Subsurface resistivity images of the Belik area, Purbalingga based on magnetotelluric data, implication for hydrocarbon exploration
Penulis: Eddy Z GaffarThe study area is an area of hydrocarbon potential located in Belik Area, Central Java. From the results of seismic survey, it seen that the depth of about 2000 meters is still visible, but the signal of the seismic instrument could not penetrate deeper than 2000 meters. Therefore, Research Center for Geotechnology did an alternative method of magnetoteluric with trending north-south trajectory. Based on Djuri 1996, the stratigraphy of the study area consists of Tertiary to the Quaternary rocks. From the oldest is Pemali Formation, Rambatan Formation, Halang Formation, Kumbang Formation, Tapak Formation, Kalibiuk Formation, Ligung Formation and Alluvial. Pemali Formation consists of marl, Rambatan Formation consists of shale, marl and calcareous sandstone, Halang Formation consists of sandstone, conglomerate and marl, Kumbang Formation consists of breccia, andesite lava and tuff, Tapak Formation consists of breccia and limestone, Kalibiuk Formation consists of silty marl and sandstone Ligung Formation consists of agglomerates, breccias, tuffs and clays. Kumbang Formation is an igneous rock as sill with a thickness of up to 2000 meters and is a breakthrough that layered rocks parallel to the rock above and below. Resistivity image of the north-south trajectory is seen a layer with high resistivity more than 1000 OhmM. It is interpreted as Kumbang Formation and underneath there is a layer with resistivity values lower than Kumbang Formation is interpreted as Halang Formation, Rambatan Formation and Pemali Formation. It is concluded that magnetotelluric method could penetrate very high resistivity layer and thick enough where seismic method can not penetrate.
AIP Conf. Proc. 1712, 040005 (2016)
ISSN / ISBN / IBSN : 978-0-7354-1359-7
DOI: doi: 10.1063/1.4941882
No. Arsip : LIPI-16024