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"Nenering Formation is essentially made up of semi-consolidated sediments, which are divided into basal conglomerate beds, conglomeratic sandstone, cross-bedded sandstone, and siltstone to muddy layers facies. It is overlie unconformable to the Berapit Formation, but conformable to the Kroh and Grik Formations. The stratigraphy of Nenering Formation is a fining upwards sequence where the thickness of conglomerate beds become thinner upwards and become thicker for conglomeratic sandstone. The thickness varies from 0.5 m to tenths of meters. The more sandy in the upper portion (cross-bedded sandstone) overlie with thin siltstone and mudstone facies. The clast and grain composition suggested that the material making up the sedimentary sequence were derived predominantly from the erosion of granitoid rocks and sedimentary and metamorphic rocks constitute a minor provenance. Imbrications and the trend sizes of clasts indicate that the palaeo-current flow toward northeast. Cross bedding that was found in conglomerate and sandstone indicates the main channel depositional environment. The sequence stratigraphy of this area match with the Saskatchewan fluvial braided channel model."

"Archaeological sites of Pengkalan Bharu, Perak is one of the important ports in Malaysia. The port is associated with the center of the Government of New Beruas. Establishment of the port city is to anticipate the enemy like a pirate attack of siam, Aceh, Maja-pahit, selangor and Portuguses."

"Lokasi penelitian ini berada di daerah Kecamatan Cimanggu dan sekitarnya yang secara geografis terletak pada koordinat batas timur laut UTM 262370 E 9198862 N serta batas barat daya UTM 256431 E 9192930 N. Wilayah ini mencakup Desa Cijati, Pesahangan, Desa Negarajati, serta desa sekitarnya, Kecamatan Cimanggu, Kabupaten Cilacap, Jawa Tengah. Daerah penelitian termasuk ke dalam Formasi Halang berdasarkan Peta Geologi Lembar Majenang (Kastowo dan Suwarna, 1996). Formasi Halang merupakan salah satu Formasi pengisi Cekungan Banyumas, terendapkan pada umur Miosen Tengah hingga Pliosen Awal, dengan dominasi batuan sedimen jenis turbidit yang terendapkan pada zona batial atas. Batuan sedimen jenis turbidit inilah yang menjadi fokus penelitian kali ini untuk mengetahui fasies endapan turbidit serta asosiasinya agar dapat menenentukan sub-lingungan pengendapan pada daerah penelitian. Bagian timur laut daerah penelitian didominasi oleh ukuran butir yang lebih kasar sedangkan pada bagian barat daya didominasi oleh butiran yang lebih halus. Daerah penelitian terbukti terendapkan dengan mekanisme turbidit dikarenakan jenis litologi yang beragam, dari yang berbutir kasar (breksi – pasir sedang) hingga berbutir halus (pasir halus – lanau). Didapatkan umur relatif Formasi Halang yang mencakup daerah penelitian pada Miosen Tengah (N11) berdasarkan analisis mikrofosil. Berdasarkan pengukuran measuring section, analisis makroskopis dan mikroskopis, didapatkan 5 lintasan log stratigrafi yang memiliki fasies dominan proksimal pada timur laut dan medial pada barat daya berdasarkan klasifikasi dekatnya dari sumber sedimen (Nichols, 2009). Diasosiasikan dengan sub-lingkungan pengendapan kipas laut dalam (submarine fan) dan diinterpretasikan merupakan bagian inner fan dan middle fan, dengan tiga fasies pengendapan channel dan levee serta depositional lobes berdasarkan Nichols (2009).

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The location of this research is in the Cimanggu region and its surroundings which is geographically located at the coordinates of the northeastern boundary of UTM 262370 E 9198862 N and the southwest boundary of UTM 256431 E 9192930 N. This area includes Cijati Village, Pesahangan, Negarajati Village, and the surrounding villages, Subdistrict Cimanggu, Cilacap Regency, Central Java. The research area is included in the Halang Formation based on the Geological Map of the Majenang Sheet by Kastowo and Suwarna (1996). The Halang Formation is one of the filling formations of the Banyumas Basin, deposited in the Middle Miocene to Early Pliocene age, with the dominance of turbidite sedimentary rocks deposited in the upper bathial zone. This turbidite sedimentary rock is the main focus of this research to determine the turbidite depositional facies and their associations in order to determine the sub-environment of the deposition in the study area. The northeastern part of the study area is dominated by coarser grain sizes, while the southwest is dominated by finer grains. The study area was proven to be deposited by a turbidite mechanism due to the various types of lithology, from coarse-grained rocks (breccia – medium sand) to fine-grained rocks (fine sand – silt). The relative age of the Halang Formation which covers the study area is in the Middle Miocene (N11) based on microfossil analysis. Based on measuring section measurements, macroscopic and microscopic analysis, obtained 5 stratigraphic log paths which have dominant facies proximal to the northeast and medial to the southwest based on the close classification of sediment sources (Nichols, 2009). Associated with sub-depositional sub-environment of submarine fans and interpreted as part of the inner fan and middle fan, with three depositional facies channel, levee and depositional lobes based on Nichols (2009)."

"This fully revised and updated edition introduces the reader to sedimentology and stratigraphic principles, and provides tools for the interpretation of sediments and sedimentary rocks."

"[ABSTRAKStudi karakterisasi reservoar merupakan salah satu studi dalam menginterpretasi reservoiar berdasarkan pada data bawah permukaan. Karakterisasi reservoir dalam penelitian ini dilakukan pada lapangan RCS yang merupakan lapangan dengan reservoar utama berupa batuan karbonat terumbu pada Formasi Tuban. Studi karakterisasi reservoar batuan terumbu sangat menarik dan pada penelitian ini dilakukan dengan pendekatan analisis petrofisik, analisis FZI dan analisis Elektrofasies. Dari keseluruhan hasil analisis ini terdapat lima tipe batuan melalui data batuan inti. Nilai FZI bervariasi mulai dari 0.145 ? 9. Nilai PHIE dan SWT bervariasi pada masing-masing yang akan dipakai pada analisis Elektrofasies. Dari hasil analisis elektrofasies terdapat lima tipe batuan di sepanjang zona interval batuan inti. Kemudian dari kombinasi keseluruhan hasil analisis ini didapat interpretasi lingkungan pengendapan bahwa lingkungan pengendapan fasies ini berada pada lingkungan carbonate platform pada bagian back barrier hingga barrier.

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ABSTRACT

Reservoir characterization study is one of a study based on the subsurface data reservoiar interpretation. Reservoir characterization for this study conducted at the RCS field with the main reservoir is carbonate rock reefs in the Tuban Formation. Reef carbonate reservoir characterization study is very interesting and in this study the research conducted by using petrophysical analysis, FZI analysis and elektrofasies approach. From the overall results of this analysis, there are five types of rock through the core rock data. FZI values ranging from 0.145 - 9. Value of PHIE and SWT varies on each that will be used in the analysis of elektrofasies. From the analysis of elektrofasies there are five types of rocks along the core interval. Then from the combination of the overall results of the analysis obtained with depositional environment interpretation that this facies depositional environment is in the carbonate platform expecially at the back barrier to barrier., Reservoir characterization study is one of a study based on the subsurface data reservoiar interpretation. Reservoir characterization for this study conducted at the RCS field with the main reservoir is carbonate rock reefs in the Tuban Formation. Reef carbonate reservoir characterization study is very interesting and in this study the research conducted by using petrophysical analysis, FZI analysis and elektrofasies approach. From the overall results of this analysis, there are five types of rock through the core rock data. FZI values ranging from 0.145 - 9. Value of PHIE and SWT varies on each that will be used in the analysis of elektrofasies. From the analysis of elektrofasies there are five types of rocks along the core interval. Then from the combination of the overall results of the analysis obtained with depositional environment interpretation that this facies depositional environment is in the carbonate platform expecially at the back barrier to barrier.]"