MERAL Myanmar Education Research and Learning Portal
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Rock Sequences and Petrography of the Popa – Kyauktaga Area, Kyaukpadaung Township, Mandalay Region
http://hdl.handle.net/20.500.12678/0000007885
http://hdl.handle.net/20.500.12678/0000007885982dfda6-fad1-416d-9c73-6c98b98cd1ef
82dda378-3f11-4a8c-91ce-b79bb05846cd
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Mar Mar Khaing.pdf (28.7 MB)
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Publication type | ||||||
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Journal article | ||||||
Upload type | ||||||
Publication | ||||||
Title | ||||||
Title | Rock Sequences and Petrography of the Popa – Kyauktaga Area, Kyaukpadaung Township, Mandalay Region | |||||
Language | en | |||||
Publication date | 2020-08-31 | |||||
Authors | ||||||
Mar Mar Khaing | ||||||
Maw Maw Myint | ||||||
Description | ||||||
The present area is the northwestern part of Mt.Popa region which lies in the Central Volcanic Line of Late Cretaceous in Myanmar. The main four types of rock sequence are observed in the area: Kyauktaga-Legyi agglomerate (KLA), basaltic lavas (V5), black tuffs and andesitic lavas ( V3) and Popa andesite(PA). The Irrawaddy Formation is well developed in the northwestern part of the area. The Popa andesite rocks are well exposed at the Popa village and found as irregular large boulders. They also capped the Irrawaddy sand rocks. The V3- flow is well exposed on the western flank of Mt.Popa volcano. Sometimes, this lava flow shows slagg and ropy structure. Andesitic tuffs also have been associated with this unit. In the upper portion of this flow, the phenocrysts of hornblende, augite and plagioclase are relatively larger size than those of the lower portion. The V5 flow is one of the last major flows on the northwestern slope of Mt. Popa cone and highly distributed near the Taungbaw village and found in the plantation area. At the northwestern end, this lava breaks up into partially cooled blocks which roll over one another and occur as blocks one upon the other. The phenocrysts of olivine have not been recognized in the middle portion of V5 - flow basalt. Kyauktaga - Legyi agglomerate unit extends as far north as the legyi village about 10.4 km from the crater. They consist of volcanic ash, tuff, pumice, scoria and unsorted volcanic fragments. | ||||||
Keywords | ||||||
Mt. Popa Volcano, Central Volcanic Line (CVL), Petrography, Irrawaddy Formation | ||||||
Journal articles | ||||||
I | ||||||
Meiktila University Research Journal, 2020, Vol.XI, No.1 | ||||||
383-388 | ||||||
XI |