V33A-4832:
Short- and Long-lived Silicic Volcanism at Árnes and Hafnarfjall-Skarðsheiði Central Volcanoes, Iceland
Wednesday, 17 December 2014
Tenley Banik1, Calvin F Miller1, Matthew A Coble2, Rita C Economos3 and Christopher M Fisher4, (1)Vanderbilt University, Nashville, TN, United States, (2)Stanford University, Stanford, CA, United States, (3)University of California Los Angeles, Earth and Space Sciences, Los Angeles, CA, United States, (4)Washington State University, Pullman, WA, United States
Abstract:
Relocation of Iceland’s subaerial rift zones over the last ~20 Myr has controlled the formation of voluminous silicic magmas in an intra-oceanic setting. While partial melting of hydrated basaltic crust plays an important role in generating silicic magmas at on-rift central volcanoes in Iceland, little is known about the timescales involved in generating silicic magmas or the petrogenesis of these evolved melts. In situ zircon analyses (U-Pb and trace elements by SHRIMP-RG, Stanford/USGS; δ18O by ims 1270, UCLA; εHf by Neptune MC-ICPMS, WSU) from silicic magmas from the Árnes and Hafnarfjall-Skarðsheiði (HS) central volcanoes in northwestern and western Iceland provide potential end members for investigating longevity and geochemical variation. Silicic magmatism at both large (>20 km diameter) centers began ~2 Myr after their parent rifts relocated and ≥20% of the erupted material is silicic in composition; however, longevity and petrogenetic processes vary between Árnes and HS. U-Pb ages reveal a short-lived (0.5 Myr) silicic lifespan for Árnes (12.8-13.3 Ma) vs. ~1.5 Myr life for HS (3.8-5.2 Ma). At HS, zircon δ18O is lowest in older units (averaging ~1.8‰ at 5.2 Ma), progressively increases to 3.3‰ in the middle units and decreases slightly in the youngest units (2.9‰; δ18O 2σ uncertainty for all samples is ~0.5–1‰), suggesting a history of silicic magma generation through partial melting of hydrothermally altered crust, transitioning toward either a greater role for fractional crystallization of basaltic parent magma or a less altered source over the volcano’s lifetime. Árnes units’ δ18O are homogeneous within error (3.2–3.6‰) and show no age correlation, consistent with a simpler petrogenetic history. Hf isotopic data reveal a more strongly depleted mantle signature for Árnes zircons (εHf0 avg~12.3±1.7) than for HS magmas (εHf0 avg~11.4±1.5).