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<strong>InterRidge</strong> Cruise Bursaries<br />

<strong>InterRidge</strong> student prizes<br />

Student awards at: Ocean Mantle Dynamics: from Spreading<br />

Center to Subduction Zone” workshop, October 2011<br />

Akiko Takeo (Earthquake Research Institute of Tokyo University)<br />

received an IR best poster award for her work entitled: “Seismic<br />

anisotropy in the uppermost mantle beneath oceanic regions from<br />

data of broadband OBSs”. She is interested in the seismic velocity<br />

structure in the uppermost mantle, as it is one of the keys to<br />

understanding plate tectonics. Takeo analyses data from broadband<br />

ocean bottom seismometers deployed in oceanic regions such as the<br />

Shikoku Basin, south of Japan. 1D radially anisotropic structures<br />

beneath the Shikoku Basin can be obtained by measuring phase<br />

velocities of surface waves, indicating deformation at depths greater<br />

than 50 km.<br />

Of the Mantle Imaging workshop, she said: “It was a good<br />

experience for me to attend the workshop because I could discuss<br />

both methods and results with seismologists, geomagnetists and<br />

petrologists. Also I learnt from other presentations about structure<br />

and processes in the mid ocean ridges and subduction zones. The<br />

field trip was also a good chance to study the composition and<br />

deformation of peridotite by seeing real rocks”.<br />

Shusaku Yamazaki (Niigata University, Japan, working with Prof.<br />

Sumio Miyashita), was also awarded an IR student poster prize for<br />

his poster: “Formation of incipient oceanic island arc crust: geology<br />

and geochemistry of the late intrusive rocks in the Oman<br />

Ophiolite”. Oman ophiolite is considered as an analogue for fastspreading<br />

oceanic crust and upper mantle sequences. Yamazaki’s<br />

interest in the Oman ophiolite is the petrogenesis of late intrusive<br />

rocks with island arc type characteristics in the <strong>low</strong>er gabbroic crust.<br />

New mapping in the <strong>low</strong>er oceanic crustal sequence al<strong>low</strong>s<br />

recognition of the detailed distribution of late intrusive plutonics<br />

and boninitic dike swarms. In the poster, it is argued that their<br />

petrogenesis is based on petrography and geochemistry, and<br />

proposes that the complex of late intrusive plutonics in the mapped<br />

area can be regarded as a good example for early stage evolution of<br />

an intra-oceanic island arc crust.<br />

<strong>InterRidge</strong>-sponsored<br />

collaborations 2008-12<br />

Since 2008, <strong>InterRidge</strong> has<br />

been supporting early-career<br />

researchers across the world, and<br />

has built up an impressive network<br />

of collaborations, as can be seen<br />

here. The next challenge is to<br />

involve South America!<br />

International collaborations<br />

sponsored by <strong>InterRidge</strong> through<br />

its Fel<strong>low</strong>ship and cruise bursary<br />

programmes between 2008-12.<br />

INTERRIDGE NEWS 23 VOL.21, 2012

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