MERAL Myanmar Education Research and Learning Portal
Item
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Metamorphic Condition of Metamorphic Rocks Exposed at the Hngetmi Taung Area, Pyawbwe Township, Mandalay Region
http://hdl.handle.net/20.500.12678/0000005642
http://hdl.handle.net/20.500.12678/0000005642e7d8cd13-61c4-4e3a-8501-79080cfb5de7
1c75c3da-ba49-4ea6-8e77-16b95101822d
Name / File | License | Actions |
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Metamorphic Condition of Metamorphic Rocks Exposed at the Hngetmi Taung Area Pyawbwe Township Mandalay Region.pdf (1.5 Mb)
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Publication type | ||||||
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Journal article | ||||||
Upload type | ||||||
Publication | ||||||
Title | ||||||
Title | Metamorphic Condition of Metamorphic Rocks Exposed at the Hngetmi Taung Area, Pyawbwe Township, Mandalay Region | |||||
Language | en | |||||
Publication date | 2020-05-30 | |||||
Authors | ||||||
Khin Pyone | ||||||
Than Than Nu | ||||||
Description | ||||||
The research area, Hngetmi Taung is located about 11 miles southeast of Pyawbwe, so it is easily accessible by any vehicle throughout the year. The area under investigation falls within Mogok metamorphic Belt and lies between the Shan Highland and Central Cenozoic Belt .The area is a rather rugged terrain with high relief. Metamorphosed pelitic rocks and igneous rocks mainly occupy the study area. These rocks, for the whole area are found as a long narrow strip along the western margin of the Shan massif. The major rock units exposed in the study area are marble, calc-silicate rocks, gneiss, schists, biotite granite, diorite and rhyolite porphyry. Due to the similarity of Litholgic attributies and Lateral continuity of outcrops it is concluded that the original age of the metasedimentary rocks of the present area is possibly Paleozoic. The mineral assemblages of rock units indicate that the metamorphic rocks of the study area belong to the amphibolite facies and pyrixene hornfel facies. The age of metamorphism in this area is tentatively assigned to during Tertiary period,i.e Late Eocene to Early Miocene. The marbles and related rocks may have been metamorphosed mainly from the Plateau limestone, and perhaps partly from the Cretaceous limestones. Due to the appearance of lithologic continuity and index minerals pointed out that the metamorphic grade in the investigated area increase towards the west. | ||||||
Keywords | ||||||
amphibolite facies, pyroxene hornfel facies, Tertiary period, Cretaceous Limestone | ||||||
Journal articles | ||||||
5 | ||||||
University of Mandalay, Research Journal | ||||||
134 -144 | ||||||
11 |