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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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