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Abstract-Late Eocene tektite material from DSDP site 612 is composed of angular to spherical tektites and microtektites containing abundant vesicles and a few unmelted to partially melted mineral inclusions. The major element compositions of the 6l2-tektites are generally comparable to those of North American tektites, but the physical features suggest that the DSDP-6l2 tektites were formed by less severe shock melting. The 8'Sr/ 8·Sr and 143Nd/ 144Nd compositions of 6l2-tektites: a) show much wider ranges than the tightly constrained group of North American tektites and microtektites, and b) are significantly different from those of other groups of tektites. The existence of large isotopic variations in tektites from DSDP site 612 requires that they were formed from a chemically and isotopically heterogeneous material in a regime that is distinctive from that of other groups of tektites. T~~uR and T~R model ages of the 6l2-tektites indicate that they were formed from a crustal source of late Precambrian mean age (800-1000 Ma) which in middle Palaeozoic time (""400 Ma) was further enriched in Rb/Sr during sedimentary processes. These source characteristics suggest that the impact which produced the 6l2-tektites occurred in rocks of the Appalachian orogeny or sediments derived from this orogenic belt. Potential source materials for both 6l2-tektites and North American tektites are present on the eastern and southeastern part of the North American continent and its adjacent shelf. The distinct isotopic differences between 6l2-tektites and North American tektites indicate that the two groups of tektites were either formed by the impact of more than one bolide in the same general area, or by a single impact event that sampled different layers.

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