Resumo

KOSTADINOFF, J.. Geophysical evidence of the Trenque Lauquen High in the northern extension of the Claromecó Basin, province of Buenos Aires. Rev. Asoc. Geol. Argent. [online]. 2007, vol.62, n.1, pp.69-75. ISSN 0004-4822.

The geophysical survey of the northern border of Claromecó basin suggests the existence of Paleozoic sequences with important thickness. Such sequences extend along the NW area of Buenos Aires province. The Claromecó and Chaco Paranense Basins are divided by a semi positive area. A NNW-trending through, 165 km long, filled with Paleozoic sediments connects important thickness of both basins.

Palavras-chave : Geophysical; Prospection; Basins; Buenos Aires.

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