000			05349nam a22002057a 4500
005			20251025094100.0
008			251024b ||||| |||| 00| 0 eng d
040			_cSSBUL
050			_a23rd edition, _bT-17 M.Sc.
100			_aKyaw Thu Tun _963384
245			_aGold Mineralization at Pangmalawt area, Kyaukme township, Shan State (North) / _cKyaw Thu Tun
264			_aYangon; _bUniversity of Yangon, _c2012.
300			_a(vii), 85 pages : _bfigures, tables, _c30 cm.
500			_aIncludes list of figures, list of tables, summary, conclusions, appendices
502			_cUniversity of Yangon, _d2012 _aABSTRACT __ The study area is located in Kyaukme Township, Shan State (North), covering about 28 square kilometer. It also lies at the east of the Shan Scarp. Stratigraphically, rock units mainly exposed of Plateau Limestone (Carboniferous), Nyaungbaw Formation (Siluarian), Namhsim Sandstone (Siurian), Pangyun Formation (Cambrain) and Chaungmagyi Group (Precambrian). The Chaungmagyi Group (Precambrian) consists of greywacke, phyllite and slate. Plateau Limestone exposed in the southern and eastern parts of the study area. Nyaungbaw Formation is to be found only at the eastern flank of the metasedimentary unit. It consists mostly of thin to fhick bedded phacoidal limestone. And also, Namshim sandstone consists of fine to medium grained, bluewish brown color on the fresh surface and yellowish to brown color underlying by plateau limestone. In the study area, there is north-south trending fault system which is only one prominent lineament system. In geochemical analysis, Cu, Pb, As, Zn, Au was determined by Atomic Absorption Spectrometer (AAS) method, the precious metal association of gold and silver elements has the lowest values in these veins. The base metal group of copper, lead and arsenic is moderate concentration in the veins. Zinc is also common element of the study area. Mean value and total range for gold is closely associated with silver element. Gold Mineralization occurs in Namshim Sandstone such as sedimentary hosted at North-West of Pangmalawt village. The GPS location of the study area is N 22° 25.602 E 096° 48.564, elevation is 727m near the Maintan Chaung. There is only one new adit in the study area, the direction of adit is 30° and the length of this adit is 6m. There are two types of alternations, especially sericitization and silicification.Sericitization is a prominent alternation in the mineralized zone. It is often associated with a few intensity of silicification. The ore controls can be considered as structural controls, lithologic and stratigraphic controls and source of magmatism is not significant. The mineralization of the study area is generally considered to be probably epithermal sedimentary deposit in the upper zone. The possible age of gold mineralization in Pangmalawt area is post Paleozoic Era. _bM.Sc.
504			_aIncludes references.
505			_rKyaw Thu Tun _tGold Mineralization at Pangmalawt area, Kyaukme township, Shan State (North) / _aCONTENTS __ ABSTRACT ACKNOWLEDGEMENTS CONTENT LIST OF FIGURES LIST OF TABLES CHAPTERS I : INTRODUCTION 1.1 Location, Size and Accessibility 1.2 Phyhsiography 1.3 Climate and Vegetation 1.4 Nature of Exposure 1.5 Purpose of Study 1.6 Methods of Study 1.6.1 Field Methods 1.6.2 Laboratory methods 1.6.3 Previous Works II : REGIONAL GEOLOGY 2.1 Regional Geological Setting III : GEOLOGY OF THE PANGMALAWT AREA 3.1 Chaung Magyi Group 3.1.1 Greywacke 3.2 Pangyun Formation 3.2.1 Schist 3.2.2 Sandstone 3.2.3 Quartzite 3.3 Nyaungbaw Formation 3.3.1 Phacoidal Limestone 3.3.2 Namhsim Sandstone 3.4 Plateau Limestone 3.4.1 Sandy Limestone 3.5 Petrography of the study area 3.5.1 General Statement 3.5.2 Chaung Magyi Group 3.5.2.1 Greywacke 3.5.3 Pangyun Formation 3.5.3.1 Sandstone 3.5.3.2 Quartzite 3.5.3.3 Sericite Schist 3.5.4 Namshim Formation 3.5.4.1 Sandstone 3.5.4.2 Phyllite 3.5.4.3 Quartz sericite schist 3.5.4.4 Sandy phyllite 3.5.5 Naungbaw Formation 3.5.5.1 Phacoidal limestone IV : STRUCTURE 4.1 Regional geological structure 4.1.1 Faults 4.1.2 Folds 4.1.3 Joints V : ALTERATION AND MINERALIZATION 5.1 Type of alteration 5.2 Zone of Alteration 5.3 Nature of Mineralization 5.4 Ore controls 5.5 Geochemical of the study area 5.5.1 Geochemical Investigation 5.5.2 Statistical Treatment of Geochemical Data 5.5.3 The Element Distribution 5.5.3.1 Distribution of Gold (Au) 5.5.3.2 Distribution of Arsenic (As) 5.5.3.3 Distribution of Silver (Ag) 5.5.3.4 Distribution of Copper (Cu) 5.5.3.5 Distribution of Lead (Pb) 5.5.3.6 Distribution of Zinc (Zn) 5.5.4 Cluster analysis of elements association 5.6 XRD analysis 5.7 Mining Methods of the Study Area VI : ECONOMIC ASPECTS 6.1 General economic of the study area 6.2 Zinc anomalous showing 6.3 Other minerals VII : SUMMARY AND CONCLUSIONS REFERENCES APPENDICES
650			_aGeology _xGold mineralization _zPangmalawt area _zKyaukme township _zShan State (North) _963385
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