Depositional facies of the subsurface Neogene Surma Group in the Sangu Gas Field, the Bay of Bengal: records for tidal sedimentation

Author:

Akter Shirin,Akhter Waheda,Rahman M. Julleh JalalurORCID,Hossain Md. Sakawat

Publisher

Springer Science and Business Media LLC

Reference51 articles.

1. Alam, M. M. (1995). Tide-dominated sedimentation in the upper Tertiary succession of the Sitapahar anticline, Bangladesh. International Association of Sedimentologists Special Paper, 24, 329–341.

2. Bakhtine, M. I. (1966). Major tectonic features of Pakistan: Part II. The Eastern Province. Science & Industry, 4, 89–100.

3. Energy, C. (1998). Sangu field evaluation report (Geology and Geophysics). Edinburgh, 1, 2–6.

4. Cant, D. J. (1992). Subsurface facies analysis. In R. G. Walker & N. P. James (Eds.), Facies models: Response to sea level change. Geological Association of Canada (pp. 27–45). Newfoundland: St. John’s.

5. Curray, J. R. (1991). Geological history of the Bengal geosyncline. Journal of Association of Exploration Geophysicists, XII, 209–219.

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