Understanding sedimentary systems and processes of the Hikurangi subduction margin; from Trench to Back-Arc. Volume 2

Author:

Strachan Lorna J.1ORCID,Orpin Alan R.2,Bland Kyle J.3ORCID,McArthur Adam D.4,Bailleul Julien5

Affiliation:

1. School of Environment, University of Auckland, Auckland, New Zealand

2. National Institute of Water and Atmosphere Research (NIWA), Wellington, New Zealand

3. GNS Science, Lower Hutt, New Zealand

4. School of Earth and Environment, University of Leeds, Leeds, UK

5. Basins-Reservoirs-Resources (B2R), Geosciences Department, UniLaSalle - University of Picardie Jules Verne, Beauvais, France

Publisher

Informa UK Limited

Reference111 articles.

1. Reconstructing the quaternary evolution of the world’s most active silicic volcanic system: insights from an 1.65 Ma deep ocean tephra record sourced from Taupo Volcanic Zone;Allan ASR;New Zealand. Quaternary Science Reviews,2008

2. Onshore–offshore correlation of Pleistocene rhyolitic eruptions from New Zealand: implications for TVZ eruptive history and paleoenvironmental construction

3. Newly recognized turbidity current structure can explain prolonged flushing of submarine canyons

4. Preconditioning by sediment accumulation can produce powerful turbidity currents without major external triggers

5. Bailleul J, Chanier F, Ferrière J, Robin C, Nicol A, Mahieux G, Gorini C, Caron V. 2013. Neogene evolution of lower trench-slope basins and wedge dynamics in the central Hikurangi subduction margin, New Zealand. In Gaullier V, Basile C, Roure F, Scheck-Wenderoth M, editors. Basin dynamics; tectonophysics Special Issue; 591, p. 152–174.

Cited by 1 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. Correction;New Zealand Journal of Geology and Geophysics;2024-07-02

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