Zobrazeno 1 - 10
of 45
pro vyhledávání: '"Soe Thura Tun"'
Publikováno v:
Journal of Asian Earth Sciences: X, Vol 4, Iss , Pp 100037- (2020)
Pyay sub-basin is located in the southern part of the Central Myanmar Forearc Basin, an elongate belt of en-echelon folds and thrust faults formed as a result of the hyper-oblique convergence of the India and Asia plates. Limited neotectonic studies
Externí odkaz:
https://doaj.org/article/ba0c53cf23e54fffa1b12f9c57f37b09
Autor:
Jean-Jacques Jaeger, Aung Naing Soe, Olivier Chavasseau, Pauline Coster, Edouard-Georges Emonet, Franck Guy, Renaud Lebrun, Aye Maung, Aung Aung Khyaw, Hla Shwe, Soe Thura Tun, Kyaw Linn Oo, Mana Rugbumrung, Hervé Bocherens, Mouloud Benammi, Kamol Chaivanich, Paul Tafforeau, Yaowalak Chaimanee
Publikováno v:
PLoS ONE, Vol 6, Iss 4, p e17065 (2011)
For over a century, a Neogene fossil mammal fauna has been known in the Irrawaddy Formation in central Myanmar. Unfortunately, the lack of accurately located fossiliferous sites and the absence of hominoid fossils have impeded paleontological studies
Externí odkaz:
https://doaj.org/article/6cffef1960a74b8cba0bc4c1b33ebb74
Autor:
Soe Thura Tun, Soe Min, Chuan-Chou Shen, Lin Thu Aung, Oo Than, Yu Wang, Sze-Chieh Liu, Hong-Wei Chiang, J. Bruce H. Shyu, Chung-Che Wang
Publikováno v:
Earth and Planetary Science Letters. 484:241-252
Upper-plate structures that splay out from the megathrusts are common features along major convergent plate boundaries. However, their earthquake and tsunami hazard potentials have not yet received significant attention. In this study, we identified
Autor:
Soe Thura Tun, Ian M. Watkinson
Publikováno v:
Geological Society, London, Memoirs. 48:413-441
The Sagaing Fault is amongst the longest and most active strike-slip faults in the world (e.g. Molnar & Dayem 2010; Robinson et al. 2010; Searle & Morley 2011). It accommodates more than half of the right-lateral motion between Sundaland and India wi
Publikováno v:
Geological Society, London, Memoirs. 48:453-471
The Kyaukkyan Fault is an active dextral strike-slip structure that passes 510 km north–south across the western Shan Plateau (e.g. Chhibber 1934; Le Dain et al. 1984; Wang et al. 2014) (Fig. 21.1a). It lies broadly parallel to and about 100–150
Publikováno v:
Journal of Asian Earth Sciences: X, Vol 4, Iss, Pp 100037-(2020)
Pyay sub-basin is located in the southern part of the Central Myanmar Forearc Basin, an elongate belt of en-echelon folds and thrust faults formed as a result of the hyper-oblique convergence of the India and Asia plates. Limited neotectonic studies
Autor:
Kerry Sieh, Kyaw Kyaw Lin, Chung-Che Wang, Soe Min, Thura Aung, Soe Thura Tun, J. Bruce H. Shyu, Yu Wang, Hong-Wei Chiang, Yu-Nung Nina Lin, Oo Than, Chuan-Chou Shen
Publikováno v:
Journal of Geophysical Research: Solid Earth. 118:1277-1303
The 1762 Arakan earthquake resulted from rupture of the northern Sunda megathrust and is one of those rare preinstrumental earthquakes for which early historical accounts document ground deformations. In order to obtain more comprehensive and detaile
Publikováno v:
Geophysical Journal International. 185:49-64
Field investigations of an ancient fortress wall in southern Myanmar reveal an offset of ~6 m across the Sagaing fault, the major right-lateral fault between the Sunda and Burma plates. The fault slip rate implied by offset of this 16th-century fortr
Publikováno v:
Journal of Earthquake and Tsunami. :43-57
Myanmar, lying in a major seismic belt, is indeed earthquake-prone and is vulnerable to hazards from moderate and large magnitude earthquakes, including tsunami hazards along its long coastal areas. The seismotectonics of the region indicates that ea
Autor:
Win Swe, Soe Thura Tun
Publikováno v:
Journal of Earthquake and Tsunami. :267-277
Wave-cut platforms, uplifted marine terraces, and areas of subsidence are among the most striking geomorphic features along some parts of the Myanmar coast. Depending on the local tectonic setting, processes of development of terraces of the Myanmar