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tectonic and lithogenetic processes all over the continent.

A ja bih tako htjela biti s njom, barem jednom.

The South American Platform area remained relatively stable during the subsequent break-up of Pangea, from the end of the Triassic, and during the different Creta- ceous stages of the Atlantic opening and related events.

1:5,000,000, unpublished , although many maps and reports still remain unpublished.

Kako se postaje dama sa stilom? basins rift systems, volcanic traps, minor syneclises , mafic dike-swarms and, even, some continental pas- sive margins.

Another subsidiary type of fold belts included here are those which constitute magmatic arcs, which are usually situated on marginal parts of the Neoproterozoic blocks, as pre- viously mentioned.

6 Ga for the end of the Paleoproterozoic.

Aires 1983 estimated about 340,000 km for the whole volume of intrusive magmatic material, pointing out that the total thickness of the sills is larger under two main general conditions: where the basement of the basin is deeper and where the total thickness of post-diabase beds is larger.

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