alexa Facies Study of the Halang Formation Turbidites in Cibalung Area, Cimanggu District, Cilacap Regency, Central Java - Indonesia
ISSN: 2157-7617

Journal of Earth Science & Climatic Change
Open Access

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Research Article

Facies Study of the Halang Formation Turbidites in Cibalung Area, Cimanggu District, Cilacap Regency, Central Java - Indonesia

Yan Rizal R1*, Gentur Waluyo2, Septo Azis Irawan2 and Alfend Rudyawan1

1Fakultas Ilmu dan Teknologi, Kebumian Institut Teknologi, Bandung, Jl. Ganesha 10 Bandung 40132 Jawa Barat, Indonesia

2Program Studi Teknik Geologi, Fakultas Teknik, Universitas Jenderal Soedirman, JL. Mayjen Sungkono Km. 05, Purbalingga 53371, Indonesia

Corresponding Author:
Yan Rizal
Fakultas Ilmu dan Teknologi
Kebumian Institut Teknologi
Bandung, Bandung, West Java, Indonesia
Tel no: +62 22 2500935
E-mail: [email protected]

Received date: July 27, 2016; Accepted date: August 03, 2016; Published date: August 06, 2016

Citation: Yan Rizal R, Waluyo G, Irawan SA, Rudyawan A (2016) Facies Study of the Halang Formation Turbidites in Cibalung Area, Cimanggu District, Cilacap Regency, Central Java – Indonesia. J Earth Sci Clim Change 7:363. doi:10.4172/2157-7617.1000363

Copyright: © 2016 Yan Rizal R, et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

 

Abstract

The Halang formation consists of sandstones, mudstones and breccias. Facies study on the Halang Formation in Cibalung Area, Cimanggu District, Cilacap Regency, and Central Java has been carried out based on the detailed stratigraphic measurements along the Cikawung and Cimindi River. The Halang Formation can be divided into 7 lithofacies namely: A1, B1, B2, C2, D2, E2 and F2. The facies associations suggest that there are sub-depositional environment for the Halang Formation, which are slope, inner fan, middle fan and outer fan of the deep marine fan. Changes in depositional environment suggest a prominent influence from the sea level change during sedimentation that may also cause by the volcanic activity.

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