Origin and structural character of hauyne(ss) in spinel dunite xenoliths from La Palma, Canary Islands

Two spinel dunite xenoliths (Fo(89.8-91.2) in olivine) from La Palma contai n minor amounts (<1%) of a pale-blue sodalite-group mineral with hauyne/laz urite chemistry. Selected-area electron diffraction (SAED) patterns of this phase indicate a cubic unit cell with dimensions 9.12 +/- 0.02 Angstrom, a nd space group P (4) over bar 3n. Superstructure spots along three <110> di rections are common, implying commensurate or incommensurate modulations al ong <110> directions. Raman spectra show peaks typical of both lazurite and hauyne. It is concluded that the mineral has a structure intermediate betw een those of pure lazurite and pure hauyne, and it is here referred to as h auyne(ss). The hauyne(ss) occurs together with strongly nepheline-normative glass in thin veinlets (<0.1 mm), in interstitial glass pockets, and as in clusions in olivine porphyroclasts. To our knowledge lazurite or hauyne has not previously been described in mantle rocks. The hauyne(ss) is strongly depleted in REE and most other highly lithophile elements relative to the c oexisting glass, whereas D-mineral/glass for Sr is approximate to 1.0, and D-Eu higher than the other REE. The hauyne(ss) crystallized from a melt now present as phonolitic glass, probably in response to rapidly decreasing pr essure during transport of the xenoliths to the surface. The coexistence of hauyne(ss) and FeS-rich sulfide globules in some samples suggests slightly more oxidizing conditions than for samples in which the glass contains sul fide globules alone.