Two dimensions (2D) seismic profile of Baruna and Jaya lines at North-East Java Basin show seismic reflector characteristics that can be used to interpret sediment thickness and continuity. Those reflector characteristics that can be applied for seismic facies analysis that represents depositional environment. This study starts from seismic data processing that using Kirchhoff Post Stack Time Migration method which is 2D seismic profile as result. Seismic reflector characterization has been done to both 2D profiles. Seismic reflector characterization was grouped as (i) individual reflection, (ii) reflection configuration, (iii) reflection termination, (iv) external form. Individual reflection characteristics show high and medium amplitude, medium and low frequency, and continuous. Configuration reflection is continuous with parallel and subparallel type. Reflection termination shows on lap, and external form shows sheet drape. Local mound appearance can be interpreted as paleo-reef. Facies seismic analysis result for this study area is a shelf.
Geologically, the province of Central Sulawesi is composed of various types of rocks, both in the form of igneous, sedimentary and metamorphic rocks. Regarding Central Sulawesi Province, mineral resources both metal and non-metal are quite varied. Increasing demand and demand for minerals, both metals, and non-metals. Research conducted to study the mineral potential in one of the regencies in Central Sulawesi Province. This research was conducted in Galang Sub-district, Tolitoli Regency, and Central Sulawesi Province by using the resistivity method and the Induced Polarization (IP) method with the Wenner-Schlumberger arrangement consisting of eight lines. The IP method is very accurate to discuss the potential of minerals that are below the surface. The inversion process does data processing in order to obtain the actual form of resistivity and chargeability modeling. Based on the modeling, the mineral potential in Galang Sub-district, Tolitoli Regency, Central Sulawesi Province is mostly found in all trajectories namely lane 01; 02; 04; 05; 05; 06; 07. Which is marked by a very high chargeability value between 300 msec - 500 msec. The research area also discusses granite and andesite, which have high resistivity values, between 2000 Ωm – 400000 Ωm.
This research was conducted to determine and mapping the value of the PGA in Indonesian territory using two empirical models of attenuation equations from the transition of the second generation to the third generation. The research was conducted by applying the Frisenda’s and Luzi’s. The calculation is based on a catalog of earthquakes that occurred from 1 January 1970 - 31 December 2020 with a variable earthquake magnitude ≥ 5 SR and hypocentre depth ≤ 60 km (destructive earthquake). The calculation results in the maximum value of PGA respectively 0.6613 g for Frisenda, and 12.257 g in the Luzi. The maximum PGA value in Luzi model is the effects of the Andaman Islands earthquake on December 26th, 2004, with a magnitude of 9,1 SR, and the maximum PGA value in the Frisenda model is the effects of the Flying Fish Cove, Christmas Island earthquake on June 13th, 2013, with the magnitude 6.7 SR. In general, these two maps show different or even opposite patterns.
West Java is an area located in the subduction zone of two major plates of the world, Indo-Australian and Eurasian plates that cause high tectonic activity. This is marked by the number of earthquake events in this area. The accumulation of earthquake-induced shocks produces a ground movement. The ground movement provides various effects such as landslides, road fractures, cracks in walls and so on. These effects need to be addressed so that any activity to be performed on the surface can take place properly. There are some ground movement activity. One of them is Peak Ground Acceleration (PGA). This research was conducted to compare two models of Peak Ground Acceleration (PGA), Faccioli and Donovan. These models based on 50-years of catalog earthquakes event in period 1965-2015 on West Java with Magnitude ≥ 5 SR and the hypocentre ≤ 80 km. The results of this research will be compared with the 2010 Indonesian earthquake map.
Lapangan RB termasuk wilayah kerja blok Rangkas yang berlokasi di propinsi Banten memiliki Petroleum System yang sudah terbukti menghasilkan hidrokarbon. Di beberapa tempat terdapat rembesan minyak tetapi masih belum ada kajian yang mendalam mengenai potensi batuan reservoir penghasil hidrokarbon tersebut. Studi ini dilakukan untuk menentukan jenis litologi pada formasi Saraweh berumur Miocene awal dan formasi Cijengkol berumur Oligocene akhir-Miocene awal yang dijadikan sebagai kandidat batuan reservoir dengan melakukan perhitungan nilai impedansi akustik dan porositasnya. Nilai impedansi akustik tersebut dicrossplotkan terhadap parameter litologi gamma ray sebagai indikator litologi. Nilai porositas batuan dihitung berdasarkan hubungan empirik antara nilai impedansi akustik dan neutron-porosity. Hasil penelitian ini menunjukkan bahwa batuan karbonat memiliki nilai impedansi akustik berkisar antara 10000 ((m/s)*(g/cm³)) - 13500 ((m/s)*(g/cm ³)) dan nilai porositas kurang dari 0.20 v/v sedangkan batupasir memiliki nilai impedansi akustik berkisar antara 3500 ((m/s)*(g/cm³)) - 8000 ((m/s)*(g/ cm³)) dan nilai porositas 0.30 v/v-0.38 v/v. Nilai porositas yang dimiliki batupasir cukup baik sehingga dapat dijadikan sebagai kandidat batuan reservoir. Berdasarkan penampang impedansi akustik dan porositas, distribusi reservoir batupasir pada umumnya berkembang dan menebal ke arah utara dan timur sehingga pada area tersebut dapat dilakukan kegiatan eksplorasi lebih lanjut.
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