Limestone Microfacies of Baturaja Formation along Air Rambangnia Traverse, South OKU, South Sumatra

<p class="Pa4">DOI: <span><a href="http://dx.doi.org/10.17014/ijog.v1i1.173" target="_blank">10.17014/ijog.v1i1.173</a></span></p><p class="Pa4">Limestones of the Baturaja Formation occur at Air Rambangnia traverse, So...

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Bibliographic Details
Main Author: Sigit Maryanto
Format: Article
Language:English
Published: Geological Agency 2014-07-01
Series:Indonesian Journal on Geoscience
Subjects:
Online Access:https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/173
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Summary:<p class="Pa4">DOI: <span><a href="http://dx.doi.org/10.17014/ijog.v1i1.173" target="_blank">10.17014/ijog.v1i1.173</a></span></p><p class="Pa4">Limestones of the Baturaja Formation occur at Air Rambangnia traverse, South Ogan Komering Ulu, South Sumatra, and they are used as objects for microfacies studies. The microfacies studies are based on a detailed petro­graphic analysis of thirty four limestone samples, taken from the traverse. Four types of the limestones are identified such as wackestone, packstone, grainstone, and floatstone. At least five microfacies form the limestone succesion of the Baturaja Formation. They are interpreted as sedimentary facies of very restricted bay and pond, back reef local slope, slope and shelf edge, winnowed platform edge sand, and reef flank facies.</p> <p class="Pa4"> </p>
ISSN:2355-9314
2355-9306