Volcanology Commons^™

Expedition 350 Methods, Y. Tamura, C. J. Busby, P. Blum, G. Guèrin, G. D.M. Andrews, A. K. Barker, J. L. R. Berger, E. M. Bongiolo, M. Bordiga, Susan M. Debari, J. B. Gill, C. Hamelin, J. Jia, E. H. John, A. -S. Jonas, M. Jutzeler, M. A.C. Kars, Z. A. Kita, K. Konrad, S. H. Mahoney, M. Martini, T. Miyazaki, R. J. Musgrave, D. B. Nascimento, A. R.L. Nichols, J. M. Ribeiro, T. Sato, J. C. Schindlbeck, A. K. Schmitt, S. M. Straub, M. J. Vautravers, Y. Yang

Geology Faculty Publications

This chapter of the International Ocean Discovery Program (IODP) Expedition 350 Proceedings volume documents the procedures and tools employed in the various shipboard laboratories of the R/V JOIDES Resolution during Expedition 350. This information applies only to shipboard work described in the Expedition Reports section of this volume. Methods for shore-based analyses of Expedition 350 samples and data will be described in the individual scientific contributions to be published in the open literature or in the Expedition Research Results section of this volume.

This section describes procedures and equipment used for drilling, coring, and hole completion; core handling; computation of …

Expedition 350 Summary, Y. Tamura, C. J. Busby, P. Blum, G. Guèrin, G. D.M. Andrews, A. K. Barker, J. L.R. Berger, E. M. Bongiolo, M. Bordiga, Susan M. Debari, J. B. Gill, C. Hamelin, J. Jia, E. H. John, A.-S. Jonas, J. Jutzeler, M A.C. Kars, Z. A. Kita, K. Konrad, S. H. Mahony, M. Martini, T. Myiazaki, R. J. Musgrave, D. B. Nascimento, A. R.L. Nichols, J. M. Ribeiro, T. Sato, J. C. Schindlbeck, A. K. Schmitt, S. M. Straub, M. J. Vautravers, Y. Yang

Geology Faculty Publications

International Ocean Discovery Program (IODP) Hole U1436A (proposed Site IBM-4GT) lies in the western part of the Izu fore-arc basin, ~60 km east of the arc-front volcano Aogashima, ~170 km west of the axis of the Izu-Bonin Trench, and 1.5 km west of Ocean Drilling Program (ODP) Site 792, at 1776 meters below sea level (mbsl). It was drilled as a 150 m deep geotechnical test hole for potential future deep drilling (5500 meters below seafloor [mbsf]) at proposed Site IBM-4 using the D/V Chikyu. Core from Site U1436 yielded a rich record of Late Pleistocene explosive volcanism, including …

Izu-Bonin-Mariana Rear Arc: The Missing Half Of The Subduction Factory, Yoshihiko Tamura, Abigail K. Barker, Cathy J. Busby, Julien L.R. Berger, Peter Blum, Everton M. Bongiolo, Gilles Guèrin, Manuela Bordiga, Graham D.M. Andrews, Susan M. Debari, James B. Gill, Cedric Hamelin, Jihui Jia, Eleanor H. John, Ann-Sophie Jonas, Martin Jutzeler, Myriam A.C. Kars, Zachary A. Kita, Kevin Konrad, Susan H. Mahony, Michelangelo Martini, Takashi Miyazaki, Robert J. Musgrave, Debora B. Nascimento, Alexander R.L. Nichols, Julia M. Ribeiro, Tomoki Sato, Julie C. Schindlbeck, Axel K. Schmitt, Susanne M. Straub, Maryline J. Vautravers, Yang Yang

Geology Faculty Publications

4GT) lies in the western part of the Izu fore-arc basin, ~60 km east of the arc-front volcano Aogashima, ~170 km west of the axis of the Izu-Bonin Trench, 1.5 km west of Ocean Drilling Program (ODP) Site 792, and at 1776 meters below sea level (mbsl). It was drilled as a 150 m deep geotechnical test hole for potential future deep drilling (5500 meters below seafloor [mbsf]) at proposed Site IBM-4 using the D/V Chikyu. Core from Site U1436 yielded a rich record of Late Pleistocene explosive volcanism, including distinctive black glassy mafic ash layers that may record large-volume …