Ophioliticlastic Ihungia igneous conglomerate (Early Miocene), North Island, New Zealand: evidence for an island source related to subduction initiation and deposition within a slump-generated submarine slope re-entrant-Reference-Cited by-同舟云学术

Ophioliticlastic Ihungia igneous conglomerate (Early Miocene), North Island, New Zealand: evidence for an island source related to subduction initiation and deposition within a slump-generated submarine slope re-entrant

Published:2014-04-03 Issue:2 Volume:57 Page:219-235
ISSN:0028-8306
Container-title:New Zealand Journal of Geology and Geophysics
language:en
Short-container-title:New Zealand Journal of Geology and Geophysics

Author:

Marsaglia KM¹,Mortimer N²,Bender-Whitaker C¹,Marden M³,Mazengarb C⁴

Affiliation:

1. Department of Geological Sciences, California State University, Northridge, CA, USA

2. GNS Science, Dunedin, New Zealand

3. Landcare Research, Gisborne, New Zealand

4. Department of Energy, Infrastructure and Resources, Mineral Resources Tasmania, Rosny Park, Tasmania, Australia

Publisher

Informa UK Limited

Subject

Earth and Planetary Sciences (miscellaneous),Geology,Geophysics

Link

https://www.tandfonline.com/doi/pdf/10.1080/00288306.2014.898665

Reference83 articles.

1. Stratigraphy of the southern Norfolk Ridge and the Reinga Basin: A record of initiation of Tonga–Kermadec–Northland subduction in the southwest Pacific

2. Evolution of the Upper Cenozoic Magmatic Arc and plate boundary in northern New Zealand

3. Northland Allochthon

4. Geometry of the Hikurangi subduction thrust and upper plate, North Island, New Zealand

5. Upper Cretaceous and Tertiary geology of Mangatu State Forest, Raukumara Peninsula, New Zealand

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