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Mubi Fault

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Journal Article
Published: 24 November 2020
Bulletin of the Seismological Society of America (2021) 111 (2): 1032–1042.
... Aperture Radar (SAR) images to calculate the 3D coseismic displacement of the 2018 Papua New Guinea earthquake. The results show clear fault traces that suggest coseismic slip on the Mubi fault and the Mananda fault that triggered landslides that spread out in a more than 260 km 2 region. Finite‐source...
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Coseismic displacement across transect (a) a–a′ (<b>Mubi</b> <b>fault</b>), (b) b–b′ (wes...
Published: 24 November 2020
Figure 7. Coseismic displacement across transect (a) a–a′ (Mubi fault), (b) b–b′ (west of Mananda fault), and (c) c–c′ (east of Mananda fault). For each transect, black dots represent the subpixel offset measurements that are less than 6 km away from the transect. Red and blue curves show
Series: AAPG Memoir
Published: 01 January 2018
DOI: 10.1306/13602029M1143704
EISBN: 9781629812786
... are well reproduced, and the modeled section appears quantitatively predictive. The modeling demonstrates three major pathways for water: (1) topographically driven flow from the onset of mountain building; (2) deep updip basinal flux, flowing along the tilted reservoirs; and (3) across fault escape from...
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(a) 3D view, (b) top views, (e) and cross‐section view of the <b>fault</b> model. ...
Published: 24 November 2020
Figure 5. (a) 3D view, (b) top views, (e) and cross‐section view of the fault model. Yellow‐to‐red colors indicate a greater amount of slip on the fault. Panels (c,d) highlight shallow slip of the Mananda and Mubi faults. The peak slip of the Mananda fault is less than ∼ 2    km in depth
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Reduced     χ  2     analysis for the dip, rake, and smoothing parameters f...
Published: 24 November 2020
Figure 4. Reduced χ 2 analysis for the dip, rake, and smoothing parameters for the Mubi fault and the Mananda fault. (a) Dip analysis of the Mananda fault; (b) dip analysis of the Mubi fault; (c) smoothing parameter analysis; (d) rake analysis of the Mananda fault; and (e) analysis
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Comparison of observed and modeled surface displacement. The residual is th...
Published: 24 November 2020
Figure 6. Comparison of observed and modeled surface displacement. The residual is the difference between the observed and modeled displacement. (a–c) horizontal displacement and (d–f) vertical displacement. Red rectangles outline the Mubi fault and the Mananda fault, and the yellow rectangle
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2010
DOI: 10.1144/SP348.3
EISBN: 9781862395961
... Abstract Cross sections, seismic data and centrifuge analogue modelling reveal the structural styles in the oil-producing areas of the Papuan Fold Belt. They include inverted basement faults, detachment faults in the Jurassic section 1–2 km beneath the Neocomian Toro Sandstone reservoir...
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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1991
AAPG Bulletin (1991) 75 (5): 857–872.
... by limestones and quartzites. The Papuan margin was dissected by Mesozoic extensional faults, in part reactivated during Neogene compression, which created basement-involved anticlines or elevated plateaus in the Papuan fold belt. The sedimentary section in the fold belt is deformed into large ramp anticlines...
FIGURES | View All (21)
Series: Geological Society, London, Special Publications
Published: 14 April 2020
DOI: 10.1144/SP490-2018-124
EISBN: 9781786205155
..., there are two water gaps, one cutting across the Kube Kabe Range (1) and the other cutting across the Kara Anticline (2), see Figure 7 . Another morphotectonic feature is the drainage diversion (DD), which marks sudden changes of a river course owing to blocking, slope changes or faulting. The Mubi River...
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