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Natural Pozzolan in Mount Popa Area
http://hdl.handle.net/20.500.12678/0000007989
http://hdl.handle.net/20.500.12678/0000007989544b30a7-7cba-4aa1-8f2f-cf176cb08c63
59f2cf05-ab74-4758-af40-008f8ec65402
Name / File | License | Actions |
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Maw Maw Myint.pdf (2.7 MB)
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Publication type | ||||||
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Journal article | ||||||
Upload type | ||||||
Publication | ||||||
Title | ||||||
Title | Natural Pozzolan in Mount Popa Area | |||||
Language | en | |||||
Publication date | 2009-12-01 | |||||
Authors | ||||||
Maw Maw Myint | ||||||
Description | ||||||
Mount Popa, in central Myanmar, is a large, steep-sided cmposite cone that rises a height of 1518m(4981'). It contains a 1.6 km wide, 850 m deep, horseshoe-shaped caldera that is widely breached to the NW. Kyauktaga-Legyi Aggloomerate unit, volcanic ash deposit, covers an area of 20 sq.ml at the north of the breach. fine-grained pyroclastics of this deposit such as volcanic ash, tuff and scoria are crushed and ground into the finely-divided materials or powder that has been also known as Natural Pozzolan. It is an important ingredient in the production of an alternative cementing material to ordinary portland cement (OPC). Although several potential sources of natural pozzolan formed by volcanic origin are identified in Myanmar, Mt. Popa area is more favourable for commercial natural pozzolan production due to lesser erosion and better accessibilities. | ||||||
Keywords | ||||||
Mount Popa, composite cone, volcanic ash deposit, natural pozzolan | ||||||
Journal articles | ||||||
1 | ||||||
Meiktila University Research Journal, Vol.3, No.1 | ||||||
167-179 | ||||||
2 |