Scheduled Cruises in 2002
Summary of a recent cruise on margins research (JP.021)
Mariana Arc
Kairei
28 October 2002 from Guam
12 November 2002 in Yokosuka
N. Seama
Kobe University, Japan
T. Goto, M. Ichiki,
seama@kobe-u.ac.jp
(1) We have conducted a preliminary seafloor MT
experiment using OBEM (Ocean Bottom Electro-Magnetometer) as a first
step towards imaging the deep conductivity structure across the central
Mariana subduction system from the subducting Pacific plate, fore-arc,
island arc, the Mariana Trough backarc basin, to the Parece-Vela Basin.
We deployed 10 OBEMs using the R/V Yokosuka cruise in October 2001,
recovered two of them during an R/V Ewing cruise in April, and will
recover the rest of them during this R/V Kairei cruise. This study has
two purposes; i) to understand the melt structure feeding the slow
spreading axis of the Mariana Trough and ii) to image the overall
mantle conductivity structure across the Mariana subduction system.
(2) We will test the MOSES (Magnetometric Off-Shore
Electrical Sounding) system at a hydrothermal site in the Suiyo
Seamount, the Izu-Bonin Island Arc, Western Pacific. The system has
been newly developed to derive the electrical conductivity structure of
a shallow part of the oceanic crust. The results from the hydrothermal
site would allow us to understand overall features of the hydrothermal
system.
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