Proceedings of the 12th International INQUA meeting on paleoseismology, active tectonic and archaeoseismology

sett ing. Ear th-Science Reviews, 156, 66-81 . https: //www. sciencedirect.com/science/ ar t icle/pi i /S00128 25216300502 Koulali, A., Tregoning, P., McClusky, S., Stanaway, R., Wallace, L., & Lister, G. (2015). New Insights into the present-day kinematics of the central and western Papua New Guinea from GPS. Geophysical Journal International, 202(2), 993- 1004. https: //doi.org/10.1093/gji/ ggv200 Liu, K. (1993). Sedimentation and tectonics of the Markham Suture, Papua New Guinea. (PhD), Australian National University, Canberra. Stanaway, R., Wallace, L., Sombo, Z., Peter, J., Palusi, T., Safomea, B., & Nathan, J. (2009). Lae, a City caught between two plates - 15 years of Deformation Measurements with GPS. Paper presented at the 43rd Association of Surveyors PNG Congress, Lae, 12th - 15th August 2009, Focus On Challenges; Society-Space-Surveyors, Lae, PNG. http://www.quickclose.com. au/LaeDeformation.pdf Fig. 4: Composite SW-NE cross section across the Atzera Range anticline, showing the various uplifted fluvial and marine surfaces. The primary profile line is shown as X-X’ in Fig. 2. Additional sub-parallel profiles were collected across the marine terraces, the War Memorial/Botanical Gardens terraces, and the coastline. Grey lines are Z, Zmax, and Zmin from 100 m wide swath profiles collected using SAGA GIS swath profiling tool through 1 m resolution LiDAR data. Inset shows conceptual model of fold development in the hanging- wall of the fault. Relative terrace riser heights are shown with subscript ‘r’. Guinea. Retrieved from Crook, K. A. W. (1989a). Quaternary uplift rates at a plate boundary, Lae urban area, Papua New Guinea. Tectonophysics, 163(1), 105-118. https: //www.sciencedirect. com/science/article/pii/004019 5189901212 Crook, K. A. W. (1989b). Suturing history of an allochthonous terrane at a modern plate boundary traced by f lysch- to- molasse facies transitions. Sedimentary Geology, 61(1), 49- 79. https: //www.sciencedirect. com/science/article/pii/003707 3889900419 Ghasemi , H. , Cummins, P. , Weatheri l l , G. , McKee, C. , Hazelwood, M. , & Al len, T. (2020). Seismotectonic model and probabi l ist ic seismic hazard assessment for Papua New Guinea. Bul let in of Ear thquake Engineering, 18, 6571- 6605. Holm, R. J. , Rosenbaum, G. , & Richards, S. W. (2016). Post 8Ma reconstruct ion of Papua New Guinea and Solomon Islands: Microplate tectonics in a convergent plate boundary R E F E R E N C E S Abbot t , L . D. , Si lver, E. A. , & Galewsky, J. (1994). Structural evolution of a modern arc- continent collision in Papua New Guinea.13(5), 1007-1034. https: // agupubs.onlinelibrary.wiley.com/ doi/abs/10.1029/ 94TC01623 Abbott, L. D., Silver, E. A., Thompson, P. R., Filewicz, M. V., Schneider, C., & Abdoerrias. (1994). Stratigraphic constraints on the development and timing of arc- continent collision in northern Papua New Guinea. Journal of Sedimentary Research, 64(2b), 169-183. https: //doi. org/10.1306/D4267F82-2B26-11D7- 8648000102C1865D Abers, G. A., & McCaffrey, R. (1994). Active arc-continent collision: Earthquakes, gravity anomalies, and fault kinematics in the Huon- Finisterre collision zone, Papua New Guinea. 13(2), 227-245. https:// agupubs.onlinelibrary.wiley.com/ doi/abs/10.1029/ 93TC02940 Buleka, J., Prior, D., & Spek, A. V. D. (1999). COASTPLAN - geology and natural hazards of Lae city and surroundings, Papua New