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Marine Ecosystems Research Department - jamstec japan agency ...

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Japan <strong>Marine</strong> Science and Technology Center<br />

Institute for Frontier <strong>Research</strong> on Earth Evolution (IFREE)<br />

3.1. Experiments in the region of the mantle downwelling<br />

We have conducted both seismic and electromagnetic<br />

experiments in the central Mariana trough and<br />

surrounding area, since (Fig.). Larger experiments<br />

under international collaboration are planned<br />

for the future. From June , a large and long-term<br />

ocean bottom seismic observation is being conducted<br />

for one year as a part of a multi scale study of the<br />

NSF-funded MARGINS project. The main aim is -D<br />

imaging of mantle structure in the island-arc and backarc<br />

basin by using seismic waves from active deep<br />

events. In addition, active monitoring of a serpentine<br />

sea mount in the fore-arc, surface wave analysis of<br />

teleseismic waves, and other studies are planned as<br />

part of this experiment. As a pilot study for this, a<br />

long-term seismic observation using ocean bottom<br />

seismometers was performed (Fig. ) from October<br />

Deep Events (1990-2000, PDE)<br />

and<br />

Mariana LT-OBS Array (2001/10-2002/10)<br />

to February . An example of the records for<br />

a large event is shown in Figure , and analysis of this<br />

data set will be made in FY. The precise activities<br />

of deep events in the subducted slab, which cannot<br />

be obtained from land data alone, will be investigated.<br />

For electromagnetic studies, we deployed ocean<br />

bottom electromagnetometers (OBEMs) in along<br />

a line crossing the Mariana trough (Fig. ). This<br />

experiment was in collaboration with the Deep Sea<br />

<strong>Research</strong> <strong>Department</strong> of JAMSTEC, the Earthquake<br />

<strong>Research</strong> Institute, Kobe University, and the National<br />

Institute of Polar <strong>Research</strong>. Two of the OBEMs,<br />

which were located on the island arc and eastern<br />

Mariana trough, were recovered in April .<br />

The other three OBEMs, which were located in the<br />

Parece-Vela basin, in the western Mariana trough,<br />

and in the Pacific, were recovered in November .<br />

Preliminary analysis of the acquired data suggests an<br />

interesting feature: that the electric conductivity is<br />

Ev: 2001/10/31 09:10:20.00 -5.91 150.20 33.0 7.00<br />

22˚N<br />

mr9 BZ<br />

20˚N<br />

mr8 BZ<br />

18˚N<br />

mr7 BZ<br />

16˚N<br />

mr6 BZ<br />

mr5 BZ<br />

14˚N<br />

mr4 BZ<br />

12˚N<br />

mr2 BZ<br />

140˚E 142˚E 144˚E 146˚E 148˚E 150˚E<br />

100 200 300 400 500 600<br />

Focal depth (km)<br />

Fig. 5 Site locations of the seismic (large circles) and electromagnetic<br />

(crosses) observations and hypocenter distribution<br />

(colored filled circles) are superimposed.<br />

Fig. 6 Vertical component records of seismic waves obtained by<br />

OBSs. Blue lines are theoretical travel times based on the<br />

iasp91 model.<br />

91

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