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Tectonic geomorphology and Holocene uplift rates of the Lae Urban Area,...
The city of Lae is Papua New Guinea (PNG)’s second largest, and is the home of PNG’s largest port. Here, a convergence rate of ~50 mm/yr between the South Bismarck Plate and the... -
Tectonic geomorphology and Holocene uplift rates of the Lae Urban Area,...
The city of Lae is Papua New Guinea (PNG)’s second largest, and is the home of PNG’s largest port. Here, a convergence rate of ~50 mm/yr between the South Bismarck Plate and the... -
Tectonic geomorphology and Holocene uplift rates of the Lae Urban Area,...
The city of Lae is Papua New Guinea (PNG)’s second largest, and is the home of PNG’s largest port. Here, a convergence rate of ~50 mm/yr between the South Bismarck Plate and the... -
Tectonic geomorphology and Holocene uplift rates of the Lae Urban Area,...
The city of Lae is Papua New Guinea (PNG)’s second largest, and is the home of PNG’s largest port. Here, a convergence rate of ~50 mm/yr between the South Bismarck Plate and the... -
Tectonic geomorphology and Holocene uplift rates of the Lae Urban Area,...
The city of Lae is Papua New Guinea (PNG)’s second largest, and is the home of PNG’s largest port. Here, a convergence rate of ~50 mm/yr between the South Bismarck Plate and the... -
Seismotectonic model and probabilistic seismic hazard assessment for Papua New Guinea
Papua New Guinea (PNG) lies in a belt of intense tectonic activity that experiences high levels of seismicity. Although this seismicity poses significant risks to society, the... -
The Rabaul Earthquake Location and Caldera Structure (RELACS) Program :...
A component of the PNG-Australia Volcanological Services Support (VSS) Project funded by AusAID -
Investigation of hot gas emissions from Koranga volcano, Papua New Guinea, in 1967
Hot emissions of mainly sulphur dioxide and carbon dioxide took place from a mound in Koranga open cut, near Wau, following a landslide at the end of May, 1967. Rocks of the... -
Preliminary catalogue of tsunamis for the New Guinea/Solomon Islands region,...
Legacy product - no abstract available -
A low-cost seismic network for Papua New Guinea
Papua New Guinea (PNG) is situated at the edge of the Pacific “ring of fire” and is exposed to frequent large earthquakes and volcanic eruptions. Earthquakes in PNG, such as... -
Probabilistic seismic hazard map of Papua New Guinea
Probabilistic seismic hazard map of Papua New Guinea, in terms of Peak Ground Acceleration, is developed for return period of 475 years. The calculations were performed for... -
Tectonic geomorphology and Holocene uplift rates of the Lae Urban Area,...
The city of Lae is Papua New Guinea (PNG)’s second largest, and is the home of PNG’s largest port. Here, a convergence rate of ~50 mm/yr between the South Bismarck Plate and the... -
Probabilistic Seismic Hazard Assessment of Papua New Guinea: 2019 revision
Papua New Guinea (PNG) lies in a belt of intense tectonic activity that experiences high levels of seismicity. Although this seismicity poses significant risks to society, the... -
The 2006 Earthquake Swarm in the Sulu Range, Central New Britain, Papua New Guinea
On 6th July 2006, an intense swarm of earthquake activity began in the Sulu Range, Central New Britain, Papua New Guinea. The earthquakes were felt almost every one to two... -
Community-based Seismic Monitoring Network of Papua New Guinea
The Papua New Guinea (PNG) region has been formed within an oblique convergence zone between the north-northeasterly moving Australian plate and the Pacific plate. The region is... -
Seismic hazard mapping of Papua New Guinea — 2019 revision
In this study, we performed a probabilistic seismic hazard assessment (PSHA) for Papua New Guinea (Figure 1) to underpin a revision of the seismic zoning map for the national...
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