Titlebook: Basin Formation, Ridge Crest Processes, and Metallogenesis in the North Fiji Basin; Loren W. Kroenke,James V. Eade (Co-Chief Scientist Boo

形上升才刺激

Morphology and Structure of the Seafloor in the Northern Part of the North Fiji Basin,l 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 inter

exclamation

Shallow Seismicity in the North Fiji Basin,vidence for (1) transcurrent faulting along the Fiji Fracture Zone; (2) hinge faulting of the Indo-Australian Plate near the Hunter Fracture Zone; (3) strike-slip faulting near the Hazel Holme Ridge; (4) strike-slip faulting within the central North Fiji Basin; and (5) normal faulting in the western

喚起

Deep Seismicity in the North Fiji Basin,use severe deformation of Pacific lithosphere subducted at the Tonga Trench. The slab segments have settled above the 700-km level and may represent a physical boundary which would preclude whole-mantle convection, at least in this area.

hereditary

留戀

Meditative

表臉

Petrology and Geochemistry of Submarine Lavas from the Lau and North Fiji Back-Arc Basins,atible-element enriched “transitional” basalts (Type III). The extremely fresh appearance of these lavas suggests that they are very young. We propose that the South Pandora Ridge represents a recently activated, pre-existing lineament that includes Rotuma Island. New isotope data from the North Fij

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