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 />
<strong>Research</strong> Activities<br />
Institute for Frontier <strong>Research</strong> on Earth Evolution(IFREE)<br />
Activities during the 2002 fiscal year<br />
On January , , two new <strong>Research</strong> Programs were started, namely Mantle-Core Dynamics and<br />
Paleoenvironment, bringing the number of IFREE <strong>Research</strong> Programs up to the four that were initially planned. The<br />
IFREE opening ceremony was held at the Tokyo Forum on January , . However, only one research group<br />
was approved for each of the respective new <strong>Research</strong> Programs, and IFREE's research organization is yet to be<br />
completed. Applications for research staff and technical research staff were invited twice during the fiscal<br />
year, and staffs were hired. As a consequence, IFREE employed research and technical research staffs by the<br />
end of the fiscal year. Among them, six are temporary staff and eleven are foreign scientists.<br />
IFREE emphasized multi-disciplinary research projects during the fiscal year. Three research subjects were<br />
selected: 'water in the interior of the Earth', 'Izu-Bonin-Mariana arc', and 'Cretaceous events', and six workshops<br />
were held on these topics. IFREE also held 'Solid Earth simulation workshop', 'Cooperative workshop for earth science<br />
and fluid engineering', 'IFREE summer school', 'Tectonics-geodynamics short course/workshop', and 'NSF-<br />
IFREE workshop on Izu-Bonin-Mariana' in Hawaii. In addition, IFREE started cooperative research<br />
projects with domestic institutions, including Earthquake <strong>Research</strong> Institute, University of Tokyo, Institute for<br />
Geothermal Sciences, Kyoto University, Tokyo Institute of Technology, Kochi University, Shimane University,<br />
Okayama University of Science, National Institute for Earth Science and Disaster Prevention, and Meteorological<br />
<strong>Research</strong> Institute, as well as with foreign institutions such as University of California at Berkeley, University of<br />
Hawaii, University of Wisconsin, University of Southampton, and University of Edinburgh.<br />
IFREE's research progressed significantly during the fiscal year, and about papers were presented at<br />
domestic meetings and about papers at international meetings. Publications included English papers and <br />
Japanese papers. Among the English papers, were published in international refereed journals. Press releases<br />
were made on the 'Finding of a splay fault in the Nankai trough seismogenic zone', 'Hot fingers in the mantle wedge<br />
of a subduction zone', and four other research findings. These results, and many other research accomplishments,<br />
were published in the 'Frontier <strong>Research</strong> on Earth Evolution–IFREE Report for -'.<br />
<strong>Research</strong> Program for Mantle Core Dynamics<br />
1. <strong>Research</strong> Overview<br />
The structure of the Earth's mantle and core records<br />
a history of activity in the Earth. In the Mantle-Core<br />
Dynamics <strong>Research</strong> Program, we perform threedimensional<br />
imaging of the mantle and core to understand<br />
the present status and past record of the Earth's<br />
activity. The obtained images, along with simulated<br />
results of convection in the mantle and core, will<br />
enable us to reconstruct the Earth's activity in the present<br />
and in the past, and to understand the dynamics of<br />
Earth's evolution.<br />
We use data from the Ocean Hemisphere Project<br />
(OHP) Network and Deep Sea Geophysical<br />
Observatories, which have been developed and<br />
deployed by Japanese universities such as the<br />
Earthquake <strong>Research</strong> Institute of the University of<br />
Tokyo in cooperation with JAMSTEC, in order to<br />
obtain new generation models of the Earth's interior.<br />
We are expanding broadband seismology from landbased<br />
observation to observation on the sea floor, and<br />
have initiated "ocean bottom broadband seismology".<br />
We are also starting electromagnetic imaging using<br />
ocean bottom observations by taking advantage of the<br />
ocean bottom environment being free from artificial<br />
noises.<br />
The imaging the Earth's interior should enable us to<br />
detect thermal and chemical anomalies associated with<br />
the mantle and core convection and delineate the convection<br />
pattern. On the basis of the imaging results,<br />
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