link below shows the Maximus Prospect geological map:
http://www.rns-pdf.londonstockexchange.com/rns/6679P_-2016-2-21.pdf
Ground Geophysics
The ground geophysics survey consisted of magnetometry and radiometry using 100 meters spaced lines over an area of approximately 90.5 km2.
The link below shows the analytical signal image with the different magnetic domains identified:
http://www.rns-pdf.londonstockexchange.com/rns/6679P_1-2016-2-21.pdf
The ground data and thematic maps produced distinguish between four magnetic domains in the block:
I - The west, north and south portions of the block have low magnetic and homogeneous values, corresponding to phyllites of Bambuí Group and sedimentary rocks of Areado Group.
II - The kimberlitic intrusion on the NW portion of the block. This anomaly stands out very clearly surrounded by a low magnetic zone. The magnetic data shows a classic dipole anomaly for this type of intrusive alkaline rock, elongated in the direction E-W, as illustrated in the total magnetic field map - TMI:
http://www.rns-pdf.londonstockexchange.com/rns/6679P_2-2016-2-21.pdf
III - The third magnetic domain defined corresponds to the occurrence of kamafugite rocks of Mata da Corda Group, together with secondary expressions of the lateritic horizons. This body of rock generates a dipole anomaly elongated to WSW-ENE as shown here:
http://www.rns-pdf.londonstockexchange.com/rns/6679P_3-2016-2-21.pdf
IV - The magnetic domain IV corresponds to a minor area with intermediate magnetic values surrounded by the domain III.
With respect to the radiometric data (gamma-spectrometry), the main observed contrasts clearly distinguish between the Bambuí Group and the Cretaceous units (Areado Groups and Mata da Corda) and Cenozoic covers:
http://www.rns-pdf.londonstockexchange.com/rns/6679P_3-2016-2-21.pdf
In the Total Count Map, the basement rocks of the Bambuí Group are related to areas with low total count values, while the sedimentary rocks of Areado Group appear coincidently to zones of moderate to high total count. The kamafugite rocks and the kimberlite intrusion are associated with high to very high radiometric values. The sedimentary cover on the top of Serra do Maxixe Plateau also shows a very low radiometric response in the Total Count map.
In the K channel map, the high K (Potassium) values on the west and north portion, are coincident with low relative values observed in thematic maps of Th channel and U channel. This corresponds to areas where the Bambuí Group occurs and the high value of K may be associated with the thick metapelite package, which normally present enriched in this element. Another possible factor responsible for this contrast is the high mobility of the K, which, in weathering processes, may have been removed from the higher portions and transported to the lower regions.
The same process can be related to the high relative values of Th and U, which correspond, in the field, to the kamafugite rocks and the lateritic crust. These Th units for higher ground throughout the region and its enrichment in these isotopes (U and Th) may be linked to depletion of K by weathering processes.
The link below shows the K channel map:
http://www.rns-pdf.londonstockexchange.com/rns/6679P_4-2016-2-21.pdf
The link below shows the Th channel map:
http://www.rns-pdf.londonstockexchange.com/rns/6679P_5-2016-2-21.pdf
The link below shows the U channel map:
http://www.rns-pdf.londonstockexchange.com/rns/6679P_6-2016-2-21.pdf
Is important to note that radiometric surveys shows only what is at the surface, therefore in areas with thick sedimentary or soil cover, the radiometric method should be used with caution.
Metallurgical Test Work
Some provisional metallurgical test work has been carried out on a sample from Maximus by ALS Minerals in Perth. Preliminary results suggest that simple screening could improve the grade, particularly of P2O5 although a more thorough work programme will be required to verify that.
Next Steps
The Company is currently preparing the ground to commence an initial air core drill programme which will involve twinning three of the original auger drillholes to a depth of 30m and then stepping out 50m to check the grade continuity. Once this programme has been completed, the Company will start an infill drill campaign to estimate a JORC resource and carry out a more detailed metallurgical test work.
Enquiries:
Harvest Minerals Limited |
Brian McMaster, Chairman |
Tel: +61 8 9200 1847 |
Strand Hanson Limited (Nominated & Financial Adviser) |
Rory Murphy / James Spinney / Ritchie Balmer |
Tel: +44 20 7409 3494 |
Mirabaud Securities LLP (Broker) |
Rory Scott |
Tel: + 44 (0) 20 7878 3360 |
COMPETENT PERSON STATEMENT
The technical information in this release which relates to the Exploration Results is based on compiled and reviewed data by Mr. Paulo Brito. Mr. Brito is a consulting geologist for Harvest Minerals Limited and is a Member of AusIMM-The Minerals Institute, as well as, a Member of Australian Institute of Geoscientists. Mr. Brito has sufficient experience which is relevant to the style of mineralization and type of deposit under consideration and to the activity which is being undertaken to qualify as a Competent Person as defined in the 2012 Edition of the "Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves". Mr. Brito also meets the requirements of a qualified person under the AIM Note for Mining, Oil and Gas Companies and consents to the inclusion in the release of the matters based on their information in the form and context in which it appears. Mr. Brito accepts responsibility for the accuracy of the statements disclosed in this release.
Appendix A: Description of Geological Units Identified at Maximus Prospect
The link below shows the stratigraphic column for Maximus Prospect area:
http://www.rns-pdf.londonstockexchange.com/rns/6679P_7-2016-2-21.pdf
Bambuí Group - This basal unit occurs in the low topographic levels, at the west and north portion of the area, and consists of light orange to brown metasedimentary rocks (phyllites), such as metapelites, metadiamictites and metarenites with foliation cleavage approximately North-South with high to moderate dip angles to the West. The Bambuí Group rocks compound the basement unit to the Mesozoic sedimentary and volcanic rocks of San-Franciscan Basin in the area.
Areado Group - In the mapped area this unit is mainly composed by brown to orange brown sandstones, subarkose to quartz composition, fine to coarse grained, with planar to cross stratification. The sandstones of Areado Group overlay the basement metamorphic rocks with a discordant sub horizontal contact. A few outcrops of claystone with very well marked planar lamination also have been mapped in this unit.
Mata da Corda Group / Patos Formation - The Patos Formation is composed by grey to olive grey volcaniclastics, pyroclastic and volcanic rocks which overlie the Areado Group unit. The volcaniclastic and pyroclastic rocks with a kamafugitic composition are predominant in this unit and occur over an area of 1,691km2. These rocks are generally highly weathered from 938 m to 1,057 m of RL along the N and S hill slopes of Serra do Maxixe Plateau. In the NW portion of the mapped area there occurs a well-defined kimberlite intrusive body with surface dimensions of approximately 124,445 m2. The rock is green to light green, phaneritic very fine texture, with olivine, magnetite, rare garnets and abundant country rock xenolith (Sandstones and Phyllites).
Mata da Corda Group / Capacete Formation - The rocks of Capacete Formation were mapped in the area. These rocks generally are highly weathered with red color, probably representing very fine volcanic arenites with a discordant contact over the Patos Formation rocks.
Detritic Lateritic Crust - This overlays the kamafugite rocks in relief level up to 1050 meters, with red to brown color, capping the plateau area. The lateritic crust generally ranges from 2 to 30 meters thickness.
Sedimentary Coverage - Sandy to silty sediments, orange to brown color, occur over the eastern part of Serra do Maxixe Plateau covering the Lateritic Crust.