![]() |
||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
projectsoverviewtagpura-maangob
|
batoto and tarale gold corridor
|
|||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
![]() batoto project site |
Cadan's Batoto gold project has a historic Philippine resource of 2.1 million ounces of gold. Work completed to date indicates that potentially profitable gold mineralisation is widespread. The Tarale gold project will be explored further, and has shown features similar to the exciting new Cadan copper-gold discovery. | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
batoto gold projectCadan's Batoto Gold Project has a historic Philippine resource of some 39mt @ 1.8 g/t gold for some 2.1 million ounces of gold. Gold mineralization is located within a regional igneous intrusive body known as the Maragusan Diorite as highlighted in the area tenement map. tarale gold projectAt the Tarale area company geologists have recognised a coincident magnetic and IP Resistivity anomaly which shows a coincident relationship with the line of high gold grade quartz veins that Cadan has bulk tested. Modelling of geophysical data has indicated that the western-most geophysical line of the survey shows anomalous features similar to the new Cadan Porphyry discovery. Further mapping will be undertaken over this exciting new prospect. batoto gold projectexplorationThere is very clear evidence from the surface mapping, drilling and geophysical data of structurally controlled stockwork vein arrays associated with locally intense quartz pyrite- sericite (clay mineral) alteration in the core of the systems. The gold mineralisation appears to be hosted within large alteration zones (selvidges) developed as haloes surrounding 1mm to 5cm wide veins - see photographs of core and surface exposures with grade of the sampled core interval. These thin veins or veinlets characteristically comprise quartz-pyrite or sometimes pyrite only, within a strongly developed quartz-sericite-pyrite selvedge that is often ten times wider than the central vein itself. Petrographic study has indicated gold to be associated with pyrite as grains of 5 to 75 microns. These features can be seen in both the weathered/oxidized host diorite and the unweathered protore but the appearance is somewhat different. batoto-tarale drilling intersections
See news releases for more information:
tarale gold projectexplorationCadan has conducted surface and underground exploration in the 9,000ha Comval Project area since mid 2003. It has completed a first phase drilling program designed to identify and delineate large low medium grade gold resources which it believes are located in several separate zones. The work completed to date clearly indicated that potentially economic gold mineralization is widespread but localized to a large extent by wide structural zones which have been extensively altered. A 50 tonne bulk sample treated from this area returned 3.2g/t of gold and 47.3g/t of silver per tonne. Channel sample assay values however are of the order of .5 g/t gold This indicates a nugget effect and suggests a different assay technique is required to provide more authentic results from the channel samples. Several thousand tonnes of mineralization has been bulk tested at a nearby CIP plant. This bulk testing trial mining and processing operation indicated that the mineralization at Batoto was amenable to treatment by simple carbon-in-pulp methods with recoveries in excess of 90%. In addition to the drilling program, Cadan undertook a large surface mapping and trenching program to help determine the principal structural zones believed to locally control the highest gold grades as well as completing a major geophysical program. The emerging geological picture from the extensive surface and underground mapping program is more complex than initially believed. However, at this time, knowledge of the entire Comval Project area is at an early stage and additional exploration activities need to be completed.
Interpretation of drilling, other sub surface data and surface data indicates that mineralisation at Batoto occurs in a ENE - WSW trending zone -Clarke Mineralised Zone - that is steeply dipping to the north. It is believed that the Clarke Mineralised Zone width is more than 100m and less than 250 metres has been mapped and is open to depth and along strike in both directions. See the table of drill intersections. |
core photos![]() ore photo ore photos ![]() ore photo ![]() microscopic gold in core sample maps ![]() comval project map ![]() satellite map of projects ![]() satellite map close-up of Comval projects models ![]() composite model ![]() magnetic intensity model ![]() Batoto-Tarale gold belt with IP overlay photos ![]() in the trench ![]() project landscape ![]() project landscape view ![]() project site |
|||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Help us improve this web site! Contact us with your questions and comments.
© Copyright 2008 Cadan Resources Corporation | All Rights Reserved | Disclaimer | Privacy Policy
Porphyry deposits are low to mid-grade, large-tonnage mineral deposits.
Epithermal deposits are mineral deposits consisting of veins and replacement bodies, usually in volcanic or sedimentary rocks.
An adit is a type of entrance to an underground mine which is horizontal or nearly horizontal. Compare to a tunnel, which is a horizontal excavation which goes completely through a body of earth.
A Mineral Resource is a concentration or occurrence of material of intrinsic economic interest in or on the Earth's crust in such form, quality and quantity that there are reasonable prospects for eventual economic extraction. The location, quantity, grade, geological characteristics and continuity of a Mineral Resource are known, estimated or interpreted from specific geological evidence, sampling and knowledge. Mineral Resources are sub-divided, in order of increasing geological confidence, into Inferred, Indicated and Measured categories. Definition from Australasian Joint Ore Reserves Committee (JORC).
Indicated Resource is that part of a Mineral Resource for which tonnage, grade and mineral content can be estimated with a low level of confidence. It is inferred from geological evidence, sampling and assumed but not verified geological and/or grade continuity. It is based on information gathered through appropriate techniques from locations such as outcrops, trenches, pits, workings and drill holes which may be limited or of uncertain quality and reliability. Definition from Australasian Joint Ore Reserves Committee (JORC).
Inferred Resource is that part of a Mineral Resource for which tonnage, grade and mineral content can be estimated with a low level of confidence. It is inferred from geological evidence, sampling and assumed but not verified geological and/or grade continuity. It is based on information gathered through appropriate techniques from locations such as outcrops, trenches, pits, workings and drill holes which may be limited or of uncertain quality and reliability. Definition from Australasian Joint Ore Reserves Committee (JORC).
Measured Resource is that part of a Mineral Resource for which tonnage, densities, shape, physical characteristics, grade and mineral content can be estimated with a high level of confidence. It is based on detailed and reliable exploration, sampling and testing information gathered through appropriate techniques from locations such as outcrops, trenches, pits, workings and drill holes. The locations are spaced closely enough to confirm geological and grade continuity. Definition from Australasian Joint Ore Reserves Committee (JORC).
Historical reserve is the measure of ore reserve that was previously calculated.
Mining companies do Resource Definition Drilling to define the tonnage and grade of deposits. Exploratory holes are drilled to take samples, and the data from the samples is used to create 3-dimensional models of the deposit.
Skarn is the name for the metamorphic rocks surrounding an igneous intrusive where it comes in contact with a limestone or dolostone formation. Skarns are often hosts for copper, lead, zinc, iron, gold, molybdenum, tin, and tungsten ore deposits.
An Intrusive is a body of igneous rock formed by the consolidation of magma intruded into other rocks, in contrast to lavas, which are extruded upon the surface of the earth.
Igneous rocks are formed by the solidification of molten material from far below the earth's surface. Metamorphic rocks have undergone a change in texture or composition as the result of the heat and/or pressure.
Limestone is a bedded, sedimentary deposit consisting chiefly of calcium carbonate.
Dolostone is a sedimentary carbonate rock that contains a high percentage of the mineral dolomite.
Magma is the molten material deep in the Earth from which rocks are formed.
A stockwork system is a system of veins making up a deposit.
Induced Polarisation (IP) is a method of ground geophysical surveying employing an electrical current to determine indications of mineralization.
K-feldspar is widespread and common in a wide variety of igneous and metamorphic rocks and in some sedimentary rocks. Its chemistry and atomic arrangement are variable, so visual properties vary as well.
Chalcopyrite is a sulphide mineral of copper and iron; the most important ore mineral of copper.
Bornite, or Copper Iron Sulfide, is an important copper ore mineral.
Pyrite is a yellow iron sulphide mineral, normally of little value. Also called "fool's gold".
Quartz is a common rock-forming mineral consisting of silicon and oxygen.