Basaltic rocks from the Andean Southern Volcanic Zone: Insights from the comparison of along-strike and small-scale geochemical variations and their sources
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文摘

Volcanic rocks from different segments of the Andean SVZ are geochemically distinct.

Large-scale differences between TSVZ and CSVZ magmas are duplicated on a small-scale.

In CSVZ and SSVZ, the Liquine–Ofqui Fault System permits ascent of diverse magmas.

Asthenospheric magma with subduction input assimilates mantle lithosphere and crust.

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