Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Lin Thu Aung"'
Autor:
Fangyi Tan, Benjamin P. Horton, Lin Ke, Tanghua Li, Jennifer Quye-Sawyer, Joanne T. Y. Lim, Dongju Peng, Zihan Aw, Shi Jun Wee, Jing Ying Yeo, Ivan Haigh, Xianfeng Wang, Lin Thu Aung, Andrew Mitchell, Gina Sarkawi, Xinnan Li, Nurul Syafiqah Tan, Aron J. Meltzner
Publikováno v:
Scientific Reports, Vol 14, Iss 1, Pp 1-16 (2024)
Abstract Late Holocene relative sea-level (RSL) data are important to understand the drivers of RSL change, but there is a lack of precise RSL records from the Sunda Shelf. Here, we produced a Late Holocene RSL reconstruction from coral microatolls i
Externí odkaz:
https://doaj.org/article/8d6b88fb3c4643f98a9ca2c7a94163a6
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:
Lin Thu Aung, Martin, Stacey Servito, Wang, Yu, Wei, Shengji, Myo Thant, Khaing Nyein Htay, Hla Myo Aung, Tay Zar Kyaw, Soe Min, Kaung Sithu, Tun Naing, Saw Ngwe Khaing, Kyaw Moe Oo, Suresh, G., Chen, Weiwen, Phyo Maung Maung, Gahalaut, Vineet
Publikováno v:
In Tectonophysics 20 August 2019 765:146-160
Autor:
Gregory F. Moore, Tin Naing Tun, Eric Hellebrand, Rina Fukuchi, Win Min Than, Achim J Kopf, Lin Thu Aung, James C. Sample, Win Naing
Publikováno v:
Gondwana Research. 74:126-143
The western margin of Myanmar is the northern extension the active Sunda (India-Eurasia) subduction zone. Coastal regions and offshore islands have remarkable exposures of chaotic rock terranes along wave-cut terraces that allow characteristics of te
Autor:
Saw Ngwe Khaing, G. Suresh, Hla Myo Aung, Lin Thu Aung, Kyaw Moe Oo, Vineet K. Gahalaut, Khaing Nyein Htay, Kaung Sithu, Soe Min, Tay Zar Kyaw, Phyo Maung Maung, Tun Naing, Stacey S Martin, Yu Wang, Shengji Wei, Myo Thant, Weiwen Chen
Publikováno v:
Tectonophysics. 765:146-160
We map the distribution of macroseismic intensities from the MW 6.9 Kani and the MW 6.8 Chauk intra-slab earthquakes in 2016 in Myanmar using the 1998 European Macroseismic Scale (EMS-98) by interpreting data gathered from field surveys, community re
Autor:
null Tha Zin Htet Tin, Takuya Nishimura, Manabu Hashimoto, Eric O. Lindsey, Lin Thu Aung, Saw Myat Min, Myo Thant
Publikováno v:
Journal of Asian Earth Sciences. 228:105125
Autor:
W N Tun, Phyo Maung Maung, Hong-Wei Chiang, Guangxin Liu, Yanbin Lu, Shufang Yuan, Lin Thu Aung, Sakonvan Chawchai, Kyaw Moe Oo, Xianglei Li, Hai Cheng, Shaoneng He, Xianfeng Wang
Publikováno v:
Science Advances
Moisture transport pathway effect offsets glacial forcings, likely explaining a lack of G-IG variability in Chinese cave records.
While Asian monsoon (AM) changes have been clearly captured in Chinese speleothem oxygen isotope (δ18O) records, t
While Asian monsoon (AM) changes have been clearly captured in Chinese speleothem oxygen isotope (δ18O) records, t
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
Publikováno v:
Geological Society, London, Memoirs. 48:65-79
The Indo-Myanmar Ranges (IMR) of Myanmar, also known as the Indo-Burman Ranges (IBR) or the Western Ranges, extend from the East Himalayan Syntaxis (EHS) southwards along the eastern side of the Bay of Bengal to the Andaman Sea, comprising the Naga H
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