The Bouvet Tr1p1e Junction Region (south Atlantic): a report on two geological expeditions

Gabriela Carrara$^1$, Giovanni Bortoluzzi$^1$, Nevio Zitellini$^1$,

Enrico Bonatti$^1$, Daniele Brunelli$^2$, Anna Cipriani$^2$, Paola Fabretti$^1$,

Luca Gasperini$^1$, Marco Ligi$^1$, Daniela Penitenti$^1$,

Pier Francesco Sciuto$^3$, Alexander Mazarovich$^4$, Alexander Peyve$^4$,

Natalija Turko$^4$, Sergei Skolotnev$^4$, Dolores Gilod$^5$

$^1$ IGM-ISMAR-CNR, Bologna, Italy

Received: March 2010 / Accepted: May 2010 - PDF FOR PRINT

Abstract:

The Bouvet Triple Junction is located where the Antarctic, south American and African plates meet in the south Atlantic. Two oceanographic expeditions were carried out in this region in 1994 and 1996 by the Institute of Marine Geology, CNR (Bologna), and the Geology Institute of the Russian Academy of Science (Moscow) under the sponsorship of the Italian Antarctic Research Program (PNRA). The main objectives of these expeditions were to define the structural, morphological and petrographical differences of the three divergent margins that meet in the Bouvet region, and to clarify the evolution in space and time of the geometry of the Triple Junction. Single and multichannel seismic reflection, gravimetric and magnetometric profiles were obtained during the first cruise, with the R/V Akademik Strakhov, in addition to medium resolution multibeam bathymetry of the Bouvet island area and in the southem portion of the Mid Atlantic Ridge. The second cruise, carried out with the R/V Gelendzhik, completed the bathymetric survey of the entire Triple Junction region using an high resolution multi- beam system. Seafloor sampling was carried out by dredging in both cruises. Some of the data obtained during these two expeditions are reported in this paper.

Figure 1: