Sr-Nd-Pb isotope evidence for the derivation of Maipo and other volcanic rocks between 33o20’S and 35o20’S, Central Andes: Less need for a subduction zone contribution
Research output: Contribution to conference › Conference abstract for conference › Research › peer-review
Original language | Danish |
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Publication date | 2011 |
Number of pages | 1 |
Publication status | Published - 2011 |
ID: 37761491