MILKY WAY INTERNATIONALGhantoot Lease Area,

Nokandi Riko Dik CHAGHIBaluchistan. PAKISTAN

Surface Survey Report of few selected points in the lease area.

Fida Hussain

FTI, SINO PAK MINING fidahunzai1@gmail.comhttp://milkwayinternational.webs.com/

GMM EL 37

Exploration Permission Letter ( EL )

75077.47 Acers (303.83 Km2) Allotted area in Topo sheet.

Export potential of smaller area adjacent to our EL area, surveyed by NL Lake Resources International.

INTRODUCTION OF CHAGHI

     The Chaghi magmatic belt, 480 km. long and 140 km. wide, is an Andean type island arc, bounded by the Chaman-Nushki left lateral, transcurrent fault in the east, Dalbandin-Mir Jawa basin in the south, and Afghan desert in the north.  It extends into Iran beyond the Pakistan-Iran border.  The rocks exposed in the Chaghi belt, in the order of predominance, are volcanic, plutonic and sedimentary.  The oldest rocks exposed in the belt are submarine, stratified volcanic and volcano - clastics, known as the "Sinjrani Group", which are late Cretaceous in age.  The rocks of the group are mainly andesitic lava flows, agglomerates, volcanic conglomerates, tuffs and subordinate limestone, shale and sandstone.  The Chaghi intrusions of younger age are wide spread in the belt and cut the older Sinjrani Group.  These intrusions are granitic, granodioritic, monzonitic, diacritic, tonalitic and gabbroic in composition and range in size from sills, dikes and stocks to batholiths.  The intrusions are from late Cretaceous to Pleistocene in age. 

The Chaghi belt hosts several prospects of metallic mineralization, which include copper, iron, molybdenum and gold.  Porphyry type mineralization is the most important of all the occurrences found in the belt.  At more than twenty localities copper/gold mineralization has been found, of which seven, i.e., Saindak, Koh-i-Dalil, Durban Chah, Kabul Koh, Max G. White, Ziarat Pir Sultan and Dasht –e -Kain, have been proved to be of porphyry type.  Hydrothermal alteration in these porphyry copper prospects is mainly associated with tonalitic and deictic stocks.  The Saindak porphyry copper deposit is at the production stage.  Preliminary investigations of   Dasht -e- Kain and Durban Chah have been undertaken by GSP whereas Koh-i-Dalil has been drill evaluated by TCC/BHB, a multinational Mining Company.  All these porphyry deposits have concentric zonal patterns consisting of potassic, phyllic, and prophylactic alteration zones. Areas, already leased out to companies will not form the subject of the presently proposed exploration program. 

     Like hundreds of porphyry copper deposits of the world, the porphyry copper system of  Chaghi magmatic belt was formed as a result of magmatic associated with subduction of the Arabian oceanic lithosphere under the southern edge of the Afghan micro continent in early Cretaceous (Sinjrani volcanism) and has been active sporadically till Recent (Koh-i-Sultan volcanism).   Iron mineralization is associated with the volcanics and is quite wide spread.  It is high grade and mainly comprises magnetite of magmatic origin. 

N. 28 57’287E. 62 92’490

N. 29 24’56. 37E. 61 17’45.

82

N. 29 01’15 52E. 62 26’01 92

Acres 52263.84 Sq Km 211.46

Iron ore zone

Extension area 92 square km

Cu, au ag

Cu, au , ag,

Iron zone

LANDSCAPE OF THE LEASE AREA.

Surface study of the selected area according to the coordinate from chekandah point M .

Point N

Cut Soils of Ghantoot E L Area.

Surface study of the selected area according to the coordinate from Point G and H

Samples of copper, lead,

pyrite, iron and tantalite

Chekanda iron rich area

Point A of leased area

Complete lease area

Ridges hills with altitude. Metallic zone

POINTS A to M

Cu

Fe

POINT “E”

POINT “K”

GeologyThe mineralized zones are at the western end of the Ghatoot lease, one of the greatmetallogenic area of the world, and which contains some of the world’s richest copper, gold, silverIron, marble, gypsum, Lime stone and some other economically important metal deposits.. These deposits are hosted mainly by met sedimentary rocks of the lateproterozoic Tethyan 7 km thick succession of sediments with minor volcanic,volcanoclastics and intrusive. Geo chronological data indicate an age of deposition of the lease areasediments of about 880 million years. Stratigraphically, the rich copper and cobalt deposits found in Ghantoot lease area. The Lower lease area is composed of sandstones volcanic ashes sulphur granite ironshale's with a basal conglomerate, while the Upper lease area A to L consists essentially of sediments and is separated from the Lower N M by a conglomerate.Within the Riko Dik area large-scale E-W to NW-SE trending folds with wavelengths extendingfor kilometers. The folds are faulted along the crests of the anticlines through which rocks of thearea have been dioptrically injected into the fault zones, squeezed up fault planes and over-thrust tolie above rocks of the younger age. The over-thrust area lithologies occur as segments or“fragments” on surface. The fragments are intact units that preserve the original geologicalsuccession within each. A fragment could be of hundreds of meters aligned across the fault plane.

Reading of Point E and Point K……Ghantoot EL

MineralizationPrimary mineralization, in the form of sulphides, within the Lower lease is associated with the DStart and RSF for the OBI and the SDB and SDS for the OBS and is thought to be sync-sedimentaryin origin. Typical primary copper sulphide minerals are bornite, chalcopyrite, chalcocite andoccasional native copper while cobalt is in the form of carrolite. The mineralization occurs asdisseminations or in association with hydrothermal carbonate alteration and solidification.Supergene mineralization is generally associated with the levels of oxidation in the sub-surfacesometimes deeper than 100 m below surface. The most common secondary supergene minerals forcopper and cobalt are malachite and heterogenite. Malachite is the main mineral mined within theconfines of the current Amirchah point.

General StratigraphyThe generalized stratigraphy of the Ghantoot Lease . The area hasbeen correlated across the A B to H Copperbelt into four main formations or groupings, The divisions between each of the series are often marked by an unconformity. Themain ore-body lithologies belong to the R2 Formation, but R3 and R4 Formations are alsoknown to contain mineralization. Within each of the R series are sub-divisions identifying thedifferent litho logical units. Rocks belonging to the Area Super group are described brieflybelow from the oldest to the youngest:Breech heterogenic or heterogeneous breccias (BH): This breccia is composed of angular and sometimes well rounded fragments of all the various rock types of the Roan. The fragments vary in size from a few millimeters to several tens of millimeters in diameter, while the matrix is made up of finer-grained sandy particles of the same material as the fragments.Breche RAT or brecciated RAT (B RAT): A reddish-pink brecciated rock with calcite and silica vein lets and is at times well mineralized with specular hematite, occurring as veinlets.Roches Argilleuses Talceuse (RAT): The RAT is considered the boundary between the R2and R1 units and consists of an upper RAT Grises (R2) and a lower RAT Lilas (R1). Both are massive but sheared in places, silty or sandy, dolomitic rocks. Mineralization in the form of malachite and black oxides occurs associated with the upper Fe belt.

Dolomie Stratifies or Stratified Dolomite (D Strat): This is a well-bedded to laminated,argillaceous dolomite, which forms the base of the traditional “Lower Ore Zone” inGecamines’ nomenclature. The mineralization consists of copper and cobalt oxides.Roches Siliceuses Feuilletées Foliated (Laminated) and Silicified Rocks (RSF): These aregrey to light-brown, thinly bedded laminated and highly silicified dolomites. The unit isgenerally well mineralized with copper and cobalt oxides. Together with the D Strat, the RSFcomprise the Ore body Inferior (“OBI”).Roches Silicieuses Cellulaires or Siliceous Rocks with Cavities (RSC): Vuggy and in filledmassive to stromatolitic silicified dolomites. Copper mineralization is almost absent in theserocks, which were therefore regarded as barren. However, the infillings are enriched in wad(manganese oxide) and heterogenite (cobalt oxide), and RSC is the target of artisanal activity.Schistes De Base or Basal Schists (SDB): Reddish-brown to grey silty and nodular dolomiteto siltstone. This unit is well mineralized with copper and cobalt in varying amounts andforms the Ore-body Superior (“OBS”).Shales Dolomitiques Superieurs or Upper Dolomitic Shales (SDS): Yellowish, cream-tored,bedded laminated dolomitic siltstones and fine-grained sandstones. The rock is sparselymineralized with malachite.Calcaire a Minerais Noirs or Calcareous Unit with Black Minerals (CMN): A slightlybanded and laminated light-grey to grey, silicified dolomite mineralized with black oxide ofiron, manganese and cobalt. The unit bears some similarities with the RSC.Dipeta (R3): Grayish to dark red or brown stratified shales and micaceous schist.Mwashya (R4): altered stratified redish rock with oolitic horizons huge deposits of Fe andfew bands of light-yellow, cu pockets with resonable deposits.

The presence of two well-Visible deposits nearby Amirchah Point A and Point E, along with at least two other prospects, is a positive indication. The geologic environment of those deposits and prospects could be extrapolated into this area. In my Visit saw abundant hydrothermally altered rocks described as rhyodacites, but which appear to be intrusions on imagery. There is a high proportion of altered rock to the total outcrop area Igneous rocks typical of geologic area containing porphyry copper gold silver and other metallic minerals deposits are common in Lease area between Mashkichah levy post and M/S Gulf Lease area.. All of the lease area is part of the Tethyan geodynamic belt, which contains porphyry copper and other metallic deposits. I delineated 12 permissive tracts for porphyry copper, gold, silver, Iron ore and gypsum deposits . In some cases, the tract is alsopermissive for copper scorn deposits, but I did not make estimates of numbers of undiscovered deposit because the area is huge un accessible by 4 wheel. Some areas need to visit by foot with overnight stay.

The information that is most needed is the complete, interpreted,aeromagnetic data set .

Further exploration require drilling of minimum 8 pits 35 m to 75 m with 3 D survey For drilling points sketch is provided.

The ghantoot lease area consists of pyrrhotite and chalcopyrite with minor cubanite, mackinawite, valleriite, pyrite, marcasite, arsenopyrite, rammelsbergite, sphalerite, tetrahedrite, magnetite, ilmenite, and an unidentified hard anisotropic mineral.

It is the best feasible lease area for the investors. According to surface indications a huge copper, silver and gold deposit with other metallic rich minerals are in bulk quantity. The area of lease is in between one huge and one normal volcanic eruption hub and its result is rich metallic minerals occurrence. Thick layer of volcanic ashes cover the metallic surface only rust of some mineral visible. It is advised that an exploration process through drilling and 3 D survey required.Satellite laser image shows its multi layer deposits of Fe, Cu, marble, gypsum and many more metals. The area is a pearl in the Tethyan belt with concentrate form of mettle and minerals. Compare to Tethyan copper company leased area; the Ghantoot lease area is dense and concentrate. Less efforts and less investment is required for mining of copper, gold silver iron etc compare to other areas in Riko Diq with minimum risk.

Investment opportunity

GOOD BYE

SINO PAK MINING GROUP