Your new experience awaits. Try the new design now and help us make it even better

CORRECTION article

Front. Earth Sci., 29 August 2025

Sec. Georeservoirs

Volume 13 - 2025 | https://doi.org/10.3389/feart.2025.1671888

This article is part of the Research TopicGas Hydrates and their Implications for Global Changes: Climate, Environment, and EnergyView all 4 articles

Correction: Evidence for gas hydrate-filled fractures forming at the sulfate-methane transition zone, Hikurangi subduction margin, New Zealand

This article is a correction to:

  1. Evidence for gas hydrate-filled fractures forming at the sulfate-methane transition zone, Hikurangi subduction margin, New Zealand

    1. Read original article
Morgane Brunet, Morgane Brunet1,2*Ann CookAnn Cook3Saffron MartinSaffron Martin3Joshu MountjoyJoshu Mountjoy4
  • 1Institut des Sciences de la mer (ISMER), Université du Québec à Rimouski, Rimouski, QC, Canada
  • 2Geo-Ocean, Univ Brest, CNRS, Ifremer, UMR6538, Plouzane, France
  • 3School of Earth Science, The Ohio State University, Columbus, OH, United States
  • 4National Institute of Water and Atmospheric Research, Wellington, New Zealand

A Correction on
Evidence for gas hydrate-filled fractures forming at the sulfate-methane transition zone, Hikurangi subduction margin, New Zealand

by Brunet M, Cook A, Martin S and Mountjoy J (2025). Front. Earth Sci. 13:1630118. doi: 10.3389/feart.2025.1630118

Affiliation “Geo-Ocean, Univ Brest, CNRS, Ifremer, UMR6538, Plouzane, France” was omitted from the paper. This affiliation has now been added for author Morgane Brunet.

The original article has been updated.

Publisher’s note

All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.

Keywords: gas hydrate, sulfate-methane transition zone, fracture network, X-ray computed tomography, Hikurangi subduction margin, New Zealand, IODP expedition 372

Citation: Brunet M, Cook A, Martin S and Mountjoy J (2025) Correction: Evidence for gas hydrate-filled fractures forming at the sulfate-methane transition zone, Hikurangi subduction margin, New Zealand. Front. Earth Sci. 13:1671888. doi: 10.3389/feart.2025.1671888

Received: 23 July 2025; Accepted: 01 August 2025;
Published: 29 August 2025.

Approved by:

Frontiers Editorial Office, Frontiers Media SA, Switzerland

Copyright © 2025 Brunet, Cook, Martin and Mountjoy. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

*Correspondence: Morgane Brunet, bW9yZ2FuZS5icnVuZXRAdXFhci5jYQ==

Disclaimer: All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.