1. Introduction
2. Mineral Occurrences in Myanmar
3. Current Mining Activity in Myanmar
4. Investment Information
I-Procedure for Foreign Investment in Mining Sector
II-Tex Regime and Royalty in Mining Sector
III-Category of Mining Permits
5.Why You Investment in Mining Sector in Myanmar
6.Conclusion
COLLECTION FOR MYANMAR GEOLOGY STUDENTS AND LEARNERS-1MYO AUNG Myanmar
COLLECTION FOR MYANMAR GEOLOGY STUDENTS AND LEARNERS-1
Geology of the High Sulfidation Copper Deposits, Monywa Mine, Myanmar
Andrew H. G. Mitchell Win Myint Kyi Lynn Myint Thein Htay Maw Oo Thein Zaw
Resource GeologyVolume 61, Issue 1
First published: 22 December 2010
https://onlinelibrary.wiley.com/doi/epdf/10.1111/j.1751-3928.2010.00145.x
Active tectonics and earthquake potential of the Myanmar region
Yu Wang Kerry Sieh Soe Thura Tun Kuang‐Yin Lai Than Myint
Journal of Geophysical Research: Solid EarthVolume 119, Issue 4
First published: 15 March 2014
https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1002/2013JB010762
Myanmar's Mining Industry Dr. Neal Reynolds Director Exploration & Evaluation...MYO AUNG Myanmar
This document provides an overview and assessment of Myanmar's mining industry, mineral potential, and operating framework. Key points:
- Myanmar has a long history of mining but production declined after independence and nationalization. The industry remains underdeveloped relative to potential.
- Minimal past exploration means the mineral potential is largely unrecognized, but Myanmar is prospective for gold, copper, zinc, tin, nickel and other commodities based on its tectonic setting and deposits in surrounding areas.
- Attracting exploration investment will require reforms to incentivize high-risk exploration through changes to the mining law regarding production sharing contracts and licensing terms.
- Understanding Myanmar's complex tectonic evolution is
This document discusses the geology and mineral resources of Myanmar. It provides background on the tectonic setting resulting from the collision of the Indian and Asian plates. It describes the major geological features of Myanmar including sedimentary basins, magmatic belts, and metamorphic belts. It also summarizes the country's major mineral provinces and key mineral deposits such as tin-tungsten, lead-zinc-silver, and jade. Maps are included showing the distribution of these major deposit types across Myanmar.
South east asia minerals & energy resourcesMasuda Sultana
The document provides information about the minerals and energy resources of Southeast Asia. It discusses the major ferrous, non-ferrous and precious stone resources found in the region. For ferrous resources, it outlines the iron ore reserves and production levels in countries like Malaysia, Vietnam, Indonesia, Laos, Philippines and Thailand. It also discusses the nickel reserves mainly found in Indonesia and Philippines. Chromium reserves are noted in Philippines, Myanmar and Vietnam. For non-ferrous resources, it summarizes the copper reserves and mines in Philippines, Myanmar, Indonesia and Laos.
WA STATE(MYANMAR) MINERAL DEPOSIT AND EXPRESS WAY R3W (KUNMING-WA STATE-BANGKOK)MYO AUNG Myanmar
WA STATE(MYANMAR) MINERAL DEPOSIT AND EXPRESS WAY R3W (KUNMING-WA STATE-BANGKOK)
DESCRIPTION: WA SET UP TIN MINE EXPORT TO CHINA and KUNMING-BANGKOK HIGHWAY ROUTE R3W ON WA STATE WA state in Myanmar set up Tin Mine in Nuoba District support by CHINESE Geological exploration WA state in Myanmar support by CHINA to do Route on KUNMING-BANGKOk HIGH WAY ROUTE R3W WA STATE IN MYANMAR HAVE REE RARE EARTH ELEMENTS DEPOSIT AND CHINESE REMINING ! ENVIRONMENT CAN BE PROBLEM.
The document discusses trends in mineral prospecting in India from 2004-2007. It summarizes that base metals, gold-diamond-bearing rocks, and atomic minerals received the most attention. Iron ore, manganese, bauxite and chromite deposits were also studied significantly. Demand increased prospecting for coal and lignite. The document describes the geological settings and formation processes of various mineral deposits in India, including their locations, for base metals, gold, diamond, iron, manganese, chromite, uranium, molybdenum, tungsten and coal.
Myanmar known until recently as Burma, is slowly but steadily starting to attract foreign investment, driven mainly by international resource firms eager to tap into the mineral-rich South East Asia's country. After more than half a century of military ruling, Burma has started benefitting from the recent suspension of sanctions by Canada, the United States and the European Union. Myanmar's gold production is increasing and could prove a key factor for the country's economic growth, but many gold miners are suffering from lung diseases due to inadequate equipment and antiquated practices. In mineral-rich areas of Kachin State, taxes from Burmese and Chinese gold mining provides an important income stream to the Kachin Independence Organization. However, these mining companies use mercury in an environmentally hazardous extraction process, which can lead to long-lasting damage for the area's forests and river ways.
This document discusses mining in the Philippines, including its history and current state. It notes that mining dates back to the 16th century and provides a significant economic contribution today. However, it also causes environmental degradation and issues with safety, processing, and community health/conditions. There are also policy issues around overlapping mining claims, revenue sharing, and outdated small-scale mining laws. The document focuses on small-scale mining by the Monte de Oro Small Scale Miners' Association, outlining their vision, mission, goals and objectives which center around responsible mining and improving livelihoods.
COLLECTION FOR MYANMAR GEOLOGY STUDENTS AND LEARNERS-1MYO AUNG Myanmar
COLLECTION FOR MYANMAR GEOLOGY STUDENTS AND LEARNERS-1
Geology of the High Sulfidation Copper Deposits, Monywa Mine, Myanmar
Andrew H. G. Mitchell Win Myint Kyi Lynn Myint Thein Htay Maw Oo Thein Zaw
Resource GeologyVolume 61, Issue 1
First published: 22 December 2010
https://onlinelibrary.wiley.com/doi/epdf/10.1111/j.1751-3928.2010.00145.x
Active tectonics and earthquake potential of the Myanmar region
Yu Wang Kerry Sieh Soe Thura Tun Kuang‐Yin Lai Than Myint
Journal of Geophysical Research: Solid EarthVolume 119, Issue 4
First published: 15 March 2014
https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1002/2013JB010762
Myanmar's Mining Industry Dr. Neal Reynolds Director Exploration & Evaluation...MYO AUNG Myanmar
This document provides an overview and assessment of Myanmar's mining industry, mineral potential, and operating framework. Key points:
- Myanmar has a long history of mining but production declined after independence and nationalization. The industry remains underdeveloped relative to potential.
- Minimal past exploration means the mineral potential is largely unrecognized, but Myanmar is prospective for gold, copper, zinc, tin, nickel and other commodities based on its tectonic setting and deposits in surrounding areas.
- Attracting exploration investment will require reforms to incentivize high-risk exploration through changes to the mining law regarding production sharing contracts and licensing terms.
- Understanding Myanmar's complex tectonic evolution is
This document discusses the geology and mineral resources of Myanmar. It provides background on the tectonic setting resulting from the collision of the Indian and Asian plates. It describes the major geological features of Myanmar including sedimentary basins, magmatic belts, and metamorphic belts. It also summarizes the country's major mineral provinces and key mineral deposits such as tin-tungsten, lead-zinc-silver, and jade. Maps are included showing the distribution of these major deposit types across Myanmar.
South east asia minerals & energy resourcesMasuda Sultana
The document provides information about the minerals and energy resources of Southeast Asia. It discusses the major ferrous, non-ferrous and precious stone resources found in the region. For ferrous resources, it outlines the iron ore reserves and production levels in countries like Malaysia, Vietnam, Indonesia, Laos, Philippines and Thailand. It also discusses the nickel reserves mainly found in Indonesia and Philippines. Chromium reserves are noted in Philippines, Myanmar and Vietnam. For non-ferrous resources, it summarizes the copper reserves and mines in Philippines, Myanmar, Indonesia and Laos.
WA STATE(MYANMAR) MINERAL DEPOSIT AND EXPRESS WAY R3W (KUNMING-WA STATE-BANGKOK)MYO AUNG Myanmar
WA STATE(MYANMAR) MINERAL DEPOSIT AND EXPRESS WAY R3W (KUNMING-WA STATE-BANGKOK)
DESCRIPTION: WA SET UP TIN MINE EXPORT TO CHINA and KUNMING-BANGKOK HIGHWAY ROUTE R3W ON WA STATE WA state in Myanmar set up Tin Mine in Nuoba District support by CHINESE Geological exploration WA state in Myanmar support by CHINA to do Route on KUNMING-BANGKOk HIGH WAY ROUTE R3W WA STATE IN MYANMAR HAVE REE RARE EARTH ELEMENTS DEPOSIT AND CHINESE REMINING ! ENVIRONMENT CAN BE PROBLEM.
The document discusses trends in mineral prospecting in India from 2004-2007. It summarizes that base metals, gold-diamond-bearing rocks, and atomic minerals received the most attention. Iron ore, manganese, bauxite and chromite deposits were also studied significantly. Demand increased prospecting for coal and lignite. The document describes the geological settings and formation processes of various mineral deposits in India, including their locations, for base metals, gold, diamond, iron, manganese, chromite, uranium, molybdenum, tungsten and coal.
Myanmar known until recently as Burma, is slowly but steadily starting to attract foreign investment, driven mainly by international resource firms eager to tap into the mineral-rich South East Asia's country. After more than half a century of military ruling, Burma has started benefitting from the recent suspension of sanctions by Canada, the United States and the European Union. Myanmar's gold production is increasing and could prove a key factor for the country's economic growth, but many gold miners are suffering from lung diseases due to inadequate equipment and antiquated practices. In mineral-rich areas of Kachin State, taxes from Burmese and Chinese gold mining provides an important income stream to the Kachin Independence Organization. However, these mining companies use mercury in an environmentally hazardous extraction process, which can lead to long-lasting damage for the area's forests and river ways.
This document discusses mining in the Philippines, including its history and current state. It notes that mining dates back to the 16th century and provides a significant economic contribution today. However, it also causes environmental degradation and issues with safety, processing, and community health/conditions. There are also policy issues around overlapping mining claims, revenue sharing, and outdated small-scale mining laws. The document focuses on small-scale mining by the Monte de Oro Small Scale Miners' Association, outlining their vision, mission, goals and objectives which center around responsible mining and improving livelihoods.
1. The document discusses exploration of the Mubda chromite deposit located in Samail Wilayat, Sultanate of Oman.
2. Fieldwork was conducted over 16 days to investigate the geology, geomorphology, and slopes of the area using topographic data.
3. Chemical analysis and geophysical methods revealed the rocks have a high chromite content and the deposits are generally located in dunite bodies. The entire area was found to have potential for economic chromite mining.
Mineral Deposits of SE Asia: Lessons for Myanmar from Adjacent -Dr Stuart Smi...MYO AUNG Myanmar
http://www.owenhegarty.com/wp-content/uploads/TigersStuart1.pdf
Presentation Outline
The Big Picture – Plate Tectonics
Mineral prospectivity is a function of plate tectonic setting
Myanmar has unusual and highly favourable tectonics
It shares tectonics with mainland Asia and Sumatra
The Concept of Mineral Deposit Models and Mineral Provinces
The mechanisms of mineral deposit formation are relatively well understood
Models derived from this understanding guide mineral exploration
Mineral deposits form provinces that reflect their tectonic setting
Details of selected mineral belts and deposits in adjacent regions
The mineral belts of adjacent regions are relatively well known
This knowledge can be transferred into Myanmar
Synthesis
Prospectivity & potential deposit styles in Myanmar
The document discusses sandstone uranium deposits found in the Phu Wiang Basin in Thailand. Three small uranium ore lenses were discovered through drilling programs in the 1970s-1980s. The mineralization is low-grade and consists primarily of coffinite dispersed in conglomeratic sandstone layers. Though additional prospecting occurred, the deposits were deemed uneconomic due to small size, low grades, and finely dispersed nature of the uranium minerals. Discoveries of dinosaur fossils during drilling provided benefits to museums, but further exploration found only uneconomic uranium occurrences in the region.
Myanmar has significant mineral potential across its four main geological belts. The document outlines Myanmar's geology, mineral provinces, current exploration and production activities for minerals such as gold, platinum, uranium, and rare earth elements. Future joint exploration programs with Japan are planned to target tin, tungsten, antimony, mineral sands, and rare earth elements. Requirements for foreign investment in Myanmar's mining industry including licenses, infrastructure needs, environmental protections, and corporate social responsibility are also discussed.
Myanmar is rich in mineral wealth. But it still left much of the virgin lands which are remote, mountainous and rugged. Much will be find. Mineral database is not well established and complete yet.
This document provides an overview of mineral resources and database building efforts in Myanmar. It describes the organization of the Ministry of Mines and its departments responsible for geological survey, mineral exploration, and mining enterprises. It then summarizes the major known mineral occurrences in Myanmar, including deposits of copper, iron, lead, zinc, silver, and nickel. The document concludes by outlining plans to develop a comprehensive mineral database for Myanmar to support further exploration and development of the country's mineral resources.
This is an abstract from the 5th Annual Minerals South Conference & Tradeshow of October 2009 in Cranbrook, British Columbia.
The subject is the Wicheeda rare earth carbonatite being explored by Spectrum Mining Corp.
Myanmar The Black Swan of Global Tin - Gardiner & Sykes - May 2015 - ITRI Con...John Sykes
Myanmar has emerged as the third largest producer of tin globally due to production from the Man Maw mining district in Wa State. However, production comes from an area outside of Myanmar's traditional tin producing regions and many questions remain regarding reserves, infrastructure, and political stability. While Myanmar has huge untapped mineral potential, it remains a high-risk jurisdiction. Further development of the mining industry could significantly help Myanmar's economy if issues of transparency, environment, and the upcoming elections and mining law changes are successfully addressed.
Myanmar known until recently as Burma, is slowly but steadily starting to attract foreign investment, driven mainly by international resource firms eager to tap into the mineral-rich South East Asia's country. After more than half a century of military ruling, Burma has started benefitting from the recent suspension of sanctions by Canada, the United States and the European Union. Myanmar's gold production is increasing and could prove a key factor for the country's economic growth, but many gold miners are suffering from lung diseases due to inadequate equipment and antiquated practices. In mineral-rich areas of Kachin State, taxes from Burmese and Chinese gold mining provides an important income stream to the Kachin Independence Organization. However, these mining companies use mercury in an environmentally hazardous extraction process, which can lead to long-lasting damage for the area's forests and river ways.
The document summarizes trends in mineral prospecting in India from 2004-2007. It discusses several important mineral deposits in India such as base metals like copper, lead, and zinc. It also discusses precious metal deposits of gold and diamond, located primarily in greenstone belts and carbonate rocks. Major ferrous deposits of iron ore are described along with chromite, manganese, and uranium deposits. Locations, geological settings, and formation processes are provided for several of these important mineral deposits in India.
x-geo-Minerals and Energy Resources-mod1-ppt.pptx4X2GAMING
The document discusses minerals and energy resources in India, including what minerals are, how they are formed and occur, how mining works, major mineral deposits and producing regions in India, and key ferrous minerals like iron ore and manganese. It provides details on the classification, production, and uses of important minerals like iron ore and manganese, as well as the leading producing states for these minerals in India.
Manganese ore deposits are widely scattered in various districts in Egypt.
They occur at some localities in Sinai Peninsula and at a few localities in the Eastern Desert.
Manganese deposits are known:
in the Um Bogma district in west central Sinai; and
in the Halaib "Elba" district in the southern portion of Eastern Desert.
In addition, minor occurrences are known in Wadi Mialik near Abu Ghosun and Ras Banas in the Southern Eastern Desert, and Wadi Abu Shaar El Qibli (Black Hill), to the north of Hurghada
This document provides an overview of uranium exploration and mining case studies in Nigeria, including:
- Uranium was discovered in the 1970s in the northeast region through exploration projects conducted by the Nigerian Uranium Mining Company.
- Four main uranium deposit areas were discovered - Gumchi, Gabrunde, Mika, and Mayo-Lope. Drilling and sampling was conducted at these sites to determine average uranium concentrations and reasonably assured resource estimates ranging from 50 to 100 tons of uranium oxide.
- The geology of Nigeria consists of a basement complex and younger granites upon which sedimentary basins were deposited. Uranium mineralization is hosted in granitic rocks and
Metallogenic Epoch and Province
Metallogenetic Epochs
Metallogenetic epochs, as defined above, are specific periods characterised by formation of large number of mineral deposits. It does not mean that all the mineral deposits formed during a definite metallogenetic epochs. In India the chief metallogenetic epochs were:
1. Precambrian
2. Late Palaeozoic
3. Late Mesozoic to Early Tertiary
massive type interlayer with gabbroic rocks in the Eastern Desert; Main occurrences of Ti-Fe oxide deposits in Egypt; Abu Ghalaga Ore Deposit; Abu Ghalaga ilmenite ore deposit categories ; Abu Ghalaga Mineral composition; Mining Techniques; Origins; Korabkanci titano-magnetite ore; black sand placer deposits type; Rosetta (or Rashid East); Northern Sinai Coast
The document analyzes heavy mineral sands ore deposits along the coast of Somaliland. Analysis using XRF, XRD, and SEM-EDS techniques revealed high concentrations of titanium and iron bearing minerals like ilmenite, rutile, and titaniferous magnetite. The mineral assemblages varied between east and west Somaliland, depending on the underlying geology. The east is dominated by quartz and titanium minerals from Proterozoic basement rocks, while the west contains more ilmenite, rutile, and mica from high-grade metamorphic and Miocene volcanic rocks. The heavy mineral deposits have potential to provide commercially important minerals like ilmenite.
The document provides information on limestone deposits in India and Tamil Nadu. It finds that South and West zones of India contain the major limestone reserves, accounting for 68% of the country's total. Within the South zone, Andhra Pradesh and Karnataka contain over 55% of the reserves. In Tamil Nadu, limestone deposits are found across multiple districts and taluks, with major occurrences in Tirunelveli, Tuticorin, Virudhunagar, Madurai, Coimbatore, Karur, Namakkal, Salem, and Tiruchirappalli districts. The document outlines the geological nature and locations of the key limestone deposits in each area.
The Tectonic and Metallogenic Framework of MyanmarMYO AUNG Myanmar
https://research-repository.st-andrews.ac.uk/bitstream/handle/10023/10689/Cawood_2016_Myanmar_OGR_AM.pdf?sequence=1
The Tectonic and Metallogenic Framework of
Myanmar: A Tethyan Mineral System
Nicholas J. Gardiner1,9*
, Laurence J. Robb1
, Christopher K. Morley2,3
,
Michael P. Searle1
, Peter A. Cawood4
, Martin J. Whitehouse5
,
Christopher L. Kirkland6
, Nick M.W. Roberts7
, Tin Aung Myint8
1. Department of Earth Sciences, University of Oxford, Oxford OX1 3AN, United
Somaliland has significant unexplored mineral potential. The mining sector is still small, with only artisanal mining currently occurring. The country possesses deposits of gold, platinum, iron, copper, tin, gemstones, and other industrial minerals. However, large areas remain unexplored due to a lack of geological surveys. Somaliland desires to develop its mining industry but faces challenges in attracting investment and building institutional capacity for resource management and data collection.
02 Mugumbate - Overview of mineral potential (1).pdfLeonNdiraya1
- Zimbabwe has significant unexplored mineral potential based on its geological formations like greenstone belts and the Great Dyke that are known to host valuable resources. However, challenges like political instability, lack of investment, and outdated exploration techniques have limited understanding of the size and distribution of resources.
- With modern exploration methods and a stable investment environment, it is likely that many currently small deposits could become large mines and many new deposits could be discovered, particularly for commodities like gold, platinum, chromium, and coal. The mineral endowment of Zimbabwe may be much larger than currently recognized.
The use of Nauplii and metanauplii artemia in aquaculture (brine shrimp).pptxMAGOTI ERNEST
Although Artemia has been known to man for centuries, its use as a food for the culture of larval organisms apparently began only in the 1930s, when several investigators found that it made an excellent food for newly hatched fish larvae (Litvinenko et al., 2023). As aquaculture developed in the 1960s and ‘70s, the use of Artemia also became more widespread, due both to its convenience and to its nutritional value for larval organisms (Arenas-Pardo et al., 2024). The fact that Artemia dormant cysts can be stored for long periods in cans, and then used as an off-the-shelf food requiring only 24 h of incubation makes them the most convenient, least labor-intensive, live food available for aquaculture (Sorgeloos & Roubach, 2021). The nutritional value of Artemia, especially for marine organisms, is not constant, but varies both geographically and temporally. During the last decade, however, both the causes of Artemia nutritional variability and methods to improve poorquality Artemia have been identified (Loufi et al., 2024).
Brine shrimp (Artemia spp.) are used in marine aquaculture worldwide. Annually, more than 2,000 metric tons of dry cysts are used for cultivation of fish, crustacean, and shellfish larva. Brine shrimp are important to aquaculture because newly hatched brine shrimp nauplii (larvae) provide a food source for many fish fry (Mozanzadeh et al., 2021). Culture and harvesting of brine shrimp eggs represents another aspect of the aquaculture industry. Nauplii and metanauplii of Artemia, commonly known as brine shrimp, play a crucial role in aquaculture due to their nutritional value and suitability as live feed for many aquatic species, particularly in larval stages (Sorgeloos & Roubach, 2021).
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1. The document discusses exploration of the Mubda chromite deposit located in Samail Wilayat, Sultanate of Oman.
2. Fieldwork was conducted over 16 days to investigate the geology, geomorphology, and slopes of the area using topographic data.
3. Chemical analysis and geophysical methods revealed the rocks have a high chromite content and the deposits are generally located in dunite bodies. The entire area was found to have potential for economic chromite mining.
Mineral Deposits of SE Asia: Lessons for Myanmar from Adjacent -Dr Stuart Smi...MYO AUNG Myanmar
http://www.owenhegarty.com/wp-content/uploads/TigersStuart1.pdf
Presentation Outline
The Big Picture – Plate Tectonics
Mineral prospectivity is a function of plate tectonic setting
Myanmar has unusual and highly favourable tectonics
It shares tectonics with mainland Asia and Sumatra
The Concept of Mineral Deposit Models and Mineral Provinces
The mechanisms of mineral deposit formation are relatively well understood
Models derived from this understanding guide mineral exploration
Mineral deposits form provinces that reflect their tectonic setting
Details of selected mineral belts and deposits in adjacent regions
The mineral belts of adjacent regions are relatively well known
This knowledge can be transferred into Myanmar
Synthesis
Prospectivity & potential deposit styles in Myanmar
The document discusses sandstone uranium deposits found in the Phu Wiang Basin in Thailand. Three small uranium ore lenses were discovered through drilling programs in the 1970s-1980s. The mineralization is low-grade and consists primarily of coffinite dispersed in conglomeratic sandstone layers. Though additional prospecting occurred, the deposits were deemed uneconomic due to small size, low grades, and finely dispersed nature of the uranium minerals. Discoveries of dinosaur fossils during drilling provided benefits to museums, but further exploration found only uneconomic uranium occurrences in the region.
Myanmar has significant mineral potential across its four main geological belts. The document outlines Myanmar's geology, mineral provinces, current exploration and production activities for minerals such as gold, platinum, uranium, and rare earth elements. Future joint exploration programs with Japan are planned to target tin, tungsten, antimony, mineral sands, and rare earth elements. Requirements for foreign investment in Myanmar's mining industry including licenses, infrastructure needs, environmental protections, and corporate social responsibility are also discussed.
Myanmar is rich in mineral wealth. But it still left much of the virgin lands which are remote, mountainous and rugged. Much will be find. Mineral database is not well established and complete yet.
This document provides an overview of mineral resources and database building efforts in Myanmar. It describes the organization of the Ministry of Mines and its departments responsible for geological survey, mineral exploration, and mining enterprises. It then summarizes the major known mineral occurrences in Myanmar, including deposits of copper, iron, lead, zinc, silver, and nickel. The document concludes by outlining plans to develop a comprehensive mineral database for Myanmar to support further exploration and development of the country's mineral resources.
This is an abstract from the 5th Annual Minerals South Conference & Tradeshow of October 2009 in Cranbrook, British Columbia.
The subject is the Wicheeda rare earth carbonatite being explored by Spectrum Mining Corp.
Myanmar The Black Swan of Global Tin - Gardiner & Sykes - May 2015 - ITRI Con...John Sykes
Myanmar has emerged as the third largest producer of tin globally due to production from the Man Maw mining district in Wa State. However, production comes from an area outside of Myanmar's traditional tin producing regions and many questions remain regarding reserves, infrastructure, and political stability. While Myanmar has huge untapped mineral potential, it remains a high-risk jurisdiction. Further development of the mining industry could significantly help Myanmar's economy if issues of transparency, environment, and the upcoming elections and mining law changes are successfully addressed.
Myanmar known until recently as Burma, is slowly but steadily starting to attract foreign investment, driven mainly by international resource firms eager to tap into the mineral-rich South East Asia's country. After more than half a century of military ruling, Burma has started benefitting from the recent suspension of sanctions by Canada, the United States and the European Union. Myanmar's gold production is increasing and could prove a key factor for the country's economic growth, but many gold miners are suffering from lung diseases due to inadequate equipment and antiquated practices. In mineral-rich areas of Kachin State, taxes from Burmese and Chinese gold mining provides an important income stream to the Kachin Independence Organization. However, these mining companies use mercury in an environmentally hazardous extraction process, which can lead to long-lasting damage for the area's forests and river ways.
The document summarizes trends in mineral prospecting in India from 2004-2007. It discusses several important mineral deposits in India such as base metals like copper, lead, and zinc. It also discusses precious metal deposits of gold and diamond, located primarily in greenstone belts and carbonate rocks. Major ferrous deposits of iron ore are described along with chromite, manganese, and uranium deposits. Locations, geological settings, and formation processes are provided for several of these important mineral deposits in India.
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The document discusses minerals and energy resources in India, including what minerals are, how they are formed and occur, how mining works, major mineral deposits and producing regions in India, and key ferrous minerals like iron ore and manganese. It provides details on the classification, production, and uses of important minerals like iron ore and manganese, as well as the leading producing states for these minerals in India.
Manganese ore deposits are widely scattered in various districts in Egypt.
They occur at some localities in Sinai Peninsula and at a few localities in the Eastern Desert.
Manganese deposits are known:
in the Um Bogma district in west central Sinai; and
in the Halaib "Elba" district in the southern portion of Eastern Desert.
In addition, minor occurrences are known in Wadi Mialik near Abu Ghosun and Ras Banas in the Southern Eastern Desert, and Wadi Abu Shaar El Qibli (Black Hill), to the north of Hurghada
This document provides an overview of uranium exploration and mining case studies in Nigeria, including:
- Uranium was discovered in the 1970s in the northeast region through exploration projects conducted by the Nigerian Uranium Mining Company.
- Four main uranium deposit areas were discovered - Gumchi, Gabrunde, Mika, and Mayo-Lope. Drilling and sampling was conducted at these sites to determine average uranium concentrations and reasonably assured resource estimates ranging from 50 to 100 tons of uranium oxide.
- The geology of Nigeria consists of a basement complex and younger granites upon which sedimentary basins were deposited. Uranium mineralization is hosted in granitic rocks and
Metallogenic Epoch and Province
Metallogenetic Epochs
Metallogenetic epochs, as defined above, are specific periods characterised by formation of large number of mineral deposits. It does not mean that all the mineral deposits formed during a definite metallogenetic epochs. In India the chief metallogenetic epochs were:
1. Precambrian
2. Late Palaeozoic
3. Late Mesozoic to Early Tertiary
massive type interlayer with gabbroic rocks in the Eastern Desert; Main occurrences of Ti-Fe oxide deposits in Egypt; Abu Ghalaga Ore Deposit; Abu Ghalaga ilmenite ore deposit categories ; Abu Ghalaga Mineral composition; Mining Techniques; Origins; Korabkanci titano-magnetite ore; black sand placer deposits type; Rosetta (or Rashid East); Northern Sinai Coast
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The document provides information on limestone deposits in India and Tamil Nadu. It finds that South and West zones of India contain the major limestone reserves, accounting for 68% of the country's total. Within the South zone, Andhra Pradesh and Karnataka contain over 55% of the reserves. In Tamil Nadu, limestone deposits are found across multiple districts and taluks, with major occurrences in Tirunelveli, Tuticorin, Virudhunagar, Madurai, Coimbatore, Karur, Namakkal, Salem, and Tiruchirappalli districts. The document outlines the geological nature and locations of the key limestone deposits in each area.
The Tectonic and Metallogenic Framework of MyanmarMYO AUNG Myanmar
https://research-repository.st-andrews.ac.uk/bitstream/handle/10023/10689/Cawood_2016_Myanmar_OGR_AM.pdf?sequence=1
The Tectonic and Metallogenic Framework of
Myanmar: A Tethyan Mineral System
Nicholas J. Gardiner1,9*
, Laurence J. Robb1
, Christopher K. Morley2,3
,
Michael P. Searle1
, Peter A. Cawood4
, Martin J. Whitehouse5
,
Christopher L. Kirkland6
, Nick M.W. Roberts7
, Tin Aung Myint8
1. Department of Earth Sciences, University of Oxford, Oxford OX1 3AN, United
Somaliland has significant unexplored mineral potential. The mining sector is still small, with only artisanal mining currently occurring. The country possesses deposits of gold, platinum, iron, copper, tin, gemstones, and other industrial minerals. However, large areas remain unexplored due to a lack of geological surveys. Somaliland desires to develop its mining industry but faces challenges in attracting investment and building institutional capacity for resource management and data collection.
02 Mugumbate - Overview of mineral potential (1).pdfLeonNdiraya1
- Zimbabwe has significant unexplored mineral potential based on its geological formations like greenstone belts and the Great Dyke that are known to host valuable resources. However, challenges like political instability, lack of investment, and outdated exploration techniques have limited understanding of the size and distribution of resources.
- With modern exploration methods and a stable investment environment, it is likely that many currently small deposits could become large mines and many new deposits could be discovered, particularly for commodities like gold, platinum, chromium, and coal. The mineral endowment of Zimbabwe may be much larger than currently recognized.
Similar to Mining Activity and Investment Opportunity in Myanmar.pptx (20)
The use of Nauplii and metanauplii artemia in aquaculture (brine shrimp).pptxMAGOTI ERNEST
Although Artemia has been known to man for centuries, its use as a food for the culture of larval organisms apparently began only in the 1930s, when several investigators found that it made an excellent food for newly hatched fish larvae (Litvinenko et al., 2023). As aquaculture developed in the 1960s and ‘70s, the use of Artemia also became more widespread, due both to its convenience and to its nutritional value for larval organisms (Arenas-Pardo et al., 2024). The fact that Artemia dormant cysts can be stored for long periods in cans, and then used as an off-the-shelf food requiring only 24 h of incubation makes them the most convenient, least labor-intensive, live food available for aquaculture (Sorgeloos & Roubach, 2021). The nutritional value of Artemia, especially for marine organisms, is not constant, but varies both geographically and temporally. During the last decade, however, both the causes of Artemia nutritional variability and methods to improve poorquality Artemia have been identified (Loufi et al., 2024).
Brine shrimp (Artemia spp.) are used in marine aquaculture worldwide. Annually, more than 2,000 metric tons of dry cysts are used for cultivation of fish, crustacean, and shellfish larva. Brine shrimp are important to aquaculture because newly hatched brine shrimp nauplii (larvae) provide a food source for many fish fry (Mozanzadeh et al., 2021). Culture and harvesting of brine shrimp eggs represents another aspect of the aquaculture industry. Nauplii and metanauplii of Artemia, commonly known as brine shrimp, play a crucial role in aquaculture due to their nutritional value and suitability as live feed for many aquatic species, particularly in larval stages (Sorgeloos & Roubach, 2021).
Phenomics assisted breeding in crop improvementIshaGoswami9
As the population is increasing and will reach about 9 billion upto 2050. Also due to climate change, it is difficult to meet the food requirement of such a large population. Facing the challenges presented by resource shortages, climate
change, and increasing global population, crop yield and quality need to be improved in a sustainable way over the coming decades. Genetic improvement by breeding is the best way to increase crop productivity. With the rapid progression of functional
genomics, an increasing number of crop genomes have been sequenced and dozens of genes influencing key agronomic traits have been identified. However, current genome sequence information has not been adequately exploited for understanding
the complex characteristics of multiple gene, owing to a lack of crop phenotypic data. Efficient, automatic, and accurate technologies and platforms that can capture phenotypic data that can
be linked to genomics information for crop improvement at all growth stages have become as important as genotyping. Thus,
high-throughput phenotyping has become the major bottleneck restricting crop breeding. Plant phenomics has been defined as the high-throughput, accurate acquisition and analysis of multi-dimensional phenotypes
during crop growing stages at the organism level, including the cell, tissue, organ, individual plant, plot, and field levels. With the rapid development of novel sensors, imaging technology,
and analysis methods, numerous infrastructure platforms have been developed for phenotyping.
Current Ms word generated power point presentation covers major details about the micronuclei test. It's significance and assays to conduct it. It is used to detect the micronuclei formation inside the cells of nearly every multicellular organism. It's formation takes place during chromosomal sepration at metaphase.
When I was asked to give a companion lecture in support of ‘The Philosophy of Science’ (https://shorturl.at/4pUXz) I decided not to walk through the detail of the many methodologies in order of use. Instead, I chose to employ a long standing, and ongoing, scientific development as an exemplar. And so, I chose the ever evolving story of Thermodynamics as a scientific investigation at its best.
Conducted over a period of >200 years, Thermodynamics R&D, and application, benefitted from the highest levels of professionalism, collaboration, and technical thoroughness. New layers of application, methodology, and practice were made possible by the progressive advance of technology. In turn, this has seen measurement and modelling accuracy continually improved at a micro and macro level.
Perhaps most importantly, Thermodynamics rapidly became a primary tool in the advance of applied science/engineering/technology, spanning micro-tech, to aerospace and cosmology. I can think of no better a story to illustrate the breadth of scientific methodologies and applications at their best.
Or: Beyond linear.
Abstract: Equivariant neural networks are neural networks that incorporate symmetries. The nonlinear activation functions in these networks result in interesting nonlinear equivariant maps between simple representations, and motivate the key player of this talk: piecewise linear representation theory.
Disclaimer: No one is perfect, so please mind that there might be mistakes and typos.
dtubbenhauer@gmail.com
Corrected slides: dtubbenhauer.com/talks.html
ESR spectroscopy in liquid food and beverages.pptxPRIYANKA PATEL
With increasing population, people need to rely on packaged food stuffs. Packaging of food materials requires the preservation of food. There are various methods for the treatment of food to preserve them and irradiation treatment of food is one of them. It is the most common and the most harmless method for the food preservation as it does not alter the necessary micronutrients of food materials. Although irradiated food doesn’t cause any harm to the human health but still the quality assessment of food is required to provide consumers with necessary information about the food. ESR spectroscopy is the most sophisticated way to investigate the quality of the food and the free radicals induced during the processing of the food. ESR spin trapping technique is useful for the detection of highly unstable radicals in the food. The antioxidant capability of liquid food and beverages in mainly performed by spin trapping technique.
Immersive Learning That Works: Research Grounding and Paths ForwardLeonel Morgado
We will metaverse into the essence of immersive learning, into its three dimensions and conceptual models. This approach encompasses elements from teaching methodologies to social involvement, through organizational concerns and technologies. Challenging the perception of learning as knowledge transfer, we introduce a 'Uses, Practices & Strategies' model operationalized by the 'Immersive Learning Brain' and ‘Immersion Cube’ frameworks. This approach offers a comprehensive guide through the intricacies of immersive educational experiences and spotlighting research frontiers, along the immersion dimensions of system, narrative, and agency. Our discourse extends to stakeholders beyond the academic sphere, addressing the interests of technologists, instructional designers, and policymakers. We span various contexts, from formal education to organizational transformation to the new horizon of an AI-pervasive society. This keynote aims to unite the iLRN community in a collaborative journey towards a future where immersive learning research and practice coalesce, paving the way for innovative educational research and practice landscapes.
Unlocking the mysteries of reproduction: Exploring fecundity and gonadosomati...AbdullaAlAsif1
The pygmy halfbeak Dermogenys colletei, is known for its viviparous nature, this presents an intriguing case of relatively low fecundity, raising questions about potential compensatory reproductive strategies employed by this species. Our study delves into the examination of fecundity and the Gonadosomatic Index (GSI) in the Pygmy Halfbeak, D. colletei (Meisner, 2001), an intriguing viviparous fish indigenous to Sarawak, Borneo. We hypothesize that the Pygmy halfbeak, D. colletei, may exhibit unique reproductive adaptations to offset its low fecundity, thus enhancing its survival and fitness. To address this, we conducted a comprehensive study utilizing 28 mature female specimens of D. colletei, carefully measuring fecundity and GSI to shed light on the reproductive adaptations of this species. Our findings reveal that D. colletei indeed exhibits low fecundity, with a mean of 16.76 ± 2.01, and a mean GSI of 12.83 ± 1.27, providing crucial insights into the reproductive mechanisms at play in this species. These results underscore the existence of unique reproductive strategies in D. colletei, enabling its adaptation and persistence in Borneo's diverse aquatic ecosystems, and call for further ecological research to elucidate these mechanisms. This study lends to a better understanding of viviparous fish in Borneo and contributes to the broader field of aquatic ecology, enhancing our knowledge of species adaptations to unique ecological challenges.
The ability to recreate computational results with minimal effort and actionable metrics provides a solid foundation for scientific research and software development. When people can replicate an analysis at the touch of a button using open-source software, open data, and methods to assess and compare proposals, it significantly eases verification of results, engagement with a diverse range of contributors, and progress. However, we have yet to fully achieve this; there are still many sociotechnical frictions.
Inspired by David Donoho's vision, this talk aims to revisit the three crucial pillars of frictionless reproducibility (data sharing, code sharing, and competitive challenges) with the perspective of deep software variability.
Our observation is that multiple layers — hardware, operating systems, third-party libraries, software versions, input data, compile-time options, and parameters — are subject to variability that exacerbates frictions but is also essential for achieving robust, generalizable results and fostering innovation. I will first review the literature, providing evidence of how the complex variability interactions across these layers affect qualitative and quantitative software properties, thereby complicating the reproduction and replication of scientific studies in various fields.
I will then present some software engineering and AI techniques that can support the strategic exploration of variability spaces. These include the use of abstractions and models (e.g., feature models), sampling strategies (e.g., uniform, random), cost-effective measurements (e.g., incremental build of software configurations), and dimensionality reduction methods (e.g., transfer learning, feature selection, software debloating).
I will finally argue that deep variability is both the problem and solution of frictionless reproducibility, calling the software science community to develop new methods and tools to manage variability and foster reproducibility in software systems.
Exposé invité Journées Nationales du GDR GPL 2024
The debris of the ‘last major merger’ is dynamically youngSérgio Sacani
The Milky Way’s (MW) inner stellar halo contains an [Fe/H]-rich component with highly eccentric orbits, often referred to as the
‘last major merger.’ Hypotheses for the origin of this component include Gaia-Sausage/Enceladus (GSE), where the progenitor
collided with the MW proto-disc 8–11 Gyr ago, and the Virgo Radial Merger (VRM), where the progenitor collided with the
MW disc within the last 3 Gyr. These two scenarios make different predictions about observable structure in local phase space,
because the morphology of debris depends on how long it has had to phase mix. The recently identified phase-space folds in Gaia
DR3 have positive caustic velocities, making them fundamentally different than the phase-mixed chevrons found in simulations
at late times. Roughly 20 per cent of the stars in the prograde local stellar halo are associated with the observed caustics. Based
on a simple phase-mixing model, the observed number of caustics are consistent with a merger that occurred 1–2 Gyr ago.
We also compare the observed phase-space distribution to FIRE-2 Latte simulations of GSE-like mergers, using a quantitative
measurement of phase mixing (2D causticality). The observed local phase-space distribution best matches the simulated data
1–2 Gyr after collision, and certainly not later than 3 Gyr. This is further evidence that the progenitor of the ‘last major merger’
did not collide with the MW proto-disc at early times, as is thought for the GSE, but instead collided with the MW disc within
the last few Gyr, consistent with the body of work surrounding the VRM.
2. Content
1. Introduction
2. Mineral Occurrences in Myanmar
3. Current Mining Activity in Myanmar
4. Investment Information
I-Procedure for Foreign Investment in Mining Sector
II-Tex Regime and Royalty in Mining Sector
III-Category of Mining Permits
5.Why You Investment in Mining Sector in Myanmar
6.Conclusion
4. Myanmar has extensive mineral resources and
a well established centuries-old mining industry.
The main resources are petroleum, gas, coal, iron, tin, tungsten,
antimony, lead, zinc, copper, silver, gold, jade and gemstones.
Clay, limestone, dolomite, barite, fluorite, gypsum, rock salt,
feldspar, quartz, glass sand and etc. are the main industry mineral
and raw mineral.
5. • Lies btw 09˚ 32’N and 28˚ 31’N(lat),
and 92˚ 10’ E and 101˚ 11’ E(long)
• The greatest N-S extent is about 2051 km
• The greatest E-W extent is about 936 km
• Total length of country border is 4000 km
• Covering area of 676580 km2
• N&NS border by China 2204 km
• SE border by Thailand 2107 km
• E border by Laos 238 km
• W border by Bangladesh 271 km
• N border by India 1338 km
Geographic Background of Myanmar
9. Mineral Deposit of Myanmar
Million Tons
Iron ore 359.24
Barite 87.32
Coal 490.00
Lead & Zinc Ore 13.80
Chromite Ore 1.03
Nickel Ore 162.00
Limestone 6560.893
Antimony Ore 2.27
Gold Ore 12.86
Tin – Tungsten 40.00
Copper Ore 1587.80
Platinum Group 21.47
Distribution of major deposits in Myanmar
11. Tin & Tungsten Deposit in Myanmar
• -one of the most important mineral resources in Myanmar
• -tin & tungsten mineralization is related to granitoid
intrusions.
• -about 480 of occurrences, along the Tanintharyi Region
and western part of the Shan Plateau.
• -occurs along the granitic belt in SE Asia peninsula
(distributed over more than 1200 Km in Myanmar with
more prominent in tungsten toward the north)
• -the ratio of tin & tungsten are varies locally.
• -Most of the cassiterite is mined from placers while
tungsten is mined from hard rock veins.
12. Distribution of Copper Deposit
Sinbo-Nankesan
Cu – 3 to 4 %
0.21 million (Possible)
Bawdwin
Cu – 0.87%
2.5 million (Possible)
Panmakut Manna
Cu – 4%
0.001 million (Possible)
Panpwe Kyauk Taung
Cu – 4%
0.001 million (Possible)
Kweeight
Cu – 4%
0.001 million (Possible)
Shangalon
Cu – 0.23%
9 million(Possible)
Kyesin Taung
Cu – 0.77%
66.5 million (Possibld)
Sable Taung & S of SB
Cu – 0.7 to 1.01 %
27.86 million (Possible)
Lrtpadaung
Cu – 0.4 %
1478 million (Possible)
Sable Taung (Kyaukse)
Cu – 1.51 %
0.88 million (Possible)
Laymyetna
Cu – 0.8 to 2%
0.28 million (Possible)
13. Distribution of Lead, Zinc, Silver
Panwa (Kachin)
Pb,Zn -1.06%
12.5 million(Possible)
Bawdwin (Shan North)
Pb,Zn- 5%
12.8 million(Probable)
Phaleng(Shan North)
Zn 15.84
0.01 million (Possible)
Yadanatheingi (Shan
North)
Pb,Zn- 4%
0.1 million (probable)
Paungdaw (Mandalay)
Pb- 4.7%
0.09 million(Probable)
Mawhki(Kayin)
Zn – 0.3%
0.332 million (Possible)
Bawsaing (Shan North)
Pb,Zn – 6%
0.0075 million (Probable)
Lon Chein (Shan South)
Zn - 36%
0.234 million (Possible)
14. Lead-Zinc-Silver Deposit in Myanmar
more than 100 occurrences of Pb-Zn-Ag mineralization in
the Eastern Highland Province
Mineralization occurs as five different styles
1. Volcanogenic massive sulphites types(VMS) at Bawdwin
mine
2. Massissipi valley type deposit at Bawsaing
3. Cavity filling vein –type in Yadanatheingi
4. In vein and skarn type near the contact between granitic
rock and marble at Phaungdaw mine
5. Zinc carbonate deposit (secondary deposit)at Long Hken
17. Antimony Deposit in Myanmar
More than 140 occurrences of stibnite and other Sb
bearing minerals are known in Myanmar.
Occurrence in Kayah State, Kayin State, Mon State,Shan
State(S)
The majority of antimony mineralization occurs in the
late Paleozoic carbonates (Triassic to Permian in age)
and also in the late Pleozoic clastic sediments of the
Mergui series.
Generally found in veins or lenses or both.
Must be successively upgraded for the required
concentation or grade.
So far, the best known antimony deposit are at Thabyu,
Kayin State. The ore is reported to be hight grade.
18. Distribution of Iron Deposit
Kantawyan (Kachin)
Fe – 49 to 69%
2.354 million (Possible)
Taungkatone Taung(kachin)
Fe – 37 to 45%
2.3 million (Possible)
Taung Nyo Taung(Kachin)
Fe – 40.67%
18.9 million (Potential)
Haemaung (Kachin)
Fe – 45.93%
1.1 million (Potential)
Mongkanwe (Shan East)
Fe – 39 to 66%
21.5 million(Potential)
Pinpet (Shan South)
Fe – 56.4% (He,Lim)
80 million (Probable)
Maputae Island (Tanitharyi)
Fe – 42%
1 million (Probable)
Lamaug (Kachin)
Fe – 51.54%
8.9 million (Probable)
Kathaing Taung (Kachin)
Fe – 50.56%
223 million (Probable)
Sanleik (Kachin)
Lim
10 million (Potential)
Kyatwinye, Inya (Mandalay)
Fe – 54%
3.7 + 4.5 million (Probable)
Minlan Thanseik,
Shwegyin(Bago)
Fe – 28 to 56.7%
75.53 million (Possible)
Kanmaw Island
(Tanintharyi)
Fe – 36%
21.2 million (Probable)
Kho Island (Thanintharyi)
Fe – 46.05%
7.6 million (Probable)
20. Nickel Deposit in Myanmar
14 occurrence of nickel deposit.
Nickel and chromium minerals are always associated with the
Ultramafic rocks .
Occur in several localities on the eastern foothill of the Western
Ranges.
Mwe Taung and Phar Tung in Chin State and Tagaung Taung in
Mandlay Region are economically attractive.
Tagaung Taung nickel mine was the largest mining project with
Myanmar and China, also one of the largest Chinese project
investments in neighboring country.
22. Chromium Deposits in Myanmar
43 of Chromium occurrences
Associated with ophiolite assemblage occur in several localities on
eastern foothill of the Westen Ranges.
Chromite deposits are wide spread occurrences in Myanmar being related
to north –south trending ophiolite lines.
24. Gold Occurrence in Myanmar
PRIMARY GOLD DEPOSITS/OCCURRENCES IN MYANMAR
(1) Mesothermal gold-quartz lode, porphyry style Cu-Au & its related
Epithermal Au along the central magmatic arc.
(2) Sediment-hosted epithermal Au mineralization along the Sagaing
fault zone.
(3) Mesothermal and epithermal gold mineralization in Tagaung
Myitkyina belt
(4) Au(Cu) skarn & Mesothermal veins in marble, gneiss and
granite within the Mogok metamorphic belt
(5) Slate belt style Mesothermal gold-quartz veins in Chaung Magyi &
Mergui Groups.
25. Gold Deposit in Myanmar
Gold is known to occur quite widely in several part of the
country.
As placer in stream channels or in the soil developed above
the mineralization area.
The central volcanic line is very attractive for epithermal and
mesothermal copper-gold mineralization.(Wintho-Bamauk
region, Kyaukpazut, Kyaukpahto gold mine and etc.)
The Slate Belt on western mergin of the EHP became a
target of Slate Belt gold (metamorphic hydration)
mineralization. (Modi Taung, Phayaung Taung, Taungoo-
Shwegyin- Kyaikhto areas)
34. Current Mining in Myanmar
Sabe Taung, Kyisin Taung(S&K) Copper Project
Also known as Monywa Project.
Myanmar Ivanhoe Copper Co Ltd(MICCL) had been foregin
joint venture with ME-1 and produced grade A cathode
copper from S&K and Sable Taung South deposits.
It ownership was transferred to local company with a foreign
joint venture company.
MICCL produced 264,036 t of cathode copper up to the
transfer date.
Early in the 20 century the S&K mine is operated by Wanbo
Mining Ltd with the name of Myanmar Yang Tse Copper Ltd.
35. Current Mining in Myanmar
Letpadaung Copper Project
LCP is located in the largest of four copper deposits in the
Salingyi Township area of Sagaing Region.
On July 24 2013 , ME -1 signed to the PSC for LCP with
Myanmar Economic Holding Ltd (MEHL) and Wanbo Mining
Ltd.
Government of Myanmar with 51%,whilst MEHL and Wanbo
retain 49% .
The estimated mine life is 30 years.
This is expected to produce 100,000 t/y of copper.
The stripping ratio in mine is almost 1:0.99.
36. Current Mining in Myanmar
Namtu Bawdwin Lead-Zinc-Silver
The famous Namtu Bawdwin lead-zinc mine has been producting refined lead
and silver, as well as nickel, copper matte and antimonial products for many
years.
Bawdwin is one of the world’s largest undeveloped silver-lead-zinc mines.
Ownership was transferred in 2010 to Win Myint Mo Industrial Co.PSC with
ME1
Bawdwin is a rich polymetallic deposit of 520g/t silver –equivalent grades.
The metal content of run-of-mine ore (ROM) around this time was 100-185 g/t
Ag, 21%Pb , 15%Zn, Cu0.23%, Ni 0.08% and Fe 4.4%, APML says silver
equivalent grade is 305-520 g/t.
Asia Pacific Mining Ltd licence application covers 80,000 ha surrounding
Bawdwin mine.
37. Current Mining in Myanmar
Tagaung Taung Nickel Project
A considerable amount of Chinese investment in the
minerals sector.
At the time, it was signed, Tagaung Taung nackel
pooject was the largest mining project, China and
Myanmar Government.
It was also one of the largest Chinese project
investments in a neighboring country.
In July 2004 China Nonferrous Metal Mining (Group) Co
(CNMC) signed exploration and feasibility agreement
with ME -3.
Total investment in the project will exceed $800 million
for annual output of 85,000 t of ferro-nickel after
completion.
It has 700,000 t of nickel resources in the mine.
39. a. In accord with the policy of the Ministry of Mines, ministry of mine is not
making their own investment, but to encourage foreign and local
investors to invest in the mining sector.
b. The investor can invest as a foreign direct investment (FDI) or joint
investment with local company.
c. For investors who would like to do exploration to confirm the reserve of a
deposit or to start with the grassroots exploration operations in a
virgin land, they may apply accordingly clearly stating their intentions.
d. Funds required to conduct the prospecting, exploration and feasibility
study are borne by the investor 100% at his own risk.
e. Ministry of Mines not allowed to export the raw ore.
f. Investor should be made value added (or) mineral processing.
g. Ministry encourages to establish the refinery plants/ smelters with the
latest technologies.
Investment Information
41. (a) Foreign companies have to send letter of courtesy call to the Union
Minister through the respective Embassy in Myanmar to Ministry of Foreign
Affairs to the Ministry of Mines officially.
(b) The Union Minister or responsible officials will discuss the investment
opportunities in mining sector mainly focus on mineral commodity and
targeted area.
(c) Site visit will be arranged if requested by the investors or company after
technical discussion with responsible departments. Recommendation letter
from the respective Embassy, letter of undertaking, tentative site visit
schedule and passport copy are required to submit to the Ministry of Mines
two week ahead.
42. (d) After the site visit, if the investor decided to invest in Myanmar, a
proposal should submit to the Ministry of Mines and copy to relevant
departments.
(e) Minerals prospecting, exploration and feasibility study are concerned to
DGSE and other
Mining Enterprises are responsible for mining operation and
production stages.
(g) After getting the approval of the Ministry of Mines and the
completion of all the require recommendation document, the
proposal and the Agreement Draft will send to the
Myanmar Investment Commission
( MIC ) for Investment permit.
43. The following documents should be included with the proposal:
1. Company Registration
2. Company Profile and other relevant facts about the company
3. Recommendation and endorsement of the respective Embassy
in Myanmar
4. Financial Bank Statement
5. List of the Board of Directors
6. Initial work program
7. Map of the proposed area with coordinates.
The require document with Proposal
46. a. For Metallic Minerals - 3 to 4 %
b. For Precious Metallic Minerals - 4 to 5 %
c. For Industrial Minerals - 1 to 3%
d. For Ruby, Sapphire, Jade and Diamond - 20%
e. For other Gems - 10 %
Royalty is taxed on value of mineral sold.
Fiscal Regime Royalty
48. a. Prospecting Permits -1 yr + 1 yr
b. Exploration Permits -3 yrs + 1 yr+1yr
c. Feasibility Study -1 yr
d. Subsistence Mining Permits -1 yr
e. Small Scale Mining Permits -5 yrs
f. Large Scale Mining Permits -15 yrs+ 5 yrs (4 Times)
Categories of Mining Permits
49. a. Prospecting Permits - 4200 Km2
b. Exploration Permits - 3150 Km2
c. Small Scale Mining Permits - not more than 1 Km2
d. Large Scale Mining Permits - depends on Investment
amount and Ore Deposit.
Area of Mining Permits
50. Production Sharing Contract (PSC) System
1. Ministry of Mine has practiced the production Sharing Contract
(PSC) system in mining.
2. In the production sharing types of agreement the investor shall have
to contribute 100% of investment in which case the government
would expect a share of the production and a production sharing
will be signed ratio to be agree upon between the parties.
3. The Production Sharing Ratio is based on the mineral commodity
like Gold, Copper, Lead, Zinc, Tin, Tungsten, Nickel, Manganese,
Industrial Raw Mineral and Coal etc. and as well as based on the
current LME (London Metal Exchange) prices.
4. The Production Sharing Ratio has to negotiate with concerning
Mining Enterprises when Foreign Company is proposed for
Mining.
51. Investment Opportunity (Joint Venture)
1988 Union of Myanmar Investment Law
1994 Union of Myanmar Mines Law
1996 Rule relating to Mines Law
To invite participation in terms of technical known-hown and investment
from sources with in the country and abroad.
Now Myanmar Foreign Investment Law and Myanmar Mining Law are
revised to fulfill the present situation and will submit to the Pyithu Luttaw
(Parliament) in near future.
52. Sr. Company Registered
Country
Type of Mineral Type of Permit
1. Conerstone Resource (Myanmar)
Ltd
Australia Zinc Ore Large Scale
Mineral Production Permit
2. Myanmar Ponepipet Co.,Ltd Thailand Tin Concentrate ၊၊
3. Myanmar CNMC Nickel Co.,Ltd China Ferronickel ၊၊
4. Simco Song Da Joint Stock Co., Vietnam Marble ၊၊
5. Asia Pacific Mining Ltd. China Lead, Zinc, Copper,
Gold
Exploration Permit
6. Nobel Gold Limited Russia Exploration Permit
7. De Rui Feng Investment Co., Ltd. China ၊၊
8. North Mining Investment Co.,
Ltd.
China Gold and Associated
Minerals
Feasibility Study
9. Myanmar Yangtze Copper Co.,
Ltd.
China Tin-Tungsten Large Scale
Mineral Production Permit
10. Myanmar Wanbao Copper Co.,
Ltd.
China Copper ၊၊
11. Daewoo Precious Resources
Co.Ltd
Korea Copper, Gold Exploration Permit
12. GPS Joint Venture Co.,Ltd China Lead, Zinc Large Scale
Mineral Production Permit
13 Sichuan Chuandi Myanmar
Mining Co.,Ltd
China Copper Feasibility Study
14 Royal Light Ron Ann Co., China Iron Exploration & Feasibility
15 Geo Pro Mining Co.,Ltd Russia Antimony Prospecting , Exploration &
Feasibility
16 Asia Mining Limited Singapore Heavy Sand ( Mineral
Sand)
Exploration
17 Myanmar VES Joint Venture Co., Thailand Jewellery Value added Processing &
Marketing
18 Myanmar Tasaki Co., Japan Pearl Large Scale Pearl Production
19 Myanmar Atlantic Co., Australia Pearl Large Scale Pearl Production
20 Myanmar Adman Pearl Co., Thiland Pearl Large Scale Pearl Production
Foreign Direct Investment List in Mining Sector
On 31.12.201
53. Sr. Company
Registere
d
Country
Type of Mineral
Type of
Permit
1.
Conerstone Resource
(Myanmar) Ltd
Australia Zinc Ore
Large Scale
Mining Permit
2. Myanmar Ponepipet Co., Ltd Thailand Tin Concentrate
၊၊
3. Myanmar CNMC Nickel Co., Ltd China Ferronickel
၊၊
4. Simco Song Da Joint Stock Co., Vietnam Marble
၊၊
5. Asia Pacific Mining Ltd. China
Lead, Zinc,
Copper, Gold
Exploration
Permit
6. Nobel Gold Limited Russia
Gold and
Associated
Minerals
၊၊
7.
De Rui Feng Investment Co.,
Ltd.
China Tin-Tungsten
၊၊
8.
North Mining Investment Co.,
Ltd.
China Ferronickel
Feasibility
Study
9.
Myanmar Yangtze Copper
Co.,Ltd.
China Copper
Large Scale
Mining Permit
Myanmar Wanbao Copper ၊၊
Permit Issued to Foreign Investors from Ministry of Mine
54. Project Requiring An Initial Environmental Examination (IEE)
Industrial Mineral (Small Scale) less than 247.1 acres
Gold (small scale) less than 20 acres
Gemstone less than 20 acres
Other Mineral(small scale) less than 20 acres
55. Project Requiring A Full Environmental Impact
Assessment(EIA)
Industrial Mineral (Large Scale) 247.1 acres and above
Gold (Large scale) 20 acres and above
Gemstone 20 acres and above
Other Mineral(Large scale) 20 acres and above
56. Why You Investment in Mining Sector in
Myanmar
Access to untapped world-class mineral resources and a
geostrategic location.
Unknown small scale mine are preserved in most of parts.
Small scale will be large scale
Undergoing political and economic reforms, which will
attract more foreign trade and FDI once the laws are in place
The first three SEZs will set up in Thilawa, Kyaukphyu and
Dawei.
57. Conclusion
Well known deposits are already occupied by local company.
So Foreign investors should be start from Green field area.
Most of area in Myanmar have no geological records and
minerals occurrence record because of security and terrain.
So investor can expect to find the big mineral deposit base on
mineral potential belt.
Combine with accumulation on local people’s data base.
Some of companies are making prospection and exploration in
wide area.
we expected to find new large deposits .