Exploration properties are located in NW Argentina in the province of Jujuy. This province is a politically stable area with a proven history of mining.
Two of Artha's properties surround the Silver Standard Pirquitas mine. This mine was completed at a cost of approx $250 million (US), and is expected to produce 8.5 million ounces of silver per year over its 9 year mine life, based on current reserves. Silver Standard reports that Pirquitas is the largest silver mine in Argentina and one of the largest primary silver mines in the world.
The geology of NW Argentina is divided into three sub-parallel northerly-trending structural belts comprising from east to west, the Sub-Andean Range, the Eastern Cordillera and the Altiplano or Puna belt. The exploration area is in Puna belt, which comprises Ordovician marine sediments, Tertiary continental sediments and, younger intrusives and volcanic rocks.
Mineral deposits in the region are dominated by base and precious metals such as well as sulphur, borax and salts. Proterozoic rocks are dominant and include interbedded sandstones, shales and greywackes of the Ordovician Acoite formation. These rocks are folded, typically with steeply-dipping axes that strike north to N 30 W.
Mineralization at the Pirquitas Mine comprises a polymetallic deposit rich in tin, silver and zinc in the form of veins, stockwork veinlets and disseminations, hosted in the Ordovician acoite formation. The mineralization is located on various groups of fractures of which the most significant are orientated N 75 W and N 45 W.
This remote, high Andean location has very well maintained access routes. The asphalted Highway 9 which heads northwards from the capital town of Jujuy, San Salvador de Jujuy, to the Bolivian border makes the property accessible throughout the year. To the west there is access to the port of Antofagasta in Chile on the newly constructed Highway 52. The nearest commercial airport is in San Salvador de Jujuy. There is a 2km gravel runway at the Pirquitas Mine site and Silver Standard Resources Inc plans to extend this to 3km.
The Pirquitas area is typical of the Argentine Altiplano: steep, rugged terrain with a distinct wet-dry season with moderate to cool days, cool to cold nights and, frequent strong winds from the west by north-west. The climate is typical for higher Andean regions with cold, dry conditions in winter, more evaporation than rainfall and, an annual temperature of around 80 C. Annual precipitation is around 300mm and is characterized by infrequent torrential rains.
The nearest community is the Nuevo Pirquitas village approximately 10 km from Pirquitas. This small community has a population of around 200 people who are already benefiting from work at the Pirquitas mine site. The nearest towns are at Susques, situated on the Trans-Andean Highway and, Abra Pampa. Both are 2 to 3 hours drive from the Artha properties.
The nearest cities are Jujuy and Salta in Argentina and Calamaand and Antofagasta in Chile.
In 2005, the Chile-Argentina paved highway was completed and allows access from the Chilean port of Antofagasta to the town of Susques in Argentina. From Susques to Pirquitas (a total length of 110km) access is by roads 74 and 74B. These gravel roads are currently being upgraded.
Access from Argentina is also by paved Highway 24 north from Jujuy to Abra Pampa and continuing northwards to the Bolivian border. There are several fairly well maintained gravel roads which head westwards across the Altiplano in the direction of the Chilean border.
There is an existing 2km long gravel airstrip at Pirquitas which allows access by light aircraft, that can fly from Jujuy or, Calama in Chile. The nearest commercial airport is at Jujuy.
Electrical power at the Pirquitas mine is generated from natural gas. The Norandino Argentina-Chile gas line was recently installed and passes to within 36km south of Pirquitas and where a 3" connection has been installed.
The Mining Integration Treaty between Argentina and Chile is the first of its kind and it was required as a result of the large number of mines in common interest regions. Additionally, several infrastructure projects promote integration between both countries.
Main features of the mining integration treaty:
Argentina not only has strong mining potential but it also offers a comprehensive and sound legal framework which provides clear rules of the game for mining investors.
Argentina provides national treatment for foreign investment and free transfer of capital and earnings. Foreign investors have the same legal treatment as nationals under the Argentine Constitution.
Foreign companies in Argentina may:
The Mining Code provides centennial rules on property, exploration and exploitation rights and obligations. It is extremely liberal, offering a wide scope to private enterprise and limiting direct government action.
The Mining Code generally establishes two large categories of minerals, namely:
Educated workforce: Argentina has one of the highest rates of university enrollment in the world and, by far, the highest in Latin America.
The lowest relative labor productivity gap in Latin America compared to the United States.

The rare earths licenses, covers over 415 square kilometers in southern Jujuy Province, NW Argentina. Susques is known to be prospective for a variety of rare earths elements, including yttrium, and thorium has been historically mined on a small scale. The local geology is dominated by Ordovician sediments and Tertiary intrusives and Carbonatites with little detailed exploration ever being done. Rare earth mineralisation observed to date is hosted in stockwork veins with the host structures up to 10 meters wide.
The properties were identified as part of the Company's continuous target generation strategy where new opportunities are constantly being reviewed to provide ongoing feedstock for our expansion and growth. The properties were selected based on extensive local knowledge and deep experience in the NW Provinces, in particular through our local country manager who has mined and prospected in this region for almost three decades. His expert knowledge has guided our efforts to secure strategically significant and geologically prospective properties, with rare earths providing an important opportunity.
A short reconnaissance program by AHC geologists in December 2009 targeted Susques where mapping and rock chip sampling identified a number of parallel mineralised veins that have been traced for over 6 km in total strike length. The initial results from this sampling included sample 26954 which returned elevated rare earth elements, including Yttrium.
| Sample Number | Ce ppm | Dy ppm | Er ppm | Eu ppm | Ga ppm |
|---|---|---|---|---|---|
| 26954 | 2990 | 106 | 18.65 | 182 | 17.2 |
| Gd ppm | La ppm | Nd ppm | Pr ppm | Rb ppm | |
| 474 | 1360 | 2550 | 472 | 13.4 | |
| Sm ppm | Sr ppm | Th ppm | Y ppm | Zn ppm | |
| 825 | 933 | >1000 | 192.5 | 90 |
Additional sampling on this property has shown that elevated levels of some rare earth metals are present on similar vein structures on other parts of the property.
These results are important first indicators of potential mineralisation considering the broader geological environment in which they lie. The ratio of heavy to light rare earths is also encouraging. More detailed work is now planned to commence in the coming months to ascertain the extent and economic potential of mineralisation.
The following is an extract from a local geology report:The small bodies and dykes of La Poma trondhjemite belt (La Poma Department, Salta) contain tantalum-niobium ( within the Cachi formation).The local geology is dominated by metasedimentary rocks of the Puncoviscana Formation. The trondhjemite bodies are barren in ore-forming elements against the metasedimentary rocks, with higher contents of Tantalum (Ta), Niobium (Nb), Lithium (Li), and Beryllium (Be). The mineralization is suggested to have formed by melting in the aureole contact on the metasediments. The Trondhjemitic magma raised the temperature of the country rocks, as observed in a thermal aureole around the plutons, changing the original rocks to greenshists (granulite facies).
When the rocks were partially melted, pegmatite lenses containing higher values of tantalium and niobium concentrated over ten times higher in the country rocks than in the trondhjemites.The pegmatite bodies have originated by partial melting of the metasedimentary rocks. Due to the process of melting, high contents of the lithophile elements sud as Ta,Nb,U, Th, W, Li and Be have been moved from metasediments to the melted zones. The trondhje,mite magma origin should be related to an active subduction zone during the evolution of the Famatinian arc (480-460 Ma). The Magmatic arc testifies a probable change in the arc configuration leading to melt the basic lower crust or the subducted young oceanic crust (< 25 Ma) or a change in the subduction angle resulting in the partial melting of the already accreted lower crust.
Artha has continued to add to its large and strategic rare earth property portfolio in northern Argentina (Map 1) through the recent staking of 60,000 hectares of ground in Jasimampa area in the Sierra Norte de Córdoba of Argentina Santiago del Estero Province. The new property lies directly east of a number of known small rare earth deposits. This new project is considered highly prospective for rare earth mineralization related to carbonatites, plus hydrothermal precious and base metal mineralization. Target generation work is planned to begin as soon as possible.
Very little modern exploration has ever been done in this new area, with historical records suggesting that the last serious exploration completed dates back to 1968. The project is well located in the province with good road access to the east of the properties (Map 2).
A research paper dated 2005 which focussed on the rare earth mineralization in the immediate vicintity, describes the area as follows"
"The Jasimampa area in the Sierra Norte de Córdoba of Argentina contains light rare earth element (LREE:Th-Nb) mineralization associated with several stages of carbonates and widespread fenitization of marble, granite (496 ± 2.9 Ma), and alkaline and siliceous igneous comendite dikes (U/Pb zircon age of 390 Ma) derived from fractionation of oceanic island basalts. This is the third discovery of LREE mineralization in Argentina and marks a new alkaline intracontinental magmatic event of Devonian age.
...Subsequent hydrothermal stages with carbonates, hematite, pyrolusite monazite, and subordinate celestine and barite caused alteration of marble that was accompanied by an increase in absolute REE abundance, up to 15.45 wt percent, and high Sr (10.5 wt %), Th (4,390 ppm), and Ba (1.8 wt %).
Alteration and mineralization at Jasimampa are the result of late-stage carbonatitic magma fractionation and fluid exsolution. This is indicated by the strongly alkaline character of early alteration, the composition of the hydrothermal carbonates, apatite, and LREE-Sr- and Ba-rich minerals, the chondrite-normalized REE patterns showing strong LREE enrichment without an Eu anomaly, and the replacement of marble by assemblages with very high Ba, Th, LREE, and Sr, and strong K, Zr, and Ti depletions. The alteration style and mineralization at Jasimampa are similar to the giant Fe-LREE-Nb deposit Bayan Obo (the world's largest deposit and producer of rare earth elements, located in Inner Mongolia) and other hydrothermal LREE deposits hosted in carbonatites of China."
The Bayan Obo Fe-REE-Nb deposit is the world's largest rare earth element (REE) resource with estimated reserves of up to 1500 Mt of iron ore (35% wt Fe), 48 Mt REE (6% wt RE 2 O 3 ) and 1 Mt Nb (0.13% Nb). The Bayan Obo Mine produced 55,300 tons of RE 2 O 3 in 2005, accounting for 47% of the total rare earth production of China and 45% of that of the world (in 2006)2.