Limestone Facies And Diagenesis On Tondo Formation At Kaisabu Village Bau-Bau City Southeast Sulawesi Province

Authors

  • Muhammad Chaerul Universitas Halu Oleo
  • La Ode Ngkoimani Universitas Halu Oleo
  • Sofyan Sadri Universitas Halu Oleo

DOI:

https://doi.org/10.24273/jgeet.2017.2.1.14

Keywords:

Tondo Formation, Diagenesis, Limestone facies

Abstract

This study aims to determine the limestone facies and diagenesis on Tondo Formation. The method used was petrographic method bypolarizing microscope. Based on the physical characteristics and biota contained, the carbonate rocks on tondo formation (Tmtl) can be grouped into two facies, namely: Wackestone and Packestone. The diagenesis process that occurred in Tondo Formation research area is microbial micritization, cementation and neomorphism which indicate that the Tondo Formation has existed on diagenetic environment of marine phreatic, meteoric phreatic and meteoric vadose.

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References

Boggs, S., Jr., 1992, Petrology of sedimentary rocks; Macmillan Pub. Co., New York, 707 p.

Davidson, 1991, Regional Stratigraphy column of Buton Islands.

Dunham, R.J., 1962, Classification of Carbonate Rocks According to Depositional Texture, in Ham, E.E., ed.Classification of Carbonate Rocks, AAPG Memoir I, p. 108-121.

Flugel, E., 2004. Microfacies of Carbonat Rock. Springer, Inc, New York.

Longman, M. W.,1980. Carbonate Diagenetic Textures from Nearsurface Diagenetic Environment,Bulletin AAPG, 64, 461 -485.

Morrow, D. W., 1982. Diagenesis 2 : Dolomite, Part 2. The Geological Association of Canada.

Tucker, M.E., Wright, V.P., 1990. Carbonate Sedimentology. Blackwell Publishing Ltd., pp. 422–467. doi:10.1002/9781444314175.refs

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Published

2017-03-01

Issue

Vol. 2 No. 1 (2017): JGEET Vol 02 No 01 : March (2017)

Section

Research Articles

License

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