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IGCP Project short title: Caribbean Plate Tectonics Duration and ...

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6.2 SCIENTIFIC MEETINGS AND WORKSHOP REPORTS<br />

15<br />

GENERAL SYMPOSIUM 17-6. CARIBBEAN PLATE TECTONICS, ORIGIN AND<br />

EVOLUTION. 31 INTERNATIONAL GEOLOGICAL CONGRESS, RÍO DE JANEIRO<br />

August 6 to 17, 2000<br />

Conveners: Manuel A. Iturralde-Vinent <strong>and</strong> Edward G. Lidiak<br />

This symposium was dedicated to analyzing the present status of <strong>Caribbean</strong> <strong>Plate</strong><br />

Tectonic models. Four special oral presentations <strong>and</strong> 12 posters were the subject of<br />

interesting debates <strong>and</strong> active exchange of data <strong>and</strong> interpretations.<br />

The oral session, attended by more than 50 persons, was celebrated the morning of<br />

August 7th. Four special speakers presented their respective viewpoints concerning how they<br />

underst<strong>and</strong> the formation <strong>and</strong> evolution of the <strong>Caribbean</strong>, but the fact is that each one<br />

produced a quite distinct scenario. In this regard, it is important to quote the senior convener,<br />

in the fact that "The <strong>Caribbean</strong> is a singular area of planet Earth, <strong>and</strong> therefore, it had had a<br />

single history". The plate tectonic models that explain the <strong>Caribbean</strong> plate as an<br />

allochthonous crust originated within the Pacific Ocean, was very well exemplified by the<br />

model of J. Pindell <strong>and</strong> L. Kennan. The special speaker Martin Meschede reviewed some<br />

<strong>short</strong>comings of recent Pindell's <strong>and</strong> Paul Mann's models, <strong>and</strong> presented his arguments for an<br />

in situ origin of the <strong>Caribbean</strong> plate. Another version of the in situ model was presented by<br />

Giuseppe Giunta (visit Comparison at Carib<strong>Plate</strong> Web Site). M. Iturralde-Vinent, as special<br />

speaker, evaluated the few similarities <strong>and</strong> many contradictions that exist among modern<br />

<strong>Caribbean</strong> <strong>Plate</strong> Tectonic models (visit Forum at Carib<strong>Plate</strong> Web Site). The in situ models<br />

were criticized because they have a problem of space in explaining the Cretaceous <strong>and</strong> early<br />

Tertiary Greater Antilles-Aves Ridge-<strong>Caribbean</strong> mountains subduction-related volcanic arcs.<br />

Some questions were also raised concerning the polarity of these arcs <strong>and</strong> the original<br />

position of some terranes of the <strong>Caribbean</strong> margins, subjects that will require more careful<br />

attention in the future.<br />

Twelve papers were presented at the Poster Session which was held in the afternoon<br />

on both August 7th <strong>and</strong> 8th. They included three of the special oral presentations as well as<br />

new results from field research in key areas of Cuba, Puerto Rico, Venezuela, <strong>and</strong> Costa<br />

Rica. This session produced an active exchange of viewpoints among presenting authors, but<br />

also with many interested congress members.<br />

The conveners <strong>and</strong> participants agreed that the symposium was an excellent forum<br />

for the most valuable exchange of ideas, but as exciting was the possibility to meet people<br />

based in different areas of the world with personal expertise <strong>and</strong> strong interest in the<br />

<strong>Caribbean</strong>. In terms of the scientific impact of the symposium, we concluded that despite the<br />

great amount of valuable information available about the <strong>Caribbean</strong> submarine <strong>and</strong> l<strong>and</strong><br />

15

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