PROVENANCE STUDIES OF SANDSTONE FROM WALAT FORMATION, LOCATED IN CIBADAK, SUKABUMI, WEST JAVA

• Main Author: Ismiyati
• Format: Theses
• Language: Indonesia
• Online Access: https://digilib.itb.ac.id/gdl/view/47248
• Institution: Institut Teknologi Bandung

The Walat Formation is an Paleogen siliciclastic sedimentary rock formed in the Bogor Basin. This formation is composed mainly of quartz sandstones, quartz conglomerates, carbonaceous clays, lignites and thin layers of coal with a depositional environment in the form of fluvial to deltaic systems. Outcrops of this formation are widespread in the Cibadak area such as in Gunung Walat, the Sand Bongkok Complex, Aseupan Sand, and the Cicareuh River. Several studies have been done before on this formation. However, studies on provenance by combining petrographic and geochemical methods are still rarely conducted, especially in the research area. This is the basis of this study. The data used in this study consisted of field data and previous research literature. The location of field data collection is located in the south of Gunung Walat, precisely in the Holcim Educational Forest (HEF) using the measured stratigraphic method. A total of 18 sandstone samples were using the petrographic method and eight samples were analyzed using the geochemical method. From one existing track, three facies were identified, namely Sp (planar-cross-bedded sand), Gh (clast supported, horizontally stratified gravel), and Fl (laminated sand, silt, and mud). This facies distribution is based on lithology, grain size, and sedimentary structure. Petrographic data indicate that the sandstones of the Walat Formation are mostly lithic arenite, sublithic arenite, and graywacke. Comparison of QFL composition shows that all sandstones come from orogenic deposits with Q compositions (78.51% - 97.74%), F (0 - 1%), and L (2.26% - 21.13%) meanwhile, QmFLt comparisons show originating from quartz recycled (three samples), transitional recycled (11 samples), and lithic recycled (four samples). Furthermore, from the results of the geochemical analysis of the main elements in the bivariate diagram, the source rock of the Walat Formation comes from quartozes sedimentary provenance with a tectonic order in the form of a passive margin.