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Title: Wall rock-magma interactions in Etna, Italy, studied by U-Th disequilibrium and rare earth element systematics

Conference · · Geochimica et Cosmochimica Acta; (United States)
OSTI ID:6390736
 [1]; ;  [2]
  1. Universite Paris 6 (France) CNRS URA 196, Paris (France)
  2. LPS/CEA-CNRS, Gif-sur-Yvette (France)

[sup 230]Th/[sup 238]U disequilibria have been studied in xenoliths and associated lavas of the 1892 and 1989 eruptions of Etna. Most xenoliths are out of secular equilibrium within 1 [sigma] errors and have lower [sup 230]Th/[sup 232]Th ratios than their host magmas. Siliceous and peraluminous xenoliths display large ranges of Th/U ratios for similar [sup 230]Th/[sup 232]Th values, which are interpreted in terms of Th isotopic rehomogenization. The siliceous xenoliths have also suffered thorium and uranium enrichments, which are best explained by chemical diffusion between xenolith melts and differentiated magmas. Estimates of thorium self-diffusivities and [sup 230]Th-[sup 238]U disequilibria give age constraints on these events corresponding to the last major volcanic event of Etna at 14 ka (formation of the elliptic crater caldera). These results suggest that magma storage in superficial and long-lived magma chambers favors the thorium isotopic homogenization of wall rocks by a thermal effect. Chemical diffusion of uranium and thorium and isotopic homogenization between siliceous melts of wall rocks and differentiated magmas may significantly modify the initial thorium isotopic compositions. Such contamination processes could explain the large variations of the [sup 230]Th/[sup 232]Th initial ratios of Etna magmas. 33 refs., 7 figs., 1 tab.

OSTI ID:
6390736
Report Number(s):
CONF-911017-; CODEN: GCACAK
Journal Information:
Geochimica et Cosmochimica Acta; (United States), Vol. 57:6; Conference: Annual meeting and exhibition of the Geological Society of America, San Diego, CA (United States), 21-23 Oct 1991; ISSN 0016-7037
Country of Publication:
United States
Language:
English