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04584nam a22002057a 4500 |
| 005 - DATE AND TIME OF LATEST TRANSACTION |
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20251023160659.0 |
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| 040 ## - CATALOGING SOURCE |
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| Transcribing agency |
SSBUL |
| 082 ## - DEWEY DECIMAL CLASSIFICATION NUMBER |
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| Edition number |
23rd edition, |
| Classification number |
T-13 M.Sc. |
| 100 ## - MAIN ENTRY--PERSONAL NAME |
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| Personal name |
Chit Ye Naung Htet |
| 9 (RLIN) |
63334 |
| 245 10 - TITLE STATEMENT |
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| Title |
Geology and tin mineralization of Kanzan area, Phekhon township, Shan State (South) / |
| Statement of responsibility, etc. |
Chit Ye Naung Htet. |
| 264 ## - PRODUCTION, PUBLICATION, DISTRIBUTION, MANUFACTURE, AND COPYRIGHT NOTICE |
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| Place of production, publication, distribution, manufacture |
Yangon; |
| Name of producer, publisher, distributor, manufacturer |
University of Yangon, |
| Date of production, publication, distribution, manufacture, or copyright notice |
2018. |
| 300 ## - PHYSICAL DESCRIPTION |
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| Extent |
(x), 68 pages : |
| Other physical details |
figures, tables, |
| Dimensions |
30 cm. |
| 500 ## - GENERAL NOTE |
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| General note |
Includes list of figures, list of tables, summary, conclusion, appendices. |
| 502 ## - DISSERTATION NOTE |
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| Dissertation note |
ABSTRACT_ The study area is located near Kanzan village, about 89km south-west of Loikaw City, Kayah State. The Mergui Group is widely distributed around the study area. In this unit, the prominent rock is sandstone and phyllite. Muscovite Granite intrudes the metasediments of the Mergui Group. The major Shan Scarp Fault, N-S trending longitudinal fault, runs in the western part of the study area, In the study area, metasedimentary rocks of Mergui Group and granite are well exposed. The metasedimentary rocks ard sandstone, siltstone and phyllite. Sandstone is fine-to medium-grained and granular texture. It is composed of quartz, orthoclase and opaque minerals. Silstone is fine-grained and composed of quartz, feldspar, mica and opaque minerals.Pyhllite is fine-grained and foliated. Granite is medium-to coarse-grained hypidiomorphic granular texture. It is mainly composed of quartz, orthoclase, plagioclase and muscovite. The common types of alteration associated with Sn mineralization in Kanzan area are greisenization, silicification, sericitization and kaolinization. The mineralization style of the Kanzan deposit is designated as vein type deposit which is hosted by the muscovite granite and metasedimentary rocks. The nature of distribution of the ore minerals in Kanzan Sn mineralization is represented by the quartz veins which contains cassiterite, pyrite ,chalcopyrite, arsenopyrite and sphalerite. Cassiterite, arsenopyrite and pyrite are early formed minerals in the vein system and late stage of the vein in represented by the chalcopyrite and sphalerite. Tin abundances range from 250ppm to 18.99% and tungsten content is from 620 ppm to 1.60% Tin is positively correlated with tungsten and copper. However, tin is negatively correlated with arsenic and rubidium. According to the mineralizations style, ore microscopic study and geochemical data, Sn mineralization of Kanzan area is associated to the granite related hydrothermal mineral system. |
| Degree type |
M.Sc |
| Name of granting institution |
University of Yangon. |
| Year degree granted |
2018. |
| 504 ## - BIBLIOGRAPHY, ETC. NOTE |
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| Bibliography, etc. note |
Includes references. |
| 505 ## - FORMATTED CONTENTS NOTE |
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| Formatted contents note |
CONTENTS _ <br/>ABSTRACT <br/>ACKNOWLEDGEMENTS <br/>CONTENTS <br/>LIST OF FIGURES <br/>LIST OF TABLES <br/>CHAPTER I : INTRODUCTION <br/> 1.1 Location, Size and Accessibility<br/> 1.2 Physiography and Drainage <br/> 1.3 Purposes of Study <br/> 1.4 Methods of Study <br/> 1.4.1 Field work <br/> 1.4.2 Laboratory work <br/> 1.5 Previous Work <br/>CHAPTER II : REGIONAL GEOLOGY SETTING <br/> 2.1 General Statements <br/> 2.2 Regional Geology <br/> 2.2.1 Plateau Limestone Group <br/> 2.2.2 Mergui Group <br/> 2.2.3 Pindaya Group <br/> 2.2.4 Mogok Metamorphic Belt <br/> 2.2.5 Central Granitoid Belt <br/> 2.3 Regional Structures <br/> 2.3.1 Sagaing Fault <br/> 2.3.2 Kyaukkyan Fault<br/> 2.3.3 Shan Scarp Fault <br/>CHAPTER III : GEOLOGY OF THE STUDY AREA <br/> 3.1 General Geology of Kanzan Area <br/> 3.2 Mergui Group <br/> 3.3 Granite <br/> 3.4 Geological Structures of the Study Area <br/>CHAPTER IV : PETROGRAPHY <br/> 4.1 General Statements <br/> 4.2 Metasedimentary Rocks <br/> 4.2.1 Sandstone <br/> 4.2.2 Silstone<br/> 4.2.3 Phyllite <br/> 4.3 Granite <br/>CHAPTER V : ALTERATION AND MINERALIZATION <br/> 5.1 Alteration <br/> 5.1.1 Greisenization <br/> 5.1.2 Silicification <br/> 5.1.3 Sericitization <br/> 5.1.4 Kaolinization <br/> 5.2 Mineralization <br/>CHAPTER VI : OREMINERALOGY <br/> 6.1 Introduction <br/> 6.2 Ore Mineralogy <br/> 6.2.1 Cassiterite <br/> 6.2.2 Pyrite <br/> 6.2.3 Chalcopyrite <br/> 6.2.4 Sphalerite <br/> 6.2.5 Arsenopyrite <br/> 6.3 Paragenetic Sequence <br/>CHAPTER VII GEOCHEMISTRY <br/> 7.1 General Statements <br/> 7.2 Interpretation of Geochemical Data <br/> 7.3 Regression Analysis of Associated Elements <br/> 7.4 Correlation Coefficients of the Study Area<br/> 7.5 Cluster Analysis <br/>CHAPTER VIII : SUMMARY AND CONCLUSION <br/>REFERENCES <br/>APPENDICES. <br/> |
| Statement of responsibility |
Chit Ye Naung Htet. |
| Title |
Geology and tin mineralization of Kanzan area, Phekhon township, Shan State (South) / |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM |
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| Topical term or geographic name entry element |
Geology |
| General subdivision |
Tin mineralization |
| Geographic subdivision |
Kanzan area |
| -- |
Phekhon township |
| -- |
Shan State (South) |
| 9 (RLIN) |
63335 |
| 942 ## - ADDED ENTRY ELEMENTS (KOHA) |
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| Source of classification or shelving scheme |
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| Koha item type |
Reference |