Crystal population density in not stationary volcanic systems: estimate of olivine growth rate in basalts of Lanzarote (Canary Islands)

Author:

Armienti P.,Innocenti F.,Pareschi M. T.,Pompilio M.,Rocchi S.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference27 articles.

1. Armienti P, Innocenti F, Masotti R, Pasquarè G, Pirera F (1989) Petrology of the basaltic lavas of Lanzarote. ESF Meeting on Canarian Volcanism, pp 83?84

2. Bottinga Y, Weill D, Richet P (1982) Density calculations for silicate liquids. I. Revised methods for aluminosilicate composition. Geochim Cosmochim Acta 46: 909?919

3. Calzolari G, Cipriani TA, Corsi P (1976) Generation and testing of pseudo-random numbers with assigned statistical properties to be used in the stochastic simulation of econometric models. IBM Tech Rep n. G513?3545, 42pp

4. Carracedo JC, Rodrignet Badiola E, Soler V (1991) The 1730?1736 eruption of Lanzarote: an unusually long, high magnitude fissurol basaltic eruption in the recent volcanism of the Canary Islands. Submitted to Contrib Mineral Petrol

5. Cashman KV (1988) Crystallization of Mount St. Helens 1980-86 dacite: A quantitative textural approach. Bull Volcanol 50: 194?209

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