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doi:10.2204/iodp.pr.312.2006

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.

Citation:

Expedition 309 and 312 Scientists, 2006. Superfast spreading rate crust 3: a complete in situ section of upper oceanic crust formed at a superfast spreading rate. IODP Prel. Rept., 312. doi:10:2204/iodp.pr.312.2006

Distribution:

Electronic copies of this series may be obtained from the Integrated Ocean Drilling Program (IODP) 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): Joint Oceanographic Institutions, Inc., 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:

    European Consortium for Ocean Research Drilling (ECORD)

    Ministry of Education, Culture, Sports, Science and Technology (MEXT) of Japan

    Ministry of Science and Technology (MOST), People's Republic of China

    U.S. National Science Foundation (NSF)

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., Joint Oceanographic Institutions, Inc., Lamont-Doherty Earth Observatory of Columbia University, Texas A&M University, or Texas A&M Research Foundation.

April 2006

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