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Stewart R. Wallace — 1919–2009 - Society of Economic Geologists

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JULY 2009 No 78 SEG NEWSLETTER 23<br />

SEG Distinguished Lecturer 2008 Report<br />

It was a surprise and an honor to be<br />

awarded the SEG’s Distinguished Lec -<br />

turer for 2008. My SEG lecture “tour”<br />

consisted <strong>of</strong> three parts: the first two<br />

were opportunities to piggyback on<br />

previously planned visits to conferences<br />

in Europe and North America, and the<br />

third was a short tour to various institutes<br />

within Australia. In each case I<br />

presented variations <strong>of</strong> a lecture entitled<br />

“The Kermadec-Tonga intraoceanic arc:<br />

An 8-year odyssey <strong>of</strong> discovery.”<br />

Our group here at GNS Science,<br />

Lower Hutt, New Zealand, in collaboration<br />

largely with our American colleagues<br />

at NOAA in Seattle and<br />

Newport, but also other groups from<br />

Australia (ANU), Canada (University<br />

<strong>of</strong> Ottawa), Germany (Kiel University<br />

and GEOMAR), Italy (IAMC and INGV),<br />

Japan (JAMSTEC and the University <strong>of</strong><br />

Kyushu), and New Zealand (NIWA),<br />

has been investigating submarine<br />

hydro thermal systems associated<br />

mainly with intraoceanic arcs. Our<br />

group has largely focused on the<br />

Kermadec-Tonga arc, where most <strong>of</strong><br />

the volcanic centers along this ~2,500km-long<br />

arc have been surveyed for<br />

their hydrothermal plumes. The initial<br />

plume survey cruise, known as<br />

NZAPLUME I, was conducted in<br />

1999 along the southern part <strong>of</strong> the<br />

Kermadec arc, to be followed by<br />

NZAPLUME’s II and III along the middle<br />

and northern parts <strong>of</strong> the Kermadec<br />

arc, respectively. Additional plume<br />

mapping cruises were also done along<br />

the Tonga arc. Twelve major volcanoes<br />

have been investigated and their<br />

hydrothermal systems sampled by the<br />

manned submersibles Shinkai 6500 and<br />

Pisces V, with the Canadian remotely<br />

operated vehicle ROPOS and the<br />

American autonomous underwater<br />

vehicle ABE also having been deployed<br />

at some <strong>of</strong> these volcanoes. We have<br />

also done similar surveys, with our various<br />

colleagues, along the submarine<br />

portions <strong>of</strong> the Tabar-Lihir-Tanga-Feni<br />

island arc <strong>of</strong>fshore Papua New Guinea,<br />

the Ghizo Ridge fore-arc <strong>of</strong>fshore the<br />

Solomon Islands, and the Aeolian arc<br />

<strong>of</strong>fshore Italy. Our American colleagues<br />

have led similar cruises along the<br />

Mariana intraoceanic arc.<br />

Cornel E.J. de Ronde (SEG 1993 F)<br />

The SEG Lectureship<br />

afforded me the opportunity<br />

to showcase<br />

some <strong>of</strong> the results from<br />

these spectacular hydro -<br />

thermal systems. Dis -<br />

coveries have included<br />

high temperature (up to<br />

300°C) black smokers<br />

vents with 5–7 m tall<br />

sulfide chimneys, very<br />

acid vent fluids (with<br />

pH

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