Marine Ecosystems Research Department - jamstec japan agency ...
Marine Ecosystems Research Department - jamstec japan agency ...
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 />
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