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doi:10.2204/iodp.pr.335.2011

Publisher’s notes

Material in this publication may be copied without restraint for library, abstract service, educational, or personal research purposes; however, this source should be appropriately acknowledged. Core samples and the wider set of data from the science program covered in this report are under moratorium and accessible only to Science Party members until 3 June 2012.

Citation:

Expedition 335 Scientists, 2011. Superfast spreading rate crust 4: drilling gabbro in intact ocean crust formed at a superfast spreading rate. IODP Prel. Rept., 335. doi:10.2204/iodp.pr.335.2011

Distribution:
Electronic copies of this series may be obtained from the Integrated Ocean Drilling Program (IODP) Scientific Publications homepage on the World Wide Web at www.iodp.org/scientific-publications/.

This publication was prepared by the Integrated Ocean Drilling Program U.S. Implementing Organization (IODP-USIO): Consortium for Ocean Leadership, Lamont Doherty Earth Observatory of Columbia University, and Texas A&M University, as an account of work performed under the international Integrated Ocean Drilling Program, which is managed by IODP Management International (IODP-MI), Inc. Funding for the program is provided by the following agencies:

• National Science Foundation (NSF), United States
• Ministry of Education, Culture, Sports, Science and Technology (MEXT), Japan
• European Consortium for Ocean Research Drilling (ECORD)
• Ministry of Science and Technology (MOST), People's Republic of China
• Korea Institute of Geoscience and Mineral Resources (KIGAM)
• Australian Research Council (ARC) and GNS Science (New Zealand), Australian/New Zealand Consortium
• Ministry of Earth Sciences (MoES), India

Disclaimer

Any opinions, findings, and conclusions or recommendations expressed in this publication are those of the author(s) and do not necessarily reflect the views of the participating agencies, IODP Management International, Inc., Consortium for Ocean Leadership, Lamont-Doherty Earth Observatory of Columbia University, Texas A&M University, or Texas A&M Research Foundation.

July 2011

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