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Late Cretaceous to Oligocene burial and collision in western Papua New Guinea: Indications from low-temperature thermochronology and thermal modelling

Luke Mahoney 1, * Sandra Mclaren 1 Kevin Hill 1 Barry Kohn 1 Kerry Gallagher 2 Martin Norvick 1 
* Corresponding author
2 Terre, Temps, Traçage
GR - Géosciences Rennes
Abstract : Recent field and analytical work have considerably improved our understanding of the structure of the MullerRange along the frontal trend of the Papuan Fold and Thrust Belt (PFTB) in western Papua New Guinea (PNG).However numerous questions remain unresolved concerning the geological evolution of the region. In particular,the Late Cretaceous to Oligocene history of the region is largely unknown due to the absence of a continuousstratigraphic record. Here, we use both new and existing low-temperature thermochronology data to investigatethe geological history of the Muller Range. Thermal history models based on these data suggest two majorCenozoic cooling episodes. The youngest, and best constrained, is clearly recorded in the stratigraphic recordand relates to Neogene collision at the northern margin of the Australian continent. An older episode of comparableor greater magnitude occurred in the Eocene to Oligocene and may relate to the removal of1500–3000m of Late Cretaceous to Eocene section across the Muller Range prior to the widespread deposition ofthe shelfal Darai Limestone. We suggest that extension along major faults beneath the Muller Range accommodatedsedimentation from the Late Cretaceous to the Eocene, consistent with long-lived extensional structuresobserved in neighbouring regions. In contrast to the Muller Range area, an almost continuous Late Cretaceous toEocene stratigraphic sequence is preserved in the hinterland<50 km to the northeast. The selective removal ofthis sequence across the Muller Range suggests it was uplifted in the Eocene to Oligocene, possibly in partfacilitated by the inversion of extensional faults in the Muller Range area. We suggest that this inversion wasrelated to the Eocene to Oligocene collision of the expansive Sepik Terrane to the northwest of the PNG margin.The new data and interpretations presented here have significant implications for the evolution of the PFTB andfor tectonic reconstructions of PNG.
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Submitted on : Thursday, January 17, 2019 - 1:17:56 PM
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Luke Mahoney, Sandra Mclaren, Kevin Hill, Barry Kohn, Kerry Gallagher, et al.. Late Cretaceous to Oligocene burial and collision in western Papua New Guinea: Indications from low-temperature thermochronology and thermal modelling. Tectonophysics, Elsevier, 2019, 752, pp.81-112. ⟨10.1016/j.tecto.2018.12.017⟩. ⟨insu-01984860⟩



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