Chemical differences between the island and submarine pumice layers of Thera
作者： A. Vinci
DOI: 10.1016/0025-3227(84)90083-5
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摘要: Abstract Investigations on tephra layers of deep-sea cores from near the island Santorini showed that only pumice clasts west can be attributed to Minoan eruption. The within caldera are uncertain origin.
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sci-hub.se 参考文章(1)
H. Puchelt, Recent Iron Sediment Formation at the Kameni Islands, Santorini (Greece) Springer, Berlin, Heidelberg. pp. 227- 245 ,(1973) , 10.1007/978-3-642-65329-2_18