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Introduction
The Argentine continental shelf has a number of distinguishing attributes with a structural history characterized by plate breakup, heat flow and magmatic activity, which have shaped its current tectonic features. The study of magnetic anomalies reveals the structural and lithologic complexity of crustal rocks, providing a window into the geological history of various sectors of the continent, mainly ancient deep-crustal formations whose seismic structures are unclear due to subsequent tectonic and metamorphic activity. The total magnetic anomaly (TMA) of an area allows the main crustal structures, faults, dykes, transform zones and edges or contacts to be rapidly located and characterized (Lefort et al., ). Therefore, by utilizing the results of filtering techniques, it is possible to analyse the structure of the Argentine continental shelf, the main offshore basin structures and the continental edge.
Several authors have conducted research in this area, including gravimetric studies of the continental-oceanic boundary (Arecco et al., a,b) and magnetic studies of the continental crust (Ghidella et al., , Max et al., ). In addition, investigations such as isostatic compensation and geoid undulation studies in the Claromecó basin (Ruiz and Introcaso, ), te
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DRY WEATHER and above normal interior temperatures today. A shortwavetrough will bring increasing moisture, with a chance for light to moderate rainfall tonight and Monday morning. Cooler temperatures can also be expected into early next week with and after the passing or a shortwave trough. (NWS)
STEPHEN DUNLAP (Fort Bragg): Clear skies & 48F on the coast this Sunday morning. Scattered periods of patchy fog (maybe a shower tomorrow morning?) this week leading to a chance of rain on Thursday. Looks like we might see some passing high clouds today.
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