Turbidite Systems in the Inner Forearc Domain of the Hikurangi Convergent Margin (New Zealand): New Constraints on the Development of Trench-Slope Basins
Author:
Publisher
Society for Sedimentary Geology
Subject
Geology
Cited by 41 articles. 订阅此论文施引文献 订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献
1. Understanding sedimentary systems and processes of the Hikurangi subduction margin; from Trench to Back-Arc. Volume 2;New Zealand Journal of Geology and Geophysics;2024-07-02
2. Early stages of trench-slope basin development: Insights from mass-transport deposits and their interactions with turbidite systems (southern Hikurangi margin, New Zealand);Marine and Petroleum Geology;2023-06
3. Composition of fine‐grained sediment in the Hikurangi Trough: Evidence for intermingling among axial gravity flows, transverse gravity flows and margin‐parallel ocean currents;Sedimentology;2023-01-11
4. Whole-rock chemistry and Sr isotope concentrations in the Upper Cretaceous shale, western Iran: evidence for a transition from trench to fore-arc setting;Arabian Journal of Geosciences;2022-09
5. Litho- and biostratigraphy of a late Oligocene–Early Miocene succession in the Weber area, southern Hawke’s Bay, and implications for early Hikurangi subduction-margin evolution;New Zealand Journal of Geology and Geophysics;2022-08-10
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