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Los pueblos de la actual provincia de Buenos Aires se fueron conformando mayormente de manera espontánea, a medida que se asentaba la población y se avanzaba sobre el espacio apropiado a los indígenas; en la mayoría de los casos al amparo de los fuertes o las capillas. Los ejidos de esos pueblos existían de hecho como tierras de pan llevar pero se trazaron formalmente recién durante el siglo XIX. A lo largo de este trabajo se analizará el modo en que se operó la construcción de un cuerpo jurídico para los ejidos bonaerenses poniendo especial interés en la influencia del derecho indiano

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The paper is based on new results of melt inclusion studies in minerals. Physicochemical and geochemical parameters of plateau basalt magmatic systems of the Siberian Platform and Ontong Java Plateau (Pacific Ocean) have been established. The studied melts are enriched in Fe. That differs them from magmatic melts of mid-ocean ridges (MOR). A comparative analysis of data on inclusions has shown a similarity of continental and oceanic plateau basalt magmatic systems. They considerably differ from those of MOR and intraplate oceanic islands. Crystallization of oceanic plateau basalts took place at lower temperatures and pressures as compared with similar rocks of the Siberian Platform. The data on inclusions evidence that the melts of the Siberian Platform and the Malaita Island underwent a serious evolution in contrast to magmas of the Nauru Basin that have more stable geochemical parameters. The most fractionated low-temperature high-Fe magmas with elevated contents of trace and rare-earth elements occur in the Malaita Island (Ontong Java Plateau) magmatic system.

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