No reef-rimmed margins to the Permian carbonate platforms of Thailand. / Dawson, Orapin; Baird, Angus; Bosence, Daniel.

In: Journal of Southeast Asian Earth Sciences, Vol. 8, No. 1-4, 1993, p. 181-186.

Research output: Contribution to journalArticlepeer-review

Published

Standard

No reef-rimmed margins to the Permian carbonate platforms of Thailand. / Dawson, Orapin; Baird, Angus; Bosence, Daniel.

In: Journal of Southeast Asian Earth Sciences, Vol. 8, No. 1-4, 1993, p. 181-186.

Research output: Contribution to journalArticlepeer-review

Harvard

Dawson, O, Baird, A & Bosence, D 1993, 'No reef-rimmed margins to the Permian carbonate platforms of Thailand', Journal of Southeast Asian Earth Sciences, vol. 8, no. 1-4, pp. 181-186. https://doi.org/10.1016/0743-9547(93)90019-L

APA

Dawson, O., Baird, A., & Bosence, D. (1993). No reef-rimmed margins to the Permian carbonate platforms of Thailand. Journal of Southeast Asian Earth Sciences, 8(1-4), 181-186. https://doi.org/10.1016/0743-9547(93)90019-L

Vancouver

Dawson O, Baird A, Bosence D. No reef-rimmed margins to the Permian carbonate platforms of Thailand. Journal of Southeast Asian Earth Sciences. 1993;8(1-4):181-186. https://doi.org/10.1016/0743-9547(93)90019-L

Author

Dawson, Orapin ; Baird, Angus ; Bosence, Daniel. / No reef-rimmed margins to the Permian carbonate platforms of Thailand. In: Journal of Southeast Asian Earth Sciences. 1993 ; Vol. 8, No. 1-4. pp. 181-186.

BibTeX

@article{5fdf34d32ec8431485fc557093d70f3e,
title = "No reef-rimmed margins to the Permian carbonate platforms of Thailand",
abstract = "In the central Thailand platform, marginal buildups (Early Permian) are formed mainly by fossiliferous grainstones with boundstones occurring only as small biostrome. Boundstones have a dominant skeletal element of encrusting Archaelithoporella and Tubiphytes with calcisponges and abundant syndepositional marine cements. This boundstone texture is similar to that of many other well documented Permian examples, such as El Capitan, U.S.A. and Trogkofel, Austria. In the Ratburi area of Peninsular Thailand, small bioherms (Middle Permian) are interbedded within grainstone shoals. Boundstone textures are matrix rich, with bryozoa, the main skeletal element and Tubiphytes, the main binding element. The Peninsular Thailand buildups formed on platform interior ridges and not in a shelf marginal position. These small biostromal and biohermal buildups in central and Peninsular Thailand did not form massive shelf-margin reef bodies as have been described from Permian platforms in western U.S.A. and southern China.",
author = "Orapin Dawson and Angus Baird and Daniel Bosence",
year = "1993",
doi = "10.1016/0743-9547(93)90019-L",
language = "English",
volume = "8",
pages = "181--186",
journal = "Journal of Southeast Asian Earth Sciences",
issn = "0743-9547",
publisher = "Pergamon Press Ltd.",
number = "1-4",

}

RIS

TY - JOUR

T1 - No reef-rimmed margins to the Permian carbonate platforms of Thailand

AU - Dawson, Orapin

AU - Baird, Angus

AU - Bosence, Daniel

PY - 1993

Y1 - 1993

N2 - In the central Thailand platform, marginal buildups (Early Permian) are formed mainly by fossiliferous grainstones with boundstones occurring only as small biostrome. Boundstones have a dominant skeletal element of encrusting Archaelithoporella and Tubiphytes with calcisponges and abundant syndepositional marine cements. This boundstone texture is similar to that of many other well documented Permian examples, such as El Capitan, U.S.A. and Trogkofel, Austria. In the Ratburi area of Peninsular Thailand, small bioherms (Middle Permian) are interbedded within grainstone shoals. Boundstone textures are matrix rich, with bryozoa, the main skeletal element and Tubiphytes, the main binding element. The Peninsular Thailand buildups formed on platform interior ridges and not in a shelf marginal position. These small biostromal and biohermal buildups in central and Peninsular Thailand did not form massive shelf-margin reef bodies as have been described from Permian platforms in western U.S.A. and southern China.

AB - In the central Thailand platform, marginal buildups (Early Permian) are formed mainly by fossiliferous grainstones with boundstones occurring only as small biostrome. Boundstones have a dominant skeletal element of encrusting Archaelithoporella and Tubiphytes with calcisponges and abundant syndepositional marine cements. This boundstone texture is similar to that of many other well documented Permian examples, such as El Capitan, U.S.A. and Trogkofel, Austria. In the Ratburi area of Peninsular Thailand, small bioherms (Middle Permian) are interbedded within grainstone shoals. Boundstone textures are matrix rich, with bryozoa, the main skeletal element and Tubiphytes, the main binding element. The Peninsular Thailand buildups formed on platform interior ridges and not in a shelf marginal position. These small biostromal and biohermal buildups in central and Peninsular Thailand did not form massive shelf-margin reef bodies as have been described from Permian platforms in western U.S.A. and southern China.

U2 - 10.1016/0743-9547(93)90019-L

DO - 10.1016/0743-9547(93)90019-L

M3 - Article

VL - 8

SP - 181

EP - 186

JO - Journal of Southeast Asian Earth Sciences

JF - Journal of Southeast Asian Earth Sciences

SN - 0743-9547

IS - 1-4

ER -