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On the distribution of silicic acid as a frontal zone tracer in the Indian sector of the Southern Ocean ArchiMer
Prego, R; Park, Yh; Barciela, Mc; Morvan, J; Poncin, J; Treguer, P.
The subantarctic frontal zone surveyed during the April-May 1991 SUZIL cruise in the Crozet-Kerguelen Amsterdam area shows a strong horizontal (north to south) gradient of dissolved silicate, increasing with depth, from 5 to 10 mu molSi kg(-1) at 100 m, and 10 to 70 mu molSi kg(-1) at 600 m. The northern limit of this frontal zone, which is formed by the confluence of the Subtropical and Subantarctic Fronts, is delimited at the surface by the 2 mu molSi kg(-1) silicate isoline. Silicate-salinity diagrams also allow different water regimes to be positioned relative to the frontal zone. This sloping interface is between two water bodies, one to the north with more saline subtropical waters of less concentrated silicate than the southern one, corresponding to...
Tipo: Text Palavras-chave: Silicate; Tracer; Frontal zone; Silicate-salinity diagram; Crozet Basin; Southern Ocean.
Ano: 1999 URL: https://archimer.ifremer.fr/doc/00239/35063/34593.pdf
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Detailed Structure and Plate Reconstructions of the Central Indian Ocean Between 83.0 and 42.5 Ma (Chrons 34 and 20) ArchiMer
Yatheesh, V.; Dyment, J.; Bhattacharya, G. C.; Royer, Jean-yves; Raju, K. A. Kamesh; Ramprasad, T.; Chaubey, A. K.; Patriat, P.; Srinivas, K.; Choi, Y..
The Central Indian Ocean, namely the Central Indian, Crozet, and Madagascar basins, formed by rifting and subsequent drifting of India (now Capricorn), Antarctica, and Africa (now Somalia). We gathered a comprehensive set of sea surface magnetic anomaly profiles over these basins and revisited location and identification of magnetic isochrons between C34ny (83.0 Ma) and C20ny (42.536 Ma) using the objective analytic signal technique. We present high-resolution magnetic isochrons for 29 periods based on similar to 1,400 magnetic anomaly picks. From the conjugate sets of picks, we derive two-plate finite rotation parameters for both the Capricorn-Antarctica and Capricorn-Somalia motions. These finite rotations are compared to three-plate reconstructions of...
Tipo: Text Palavras-chave: Magnetic isochrons; Central Indian Basin; Crozet Basin; Madagascar Basin; Plate reconstruction.
Ano: 2019 URL: https://archimer.ifremer.fr/doc/00637/74935/76014.pdf
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