Academic literature on the topic 'Northwest Java'

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Journal articles on the topic "Northwest Java"

1

Denney, Dennis. "Hybrid Gas-Lift Application Offshore Northwest Java." Journal of Petroleum Technology 52, no. 05 (2000): 30. http://dx.doi.org/10.2118/0500-0030-jpt.

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2

Sutayasa, Md. "Notes on the Bum Pottery Complex, Northwest Java." Mankind 8, no. 3 (2009): 182–84. http://dx.doi.org/10.1111/j.1835-9310.1972.tb00433.x.

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3

Septama, Erlangga, C. Prasetyadi, A. Abdurrokhim, et al. "The hidden sedimentary basin underneath the Quaternary volcanic unit in Bogor and Kendeng area." Berita Sedimentologi 47, no. 2 (2021): 25–47. http://dx.doi.org/10.51835/bsed.2021.47.2.323.

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The Java Island is an active volcanic arc that experiences several volcanism episodes, which gradually changes from South to North from the Late Oligocene to Pleistocene, following the subduction of the Australian plates underneath the Eurasian plates. During the Eocene, the southern and northern part of Java was connected as one passive margin system with the sediment supply mainly comes from Sundaland in the north. The compressional tectonics creates a flexural margin and a deep depression in the central axis of Java Island and acts as an ultimate deep-sea depocenter in the Neogene period. I
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4

Widianto, E. "Petroleum system of Northwest Java basin based on gravity data analysis." IOP Conference Series: Earth and Environmental Science 106 (January 2018): 012106. http://dx.doi.org/10.1088/1755-1315/106/1/012106.

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5

Namara, Aliep Fishabil, I. Wayan Nurjaya, and Mochamad Tri Hartanto. "Modelling of ocean currents and distribution of total suspended solids in Citarum River estuary." BIO Web of Conferences 106 (2024): 03004. http://dx.doi.org/10.1051/bioconf/202410603004.

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The Citarum River is an important river in West Java, which empties into the Java Sea carrying large suspended sediment concentrations. The purpose of this study is to examine the interaction of current patterns and distribution of total suspended solids (TSS) in the Northwest and Southeast Monsoons using hydrodynamic Modelling. The flow model and TSS used were 2-dimensional models with the OpenFlows FLOOD software. The ocean tide model results were validated using the Root Mean Square Error (RMSE) method with a value of 0.10. The current velocity in the West and East monsoons ranges from 0.07
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6

Adriansyah and George A. McMechan. "AVA analysis and interpretation of a carbonate reservoir: northwest Java basin, Indonesia." GEOPHYSICS 66, no. 3 (2001): 744–54. http://dx.doi.org/10.1190/1.1444964.

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A detailed analysis is performed of amplitude variation with angle (AVA) observations in six common‐midpoint gathers with reflection points that are over and beside carbonate reefs in the Parigi Formation in the northwest Java basin. Both empirical analysis and full‐wavefield modeling of the AVA data suggest that the presence of gas affects AVA by reducing the bulk density of the reservoir, decreasing of the overburden [Formula: see text] ratio and by local attenuation caused by gas sieving through the overlying sediments. The slopes of AVA curves for reflections from the top of the Parigi are
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7

Hidayati, Sri, Y. Suparman, and A. Loeqman. "Focal Mechanism and Parameter of Volcano-Tectonic Earthquake Source, in Mount Guntur, West Java." Indonesian Journal on Geoscience 6, no. 1 (2011): 1–11. http://dx.doi.org/10.17014/ijog.6.1.1-11.

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DOI: 10.17014/ijog.v6i1.111Guntur Volcano in West Java is one of the most active volcanoes in Indonesia. The last eruption took place in 1847 and the volcanic activity has been dormant since then, however its seismicity is active. During the period of July to October 2009, the hypocenter distribution of VT earthquakes is mostly located at western flank of the volcano, beneath Guntur - Gandapura craters at the depth of less than 5 km. The depth pattern shows deeper to the northwest. The VT earthquakes deeper than 5 km were not found in this period. The focal mechanism of VT earthquakes are obli
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8

Napitupulu, Haposan, Leroy Ellis, and Richard M. Mitterer. "Post-generative alteration effects on petroleum in the onshore Northwest Java Basin, Indonesia." Organic Geochemistry 31, no. 4 (2000): 295–315. http://dx.doi.org/10.1016/s0146-6380(99)00154-0.

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9

Adriansyah, A., and George A. McMechan. "Analysis and interpretation of seismic data from thin reservoirs: Northwest Java Basin, Indonesia." GEOPHYSICS 67, no. 1 (2002): 14–26. http://dx.doi.org/10.1190/1.1451317.

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A detailed analysis and interpretation is performed of a 2‐D seismic line over a sequence of thin reservoirs in the upper Cibulakan formation in the Northwest Java Basin. Most well sites in this area are selected to be structures near fault zones as faults are assumed to be the main hydrocarbon migration paths. Amplitude variation with offset analysis is little used because of contamination by thin‐layer tuning effects. Attribute analysis, impedance inversion, and full‐wavefield modeling suggest that gas reservoirs are detectable even when they are less than their tuning thickness, as they cor
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10

Tri Muji Susantoro, Sugihardjo, Ketut Wikantika, et al. "CCUS-EOR Optimization to Achieve Zero Emission Program Targets in Northwest Java Basin." Evergreen 10, no. 3 (2023): 1809–18. http://dx.doi.org/10.5109/7151730.

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