MIKROFASIES DAN DIAGENESA BATUGAMPING FORMASI ZAAG DI PULAU MISOOL DAN SEKITARNYA
DOI:
https://doi.org/10.34151/technoscientia.v3i1.430Keywords:
Zaag Formation, Packstone Facies and Grainstone Facies, DiagenesisAbstract
The study of carbonate rocks of Zaag Formation shows that the carbonate rock of Paleo-cene-Eocene occurred in Misool Island and outcropped among the rock of Paleozoik– Tertiary. The field survey shows that the Zaag Formation is outcropped at the mid part of the Misool Island from the west to east and also at several the surrounding small islands. The petrography analysis indicated that there are two facies forming the Zaag Formation, indicated found it was form at shoal environment of Packstone Facies and Grainstone Facies. The diagenesis process observed at the thin section is micritisation, cementation, dissolution and tectonic activity.
References
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Siregar M. Safei, 1985, Karbonat Formasi Waaf Berumur Kapur, di Pulau Misool, Majalah RISET Geologi dan Pertambangam , Jilid 6 No 2, 1985, Bandung
Siregar M. Safei, 1986, Endapan Karbo-nat Laut Dalam di pulau Misool, Proseding PIT XV IAGI, Yogyakarta.
Siregar M. Safei, Fred Hehuwat, Yono S. Atot, 1986, Geologi Batuan Fosfatan di Pulau Misool Irian Jaya, Proseding PIT XV IAGI, Yogyakarta.
Simbolon R., Martodjoyo S., Gunawan R., 1984, Geologi And Hydrocarbon Prospects of The PreTertiary System Of Misool Area, Procedings Indonesian Petroleum Association, Trirteenth Annual convention, May 1984.
Rusmana dkk, 1989, Peta Geologi Lemabr Misool, Pusat Survei Geologi, Bandung
Piagram C. J. et al, 1982, Lithostragraphy Of The Misool Archipelago, Iran Jaya, Indonesia, Geologie en Mijnbouw.p 265-279.
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Published
18-01-2019
How to Cite
Mulyadi, D. (2019). MIKROFASIES DAN DIAGENESA BATUGAMPING FORMASI ZAAG DI PULAU MISOOL DAN SEKITARNYA. JURNAL TEKNOLOGI TECHNOSCIENTIA, 3(1), 22–27. https://doi.org/10.34151/technoscientia.v3i1.430
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