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GEOMORPHOLOGIC AND STRATIGRAPHIC DETERMINATION USING OUTCROP DATA, THIN SECTION AND MICROFOSSIL ANALYSIS IN BENTARSARI AREA, BREBES DISTRICT, CENTRAL JAVA Dewi, Viska Triaraminta; Nurdrajat, Nurdrajat; Firmansyah, Yusi; Fachrudin, Kurnia Arfiansyah
Journal of Geological Sciences and Applied Geology Vol 2, No 6 (2018): Journal of Geological Sciences and Applied Geology
Publisher : Faculty of Geological Engineering, Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.24198/gsag.v2i6.20876

Abstract

Administratively, Bentarsari area was located in Salem Sub-District and Brebes District in Central Java Province with coordinate 108°46’45,15” - 108°49’28.29” BT - 108°39’32.4” BT and 7°7’40.34” LS - 7°10’22.22” LS.  This research aims is to give an understanding about geological condition in geomorphology and stratigraphy aspects which are described by thematic map in 1:12.500 scale within an area of 25km2. This research was accomplished with surface data (outcrop) and field orientation method using of GPS, geological compass, loop, geological hammer, comparator, and any other tools. Afterward, thin section and fossil analysis were also collected to determine the type of rocks and the age of the stratigraphy unit. This research will include the classification of geomorphology unit based on 3 aspects, which are morphography,  morphometry, and morphogenetic and also classification of stratigraphy unit, based on characteristics of rocks such as rock texture, mineral contents and fossil contents. The geomorphology of the Bentarsari region can be divided into 3 (three) geomorphological units, namely: the alluvium high altitude fluvial unit, high hills of steep structural sediments unit, and very steep high structural sedimentary hills unit. While the Litho-stratigraphic on research area divided into 4 (four) units, from the oldest to the youngest stratigraphy position is sandstone unit (Tbp), claystone unit (Tbl), fine-grained sandstone unit (Tpbph), and breccia unit (Qpbx). Thus, by having the result of this research, can be useful as a reference to have further studies in this located area. 
SISTEM POROSITAS RESERVOIR BATUAN KARBONAT PADA SEKUEN DROWNING CAP, FORMASI KUJUNG ATAS DI LAPANGAN VITA, CEKUNGAN JAWA TIMUR DEWI, VISKA TRIARAMINTA; Mardiana, Undang; Mohammad, Febriwan; Ahdyar, LaOde
Bulletin of Scientific Contribution Vol 17, No 2 (2019): Bulletin of Scientific Contribution : GEOLOGY
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (16869.888 KB) | DOI: 10.24198/bsc.v17i2.22992

Abstract

ABSTRAKBatuan karbonat merupakan batuan yang banyak ditemukan sebagai batuan reservoir. Hal ini tentu dikarenakan batuan karbonat memiliki nilai porositas dan permeabilitas yang baik. Namun, tingginya kompleksitas dan heterogenitas dari batuan karbonat membuat suatu kualitas reservoir batuan karbonat sulit di prediksi. Distribusi sistem porositas batuan karbonat sangat dikontrol oleh litofasies dan juga proses diagenesis. Maka, interaksi dari kedua faktor tersebut akan menghasilkan variasi jenis porositas yang nantinya akan mempengaruhi nilai permeabilitas dari suatu reservoir.Objek penelitian ini adalah Reservoir Vita yang merupakan karbonat build up, berumur Oligosen hingga Miosen di Formasi Kujung Atas. Reservoir ini telah menjadi produsen minyak terbesar di Indonesia dan saat ini telah menghasilkan sejumlah hidrokarbon yang banyak. Dengan menggunakan data batuan inti sepanjang 429 ft (keseluruhan) dan lebih dari 500 sayatan tipis pada 3 sumur, penelitian ini bertujuan untuk mengetahui variasi dari sistem pori pada sekuen Drowning Cap di Reservoir Vita. Analisa kualitatif dilakukan untuk mendeterminasi jenis porositas reservoir yang terdiri atas interparticle, separated vugs (moldic), touching vugs, microfracture, dan minimum dissolution. Kelima jenis porositas ini terbentuk pada litofasies yang berbeda-beda. Tentu hal ini menunjukkan bahwa, sistem porositas pada objek penelitian tidak hanya dikontrol oleh tekstur, melainkan oleh proses diagenesis yang terjadi. Pemahaman terkait sistem porositas di reservoir drowning cap ini tentu menghasilkan dampak yang baik untuk mengetahui distribusi kualitas reservoir yang komprehensif. Kata Kunci : Jenis porositas, diagenesis, Reservoir Batuan Karbonat  ABSTRACTCarbonate rocks known as one of a common major reservoir rock in the world due to its good porosity and permeability. However, its heterogeneity makes the variability of carbonate reservoir quality is difficult to predict. Carbonate pore system distribution is controlled by the lithofacies and also by the occurrence of diagenetic process. Therefore, this interaction results the variation of pore types that will eventually define the permeability of the reservoir.The object of this research is Reservoir Vita which is an Oligocene to Miocene carbonate build up reservoir, specifically in Drowning Cap Sequence. Vita Reservoir is located in East Java Basin, Upper Kujung Formation which has becoming the largest oil producer in Indonesia and currently it has been producing a significant amount of hydrocarbon. By using cores (429 ft in total) and more than 500 thin sections data from 3 wells, this research aims to observe the variety of total pore system in drowning cap sequence in Reservoir Vita. Qualitative analysis was done in determining the pore types of reservoir that consist of interparticle, separated vugs (moldic), touching vugs, microfracture, and minimum dissolution. These five pore types are encountered in wide variety of lithofasies or depositional facies. Thus, this observation has proved that the pore system distribution in research object, is not only mainly controlled by its texture, but also strongly controlled by diagenetic process and it results different value of porosity and permeability. Understanding of pore system in drowning cap reservoir will bring significant value comprehensive reservoir quality distribution.  Keywords: Pore types, Diagenetic prosses, Carbonate Reservoir