The upper paleozoic pebbly mudstone facies of peninsular Thailand and western Malaysia — Continental margin deposits of Paleoeurasia — Reply

Author:

Altermann Wladyslaw

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences,General Earth and Planetary Sciences

Reference5 articles.

1. Geol. Surv. Paper;S. Bunopas,1981

2. Burton, C. K. (1983): Stratigraphy and correlation of the Middle to Late Paleozoic in peninsular Thailand. - Proc. Workshop Strat. Correl. Thailand and Malaysia.,2, Had Yai, Thailand, Sept. 1983.

3. Burret, C. &Stait, B. (1984): Southeast Asia as a part of Early Paleozoic Gondwanaland. - GEOSEA V Proc. Vol. 1, Geol. Soc. Malaysia Bull. 19, April 1986, 103–107.

4. Grant, R. E. (1976): Permian brachiopods from southern Thailand. - J. Paleont.50, Part II of II, Suppl. to No.:3, The Paleont. Soc. Mem. 269pp.

5. Mc Elhinny M. W., Haile, N. S. &Crawford, A. R. (1974): Paleomagnetic evidence shows Malay Peninsula was not a part of Gondwanaland. - Nature,252, Dec. 20/27, 641–645.

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