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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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c7f054d03c1d4ee0991b13b5e6e8cbaf
https://doi.org/10.1144/m48.21
https://doi.org/10.1144/m48.21
Publikováno v:
Memoirs Special Publications; 2017, Vol. 48 Issue 1, p453-471, 19p