The Dingan Gold & Polymetallic Project, Hainan
- The four contiguous exploration permits, totaling 165.4km2, are 100% owned by HT Mining (Beijing) Limited Company;
- The high grade Au-Ag orebodies in the FW Gold Mine, which is encompassed by our properties, is of high grades ranging from 10-200g/t, averaging 52.36 g/t Au, 153.37g/t Ag, with significant Pb-Zn of up to 12%;
- The nearby FW orebodies are up to 650m long, extending from the surface to over 400m in depth. The multiple layers of orebodies occur at very low angle of 10-38 degrees dipping NE;
- The regional and more detailed geochem work have shown strong anomalous of Au¡¢Ag¡¢Cu¡¢Pb¡¢Zn¡¢As¡¢Sb¡¢Hg at large scales. Detailed geophysical work results are interpreted as a granodiorite underlying the sandstones leading to the gold and silver mineralization.
The DingAn gold and polymetallic exploration project is located in DingAn County, which is about 40 km south of Haikou, the capital city of the Hainan Island Province. The main road runs through most of the prospect areas. The four exploration permits of the DingAn gold and polymetallic project of 165.4 km2 are 100% owned by HT Mining (Beijing) Limited Company. We have carried out significant amount of geochemical and geophysical work in the last two years.
The properties are located in the northern part of the Hainan Island, tectonically belonging to the northern Leiming RIFT within in the Wuzhishan Uplift, which is part of the Southern China-Fold. Regional stratigraphy is simple, with Cretaceous sandstone being the main rock unit; and widespread igneous rocks of Permian-Cretaceous age are outcropped in the southwest area. This area has good geological mineralization background for gold, and uranium.
Stratigraphy in the mining area is simple, being the Cretaceous Lumuwan Group; Tertiary basalt cover and some basic dyke intrusions. In the SW area, there are some Mesozoic granites. The structures in the mining area are dominated by three groups trending NW, EW and NNW. The NW-trending group is the fault caused by interlayer sliding, trending NW and dipping NE @ 10¡ã~25¡ã. It¡¯s the major mineralization structure in this area, controls ore body V14¡¢V15¡¢V17 in the nearby FW Mine. The EW-trending group is a group of extending structure obliquely cross the rocks beds; the scale is small and extending is limited, controls ore body V1¡¢V4¡¢V13 in the nearby FW Mine; and dipping North @ 25¡ã~37¡ã. The NWN-trending group is a regional structure. It consists of a number of parallel or intermittent linear distribution fracture zones. The typical one is F2, being a normal fault, up to 440 m long and 1~5 m wide, trending 230¡ãand dipping 78¡ã.
Small granodiorite and granite intrusions of the late Mesozoic age are exposed near the ore bodies V17 and V14 in the FW Mine. The Granodiorite is oval-shaped, the exposed intrusion is some 0.12 km2, and it has intrusive relations with Cretaceous rock units. There are some pyrite (sulfidation?) and auriferous quartz veinlets occur in the inner contact zone. Gold mineralization may have spatial relationships with these intrusions.
In an area of some 5km2, about 20 gold orebodies have been identified by shafts and trenching in the FW mining area, which is encompassed by our four properties. The orebodies mainly occur along the sliding structure betweens the rock layers. They are 70 -650 m long, extending for 360~680 m along the dip, trending 78¡ã and dipping 10-38¡ã. The thicknesses of the orebodies range from 0.13-3.2m. The ores are of high grades ranging from 10-200g/t, averaging 52.36 g/t Au, 153.37g/t Ag, with significant Pb-Zn of up to 12%.
Geochem work has shown regional geochem anomalous in an area of 189.60Km2. More detailed work identified an area of 64 Km2 with high Au-Ag-Cu-Pb-Zn-As-Sb-Hg geochem anomalous. Detailed geophysical gravity and magnetic work suggests that the granodiorite in the SW area should extend underlying the exploration area and the FW Mine area¡£
Both the geochemical and the geophysical data indicate a significant potential to find a large, high grade gold and polymetallic deposit.
Hongling-Junying Cu, Au and Fe-Co Belt Project
- The three exploration permits, namely Hongling, Junying and Hongtianqidui, are totaling 60.48km2, and 100% owned by HT Mining (Beijing) Limited Company;
- The Pingyuancun Cupper Prospect is of high grade copper averaging over 1% copper with some 10-20g/t Ag, showing the characteristics of ¡°sandstone hosted copper¡± with very significant potential;
- he Junying Fe-Co Prospect contains significant Fe-Co orebodies, it in a belt parallel to, and only 20km from the high grade, large Shi Lu Iron Mine belt. The mineralization is widely spread in the Carboniferous meta-sedimentary rocks, and may be also related to a nearby andisite. All the characteristics of tectonic background, the host rock unit, and particularly the Fe-Co association with local high Cu, are comparable with the Shi Lu Iron Deposit. There is great potential to find a big Fe-Co deposit as indicated by the magnetic anomalous;
- he Hongling Iron Prospect occurs in the pre-Devonian meta-sedimentary rocks. The ore grade ranges 40.26%-67.12% total Fe. There are wide-spread iron mineralization in the whole Hongling-Junying area, therefore, there is the potential to find a large scale iron deposit in the area;
- he Hongling Gold Prospect is hosted in the Silurian phyllite. Our detailed geochem work indicates strong geochem anomalous of Au-Ag-As-Sb. Further geological mapping and trenching have discovered some auriferous quartz vein systems.
The Hongling-Junying Cu-Au-Fe-Co exploration project is located in Zhanzhou area, some 160km SW of Haikou, the capital city of the Hainan Island Province. The main roads run through most of the prospect areas. The two exploration permits of the Hongling-Junying Cu-Au-Fe-Co project, totaling of 53.8km2, are 100% owned by our HT Mining (Beijing) Limited Company. We have been carrying out significant geochemical and geophysical work as well as significant trenching and drilling work since 2006.
The properties are located in the western part of the Hainan Island, tectonically belonging to the NW of Wuzhishan Fold-Belt, and in eastern part of the Junying fault graben. The main rock units are the pre-Devonian silica-carbonate sedimentary rocks, actinolites, and meta-dolomite, hosting the Hongling iron deposit and the Pinyuancun copper deposit; the Silurian phyllite hosting the Hongling gold mineralization; and the Carboniferous meta-sedimentary rocks hosting Fe-Co orebodies.
There is a Variscan Junying diorite (293 Ma) in the eastern part of the prospecting area near the major Fe-Co mineralization. Strong magnetic geophysical anomalous is spatially related to the Fe-Co mineralization. The iron mineralization is wide-spread; the iron orebodies are normally composed by 6-7 layers, totaling 15-70m in thickness, 50-170m long and extending for over 200m along the dip. The Fe grade is normally 50.5-59.5%. The Co orebodies appear to be spatially associated with the iron orebodies, normally within 30m of the footwalls and the hanging walls of the iron orebodies; they occur in the fractured rocks as veins, 65-170m long, and up to 6.4m wide. The Co contents are typically of 0.08-0.15%. All the characteristics of tectonic background, the host rock unit, and particularly the Fe-Co association with local high Cu, are comparable with the Shi Lu Iron Deposit. There is great potential to find a large Fe-Co deposit of the Shi Lu Iron Deposit type.
The Pingyuancun copper deposit occurs in the bottom part of the Carboniferous dolomite, which has been strongly silicified. Some trenching and aditing work discovered the orebody of some 10m wide. The orebody has been traced for over 60m along an adit previously dug by local people. The ores contain about 4-5% Cu with 8-25 g/t Ag, and there appears to be a normal correlation between the contents of copper and silver. The geological and elemental characteristics suggest the Pingyuancun deposit may be the type of ¡°sandstone hosted copper¡±. Therefore, there is a potential to find major copper mineralization in the silicified carbonate rock and in the underlying red sandstones.
The Hongling gold mineralization occurs in the Silurian Tuolie phyllite. The significant Baolun Gold Deposit, which contains over 2Moz gold of high grade, occurs in the same rock units. Detailed geochem work identified strong geochem anomalous of Au, Ag, As and Sb in this area. The follow up geological mapping and trenching discovered some auriferous quartz veins. The potential may be significant.
Please contact us for enquiries or would like to express interest in the project.
Very Prospective Gold & Silver Projects In China
Details of the Project (AKZ):
- We have a Framework Agreement with the permit owner, and have finished a three months pre-feasibility study on the property;
- The project comprises two exploration permits totaling ~20 km2;
- Many auriferous quartz vein systems have been identified by systematic geochemical and geophysical work and surface trenching along a 7 km long and 2km wide NW trending shear zone including four major orebodies;
- A small testing shaft was sunk from the surface to approximately 200m in depth at one of the orebodies. The quartz vein becomes wider and higher grade in depth: e.g. 5m wide averaging @ 13.59g/t at 120-140m deep; and about 7m wide averaging @ 29g/t at around 170m depth.
We collected two rock chips samples from the surface waste dump near the shaft. One sample has 5.5g/t Au; and the other contains 54.7g/t Au, 41.3g/t Ag and 4.63% Pb. Also, the alteration we observed from the rocks near the shaft is green mica-ankerite-silicification, very pervasive.
This project needs be financed in a restricted time frame and we are negotiating with a few potential investors. Should any party be interested in this very prospective project, please contact us ASAP while the opportunity lasts!
The PS Ag-(Au) field in NE China comprises an area of approximately 58 km2 including two deposits and three prospects.
Limited work identified over 9,000,000t ores of averaging 190-290g/t Ag and 1.24-2.00g/t Au, i.e. over 2000t Ag and some 10t Au. One of the major orebodies averages 4m wide, and extends up to 2km long.
The alteration zone of the mineralization is a few 10s of meters wide, and extends for 14km. The main structure in the Ag-Au field is NNE, however, in the south of the field, the major NNE structure appears to be replaced by NS structures. Most of the orebodies contain 1-2g/t gold. There are a few gold prospects in the filed with some Hg anomalous.
Sino-QZ Group has signed a LOI with the local geological brigade, and welcomes investors for the very prospective silver-gold project.
The HY exploration project is located in NW of China. It directly surrounds two main gold deposits enclosing an area of some 30km2. The YZS deposit is one of the most significant new discoveries of high-grade gold deposit by the provincial Bureau, with milling grade over 9g/t. The other deposit is of broad alteration and mineralization zone with multiple vein systems. The potential for new discovery of both large and high-grade gold resources is significant.
The PGMB has agreed that Sino-QZ Group shall bring a third party for a JV of the exploration region directly around the two mines, ie about 30km2 exploration permit. According to the meeting with the Directors and Geo Division Chief of the PGMB, Sino-QZ Group will pay some money to gain 3 months exclusive right for evaluating the property, and negotiating for a possible JV.
The gold deposit is located along a major regional shear zone. From north to the south seven gold deposits occur along the major shear zone. The provincial Bureau has carried out 1:10,000 scale geological mapping and soil geochemistry for the entire region, the work also includes some trenching, drilling and a card measurement. Two major gold ore zones comprising 10 main orebodies have been identified. Over three quarters of Milt ores @ average 5.10g/t resources have been identified by the limited work. The grade normally varies between 3 and 10 g/t, up to 177.80 g/t. The mineralization is controlled by regional NE-trending shear zones, and hosted in the sub-structures of NE-trending mylonized and faulted alteration zones. Most of the orebodied are under the overburden, the orebodies are generally thin on the top, and become thicker in depth.
The Provincial Bureau has agreed that Sino-QZ Group will finance or bring a third party for a JV of the exploration region, i.e. about 12.78km2 exploration permit. According to the meeting with the Directors and Chief Geo of the PB, Sino-QZ Group will gain 1-3 months exclusive right for evaluating the property, and negotiating for a possible JV.
This is a grassroots project, with significant potential. The main geological works has been done includes regenal 1:50,000 scale stream sediments geochem, and 1:10,000 scale geological mapping. 43 geochemical anomalous of Aus, Ag, Cu, Pb, Zn, Sb, As and Bi have been identified in the regional work, 7 of them with good potentials. In the prospect area, gold anomalous normally ranges 50ppb-2ppm, up to 10ppm gold. In the highest anomalous area of 16km2 gold values varies normally between 0.5-3ppm. The mineralization appears to be controlled by the fractures and faults along the layers and schistoses of the slate belt and phyllite. Most of the gold-quartz veins occur in strongly faulted rocks. In the direct adjacent area a gold deposit of high grade has been found by limited exploration work recently. Twelve auriferous veins haven found in the deposit, normally are 20-50m long 0.5-3.0m wide. The grade ranges 1-38.77 g/t, averaging 9.41g/t.
The owner has agreed that Sino-QZ Group will finance or bring a third party for a JV of the exploration WX region, i.e. about 54.39km2 exploration permit. According to the meeting with the Directors and Chief Geo, Sino-QZ Group pays PGEI some money to gain 1-3 months exclusive right for evaluating the property, and negotiating for a possible JV.
Please contact us for enquiries or would like to express interest in the project.
8 NOV 2008 // Beijing, CHINA
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