Abstract
A geophysical survey of the north central North Fiji Basin provides a high density data base for accurately charting seafloor morphology and defining major structural trends. The resulting bathymetric chart is believed to reliably portray the tectonic fabric of the basin and provide insight into the formation of the seafloor and development of associated structural features. The South Pandora Ridge (Hazel Holme Fracture Zone) appears to be a young or recently formed spreading ridge that bifurcates at its eastern end into the ENE-trending Rotuma Ridge and ESE-trending Tripartite Ridge. Southwest of South Pandora Ridge lies Pentecost Basin, interpreted to be originally formed along the western limb of the extinct central North Fiji Basin (CNFB) triple junction and now inundated, at its southwestern end, by sediment of the New Hebrides archipelagic apron. Southeast of the ridge lies Balmoral Basin, interpreted to be originally formed along the eastern limb of the old CNFB triple junction. Between the two basins lies a wedge of sediment-free ridge and trough terrain believed to be formed by a propagating rift. To the east, in the southern part of Balmoral Basin, Balmoral Ridge is interpreted to be the upraised leading edge of an overthrust block of North Fiji Basin crust, to the south of which lies the eastern end of the Fiji Fracture Zone, a presently active transform fault.
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Kroenke, L.W., Smith, R., Nemoto, K. (1994). Morphology and Structure of the Seafloor in the Northern Part of the North Fiji Basin. In: Kroenke, L.W., Eade, J.V. (eds) Basin Formation, Ridge Crest Processes, and Metallogenesis in the North Fiji Basin. Circum-Pacific Council for Energy and Mineral Resources Earth Science Series, vol 15. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-85043-1_2
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DOI: https://doi.org/10.1007/978-3-642-85043-1_2
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