Depositional rate, grain size and magnetic mineral sulfidization in turbidite sequences, Hikurangi Margin, New Zealand-Reference-Cited by-同舟云学术

Depositional rate, grain size and magnetic mineral sulfidization in turbidite sequences, Hikurangi Margin, New Zealand

Author:

Noda Atsushi¹^ORCID,Greve Annika²^ORCID,Woodhouse Adam³⁴^ORCID,Crundwell Martin⁵^ORCID

Affiliation:

1. Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology, Tsukuba, Japan

2. Department of Earth Sciences, Utrecht University, Utrecht, The Netherlands

3. School of Earth and Environment, The University of Leeds, Leeds, UK

4. Institute for Geophysics, University of Texas, Austin, TX, USA

5. Surface Geosciences Department, GNS Science, Lower Hutt, New Zealand

Funder

Korea Institute of Energy Technology Evaluation and Planning

nederlandse organisatie voor wetenschappelijk onderzoek

Publisher

Informa UK Limited

Subject

Earth and Planetary Sciences (miscellaneous),Geology,Geophysics

Link

Reference110 articles.

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