Experimental Development of Transport Percussion Marks on Obsidian Clasts, Pilauco Site, Chilean Nor...
Experimental Development of Transport Percussion Marks on Obsidian Clasts, Pilauco Site, Chilean Northwestern Patagonia
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Basel: MDPI AG
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English
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Basel: MDPI AG
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In the Pilauco site (40°34′11″ S, 73°06′17″ W; 13,570 ± 70–12,540 ± 90 14C year BP), a previous geochemical trace analysis suggested that the Puyehue-Cordón Caulle Volcanic Complex is the most likely source for obsidian and dacitic glass artifacts at Pilauco. It was hypothesized that the glassy rocks were probably collected from a pebble beach depo...
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Experimental Development of Transport Percussion Marks on Obsidian Clasts, Pilauco Site, Chilean Northwestern Patagonia
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TN_cdi_proquest_journals_2642512690
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2642512690
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ISSN
2075-163X
E-ISSN
2075-163X
DOI
10.3390/min12030343
