Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Cherdsak Utha-Aroon"'
Publikováno v:
Sedimentary Geology. 157:235-252
The Khorat Plateau of northeast Thailand and Laos was an area of widespread deposition of evaporites and siliciclastics (Maha Sarakham Formation) during the Cretaceous and three types of dolomites are associated with this formation: (1) limpid dolomi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::93c2fe3e86c409e863de1ca170b6f312
https://doi.org/10.1016/s0037-0738(02)00235-x
https://doi.org/10.1016/s0037-0738(02)00235-x
Publikováno v:
Sedimentary Geology. 123:31-62
Evaporites of the Cretaceous to early Tertiary Maha Sarakham Formation on the Khorat Plateau of southeast Asia (Thailand and Laos) are composed of three depositional members that each include evaporitic successions, each overlain by non-marine clasti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1b97769d1f733af6b1fe5ecfc8500bb3
https://doi.org/10.1016/s0037-0738(98)00083-9
https://doi.org/10.1016/s0037-0738(98)00083-9
Autor:
Mohamed El Tabakh, Cherdsak Utha-Aroon
Publikováno v:
Sedimentary Geology. 121:97-119
In Thailand, during the Permian, an extensive carbonate platform developed on the margin of the Indochina Plate and near to a coeval and deeper siliciclastic-dominated marine basin. This basin separated the Indochina Plate, to the east, from the Shan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2831d999089de4535b61e863c97d14a3
https://doi.org/10.1016/s0037-0738(98)00064-5
https://doi.org/10.1016/s0037-0738(98)00064-5
Publikováno v:
Sedimentology. 45:579-594
Development of a diagenetic anhydrite bed at the base of the Cretaceous Maha Sarakham Saline Formation (the ‘Basal Anhydrite’ member) of the Khorat Plateau in north-eastern Thailand took place due to leaching and/or pressure dissolution of salt a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d3de5bbbc9a010f5bd534538590d446e
https://doi.org/10.1046/j.1365-3091.1998.00162.x
https://doi.org/10.1046/j.1365-3091.1998.00162.x
Autor:
Cherdsak Utha-Aroon
Publikováno v:
Journal of Southeast Asian Earth Sciences. 8:193-203
Recent sedimentologic analysis of the potash-bearing Maha Sarakham Formation (Upper Cretaceous) shows that it is not of marine origin as previously thought. The main reason is the lack of evidence suggesting transgression onto the underlying redbeds
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a4aef8a857c6fb2af6be850cf4863a65
https://doi.org/10.1016/0743-9547(93)90021-g
https://doi.org/10.1016/0743-9547(93)90021-g