Research Publications

Academic theses and dissertations are regularly published and widely disseminated in YUOE Journal, Monographs, Universities Research Journal (URJ), Myanmar Academy of Arts and Science (MAAS) Journal, AsTEN Research Journal and International online Journals for sharing knowledge and contributing to the development of our education.

Myanmar Academy of Art & Science List of Research

No. Researcher Title Abstract Year
651 Thida Lwin ?????????? ?????????????????????????????? ????????? ?????????? ?????????? ?????????????????????????????? ????????? ?????? ?????????? ??????????????? ???????????????????????????? ???????? ???????????? ????????????????????????? ???????????? ????? ?????????????????? ?????????????????????? ????????????? ?????? ?????????? ?????????????????????????????? ???????????? ??????????? (?) ????? (?) ???????????????????? (?) ????????????? ????? ???????????????????????? ???????????? ?????????????? ???????????? ?????????????????? ??????????? ???????? ?????? ?????????????????? ?????????????????? ????????????????? ???????????????? ??????????????????????????? ???????????????? ???????? ??????????????????? 2019
652 Si Si Win ???????? ???????????????????????? ?????????? ???????? ??????????????????????????? ?????????? ?????? ?????????????? ?????????? ?????????????????? ??????????? ??????????????????? ????????????? ????????????????? ??????????????? ??????? ?????????????????????? ??????????? ?????(?) ???????? ????????? ?????(?) ???????? ???????????????????????????? ????? ???? ???????? ??????????? ?????????????????????? ????????? ?????????? ?????????? ??????????????????? 2019
653 San San Htay ????????????????????????? ???????? ?????? ?????????????????? ?????????? ???????????????? ????????????? ????????? ??? ???????? ???????? ??????????????????????????????? ????????????? ?????? ???????????????? ?????????? ?????(?)???????? ????? ?????????????? ?????(?) ??????????????????????????? ?????(?) ?????????????? ?????(?) ??????????????????? ?????? ????????????? ????????? ?????????? ????????????????????????? ???????? ?????????????? ?????????????????? ???????????? ???????????????????????? ???????? ?????????????? ????????????? ?????????????? ????????? ????????????? ?????? 2019
654 Thiri Yandana Khaing Mon Mon Thein ????????????? ????????????????? ???????????????? ?????????? ?????????????? ????????????? ??????????????? ????????????? ?????????????????? ??????????????????? ?????????? ?????? ???????????????? ?????????????????? ????????????? ?????? ??????????? ?????????????? ??????????? ????????????? ?????(?) ??????? ????????????????? ????????????? ???????????? ??????????? ?????????????????? ????????????????? ?????(?) ????????????? ?????????????????? ???????????????????? ????????????????????? ????????????????? ?????????????????????? ??????????????????? ????? ?????????????? ????????? ???????????????? ??????????? ??????? ???????????????? ??????????????????? ???????????????????? ?????????? 2019
655 Maw Maw Aung ????????????????????????????????? ?????????? ?????????????????????? ?????????(?)??????? ??????????????? ???????????????? ???????????????? ?????????? (?) ????????? ????? (?) ?????????????????? ???????? (?)?????????? ?????????? ?????????? ?????? ???? (?)??? ??????????? ??????? ???????????????????? ????????????????? ????????????? ??????? ?????????? ???????? ??????????????? ???????????????? ????????? ??????????????????? ?????????????????????? ?????????????????????? ???????????????????? ?????????????? ??????? ????????????? 2019
656 Theint Theint Oo ???????????????? ???????????????????????????????? ??????????? ???????????????? ????????? ]?????????} ??????? ????????????? ?????????????????????????? ?????????????? ]?????????} ???????? ????????????????? ?????????????????????? ?????? ????? ???????????? ?????????? ????????????? ????? ???????? ]?????????} ???????? ??????????? ?????????????????????? ????????????? ????????????????????????? ??????????????????????????????? ?????????? ??????????????????????? ???????? ??????????????? ?????(?)???? ]?????????}?????????????? ?????????????????????????????????? ?????(?)???? ????????????? ???????????????????????????? ?????(?)???? ]?????????} ?????????????? ????????????? ??????????????????????? ??????????? 2019
657 Ei Ei Mon ???????????????? ??????????????? ????????? ?????????? ?????????????????????? ???????????????? ?????? ?????????? ????????????? ?????????????????????? ????????????????? ?????? ?????????? ?????????? ??????????? ?????????????????? ??????? ???????????????????? ??????????????? ??????????????????????? ???????????????? ?????????? ????????????? ????????????? ???????????????? ????????????? ??????????????????????????????????? ???????? ????? ?????? ??????????? ?????????? ??????????? ?????(?) ???? ?????? ?????(?) ????????????????????????? ?????(?) ???????????????? ??????????????? ???????????? ????????????? ????????? ???????????????? ??????????????? ??????????????????????? ??????????????? ??????????????????????? ??????????????????? ???? ??????????????????????? ?????????????? ?????????? ????????? ????????? ???????????????? ???????????????? ?????????????????????? 2019
658 Thet Hnin Aye ??????? ???????????????? ?????????????? ???????????????? ?????????? ????????????????????????? ?????????????????? ???????? ??????????????????????????? ???????????????????????? ???????????????? ?????????? ??????????? ??????????????? ?????? ?????????? ?????????????????????????????????? ??????? ???????????????? ????????????????? ????????????? ????????????? ?????????????? ??????????????? ?????????????? ??????????? ????????? ?????????? ????????????? ??????????????? ??????????????? ??????????? ?????? ???? ??????????? ?????(?) ????????????? ?????(?) ???????? ?????? ???????????????????? ?????(?) ??????? ???????????????? ?????????????? ??????????????????????? ??????????????????? ?????????????? ?????????????????????????? ???????????????????? ???? ??????????? 2019
659 Dr Ye Kyaw Thu METAMORPHIC CONDITIONS OF HIGH–GRADE MARBLES FROM MOGOK–KYATPYIN AREA OF THE MIDDLE SEGMENT OF THE MOGOK METAMORPHIC BELT, CENTRAL MYANMAR* The Mogok-Kyatpyin area forming a mountainous region with two distinct valleys of Mogok valley and Kyatpyin valley is well known for its gem minerals. A variety of marbles, calc-silicate rocks, gneisses, migmatites and locally granulites are well exposed with the emplacement of various types of granitoid rocks. The high-grade assemblages of marble samples are characterized by calcite + dolomite + diopside + spinel + graphite with forsterite and clinohumite in some samples. Based on the mineral assemblages and textural relationship, temperature and fluid (T-XCO2) diagrams indicate temperature and XCO2 conditions of > 800 °C and > 0.5 at an isobaric pressure of 0.8 GPa for the clinohumite-bearing and forsterite-bearing marble samples for the peak stage. Re-equilibrium texture of clinohumite + tremolite + dolomite indicates a decrease in temperature and XCO2 condition, and yields <540 °C and <0.02 at an isobaric pressure of 0.4 GPa. The present study combining with other high-grade areas along the Mogok metamorphic belt suggest widespread distribution of upper amphibolite to granulite facies metamorphism in the middle segment including Mogok-Kyatpyin area. During peak metamorphic stages, the fluid conditions had higher XCO2 value. In contrast, decreasing XCO2 values with decreasing temperature and pressure might indicate that infiltration of H2O-rich fluid occurred during retrograde metamorphism. 2020
660 Teza Kyaw PETROLOGY OF IGNEOUS ROCKS EXPOSED IN KHUNTHA-MINDAW AREA, SALINGYI TOWNSHIP The Khuntha-Mindaw area is situated in part of the 45-km long Monywa-Salingyi segment of Western Myanmar magmatic arc (WMA). Lithologically, the area comprises diorite, granite, gabbro, and pegmatite of intrusive and basalt, andesite, dacite and rhyolite of extrusive rocks which are formed during Cretaceous. These igneous rocks are overlain by Oligocene to Pliocene clastic sedimentary units with locally Upper Oligocene-Lower Miocene limestone. The mineral composition and textures of diverse rock units are analyzed and interpreted by binocular polarizing microscope and chemical composition by XRF from Department of Chemistry, Monywa University. Mineralogically, the volcanic rocks contain more than 20% phenocrysts of plagioclase feldspar, pyroxene, hornblende, biotite and quartz embedded in microlites to crystallites groundmass. The zoning, cumulophyric and resorbed textures indicate the fractional crystallization and magma mixing igneous activity in long-lived evolving magma. The multiple twinned plagioclase with interstitial quartz and orthoclase in granites suggest the calc-alkaline plutonic rocks. Petrochemically, the plutonic and volcanic rocks in the study area belong to the subalkaline series and falls within the calc-alkaline suite. Moreover, the major chemical compositions of the plutonic rocks fall within I-type and S-type granitoid field. Thus all igneous rocks exposed in the present area may be erupted from subduction related calc-alkaline magmatic volcanic-arc of convergent plate margins. 2020