Approximate surface projection on Pacific Ocean of Havre Trough
The Havre Trough (Havre Basin[1]) is a currently actively rifting back-arc basin[1] about 100 km (62 mi) to 120 km (75 mi) wide,[2] between the Australian Plate and Kermadec microplate. The trough extends northward from New Zealand's offshore Taupō Volcanic Zone commencing at Zealandia's continental shelf margin and continuing as a tectonic feature, as the Lau Basin which currently contains active seafloor spreading centers. Its eastern margin is defined by the Kermadec Ridge created by Pacific Plate subduction under the Kermadec microplate, while the western margin is the remnant Lau-Colville Ridge.
- ^ a b Artemieva 2023, Section:#18. Harve Basin
- ^ Caratori et al. 2019, Section:Evidence of past seafloor spreading in the Havre Trough