The structural evolution of the Johannesburg Dome, Kaapvaal Craton, South Africa

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Why are there no low-δ18O magmas In convergent margins? A case of the Central Andes, Northern Chile by Sigauke, Connie

“…Low-δ 18O magmas are rare, worldwide, especially in subduction zone settings. The main objective of this study was to conduct a search for low-δ 18O magmas in the Central Volcanic Zone (CVZ) of the Andes, to verify if their rarity is due to under sampling. …”
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