Article Per Year (5 Year)
p-Index From 2021 - 2026
0.23
P-Index
This Author published in this journals
All Journal Journal of Geoscience, Engineering, Environment, and Technology Jurnal Geologi dan Sumberdaya Mineral (Journal of Geology and Mineral Resources)
Ismawan Ismawan
Faultas Teknik Geologi Universitas Padjadjaran
Chemistry Earth & Planetary Sciences Energy Engineering Environmental Science Physics

Published : 3 Documents Claim Missing Document
Claim Missing Document
Check
Articles

Found 3 Documents
Search

 1 
Characterization of Basement Fracture Reservoir In Field ‘X’, South Sumatera Basin, Based On The Analysis of Core And FMI Log Hartawi Riskha; Ildrem Syafri; Ismawan Ismawan; Nanda Natasia
Journal of Geoscience, Engineering, Environment, and Technology Vol. 2 No. 2 (2017): JGEET Vol 02 No 02 : June (2017)
Publisher : UIR PRESS

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (3544.342 KB) | DOI: 10.24273/jgeet.2017.2.2.196

Abstract

Basement reservoir is a reservoir that is located in the basement rock, comprised of either igneous rock or metamorphic rock that has secondary porosity, resulting in its capability to store oil and gas. The research was conducted at field 'X' that is located at South Sumatra basin and it is a part of Jambi Sub-Basin. The study was focused on discussing hydrocarbon potential in Fields 'X', particularly at the basement metamorphic rock. The study was conducted at two wells in the field. The secondary porosity system of the basement is fracture porosity. Fracture analysis as secondary porosity system was performed on two wells, HA-1 and HA-2, by using FMI log interpretation. Based on the analysis of fracture on HA-1 well, the trend of fracture system is Northeast - Southwest (NE-SW) with a fracture porosity of 1.49%. On a different note, the trend of fracture system on HA-2 wells is East Northeast - West Southwest (ENE-WSW) with a fracture porosity of 0.888%. The effect of rock properties itself has little influence on the number of fractures as opposed to the effect of surrounding tectonic forces. The fractures are controlled by geological structures following Jambi pattern that has an orientation of Northeast - Southwest (NE-SW). Although the fracture porosity is relatively small, it is enough to storing hydrocarbons in economical quantity.
Structure and Tectonic Reconstruction of Bayah Complex Area, Banten Jemi Saputra Ahnaf; Aton Patonah; Haryadi Permana; Ismawan Ismawan
Journal of Geoscience, Engineering, Environment, and Technology Vol. 3 No. 2 (2018): JGEET Vol 03 No 02 : June (2018)
Publisher : UIR PRESS

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (2167.168 KB) | DOI: 10.24273/jgeet.2018.3.2.1554

Abstract

The research aimed to reconstruct the geological structures and tectonics of the Bayah complex area. The structures found that grouped into regional structural patterns used to determine the ages and the events that responsible to its formation. The methods used in this research include field and studio method. Field method carried out to map the outcrops and record geological structures data using geological compass, GPS, tape measurement, and geological hammer, while studio method performed to process and analyze data using software such as Win Tensor, Dips, MapInfo Professional 10.5 and CorelDraw X4. The geological structure of the Bayah has varying patterns and ages. The fracture patterns show N-S and E-W direction which is belong to Sundanese and Java Pattern formed in range of the Early Eocene to Pliocene. While the faults that have direction of SW-NE and E-W are classified into Meratus and Java Pattern. However, metamorphic rock foliations show NW-SE and N-S direction that belonging to the Pre-Tertiary Sumatra Pattern. The three faults of this research are estimated to be formed by the effect of orogenesis that occurring in different events and ages. JSA-014 fault is predicted to form due to orogeny I or orogeny II in the Early Oligocene - Middle Miocene, this fault classified as the 2nd order right lateral wrench fault. JSA-034 fault is formed by orogeny I in Early Oligocene - Middle Miocene, this fault is also classified as the 2nd order right lateral wrench fault. While JSA-080 fault has relatively young age that formed due to orogeny III in the Middle Miocene - Pliocene and belonging to the 3rd order left lateral wrench fault.
Potensi Penguatan Gelombang Gempabumi oleh Sedimen Permukaan Berdasarkan Analisis Mikrotremor: Studi Kasus di Cekungan Bandung Bagian Selatan Robby Setianegara; Dicky Muslim; Ismawan; Marjiyono
Jurnal Geologi dan Sumberdaya Mineral Vol. 24 No. 2 (2023): JURNAL GEOLOGI DAN SUMBERDAYA MINERAL
Publisher : Pusat Survei Geologi

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.33332/jgsm.geologi.v24i2.749

Abstract

Besarnya intensitas goncangan akibat gempabumi pada suatu wilayah tidak hanya bergantung kepada kekuatan (magnitudo) ataupun jarak terhadap sumber gempabumi akan tetapi sangat dipengaruhi juga oleh kondisi geologi setempat (site response). Penelitian ini dimaksudkan untuk memperkirakan tingkat penguatan gelombang gempabumi di wilayah Cekungan Bandung bagian selatan. Metode yang digunakan dalam penelitian ini adalah kombinasi mikrotremor array dan mikrotremor single station, dimana pemodelan kondisi bawah permukaan didekati model sederhana dua lapis dengan mempertimbangkan kontras kecepatan gelombang geser terbesar. Hasil penelitian menunjukkan bahwa kecepatan gelombang geser lapisan sedimen permukaan di daerah ini berkisar antara 150 - 330 m/detik, sedangkan kecepatan gelombang geser batuan yang mengalasi sedimen permukaan berkisar 240 - 500 m/detik yang diduga masih merupakan fasies endapan danau yang lebih tua. Hasil perhitungan nilai penguatan gelombang gempabumi oleh lapisan sedimen permukaan diperoleh nilai 1,05 - 2,0 dengan zona berpenguatan gelombang (site amplification) tinggi menempati pada pinggir cekungan. Kata kunci: Cekungan Bandung, mikrotremor array, mikrotremor single station, penguatan gelombang
Co-Authors Aton Patonah Dicky Muslim Hartawi Riskha Haryadi Permana Ildrem Syafri Jemi Saputra Ahnaf Marjiyono Nanda Natasia Robby Setianegara