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In situ quantification of crystallisation kinetics of plagioclase and clinopyroxene in basaltic magma: Implications for lava flow

DOI: 10.1016/j.epsl.2021.117016 DOI Help

Authors: Nolwenn Le Gall (University College London; Research Complex at Harwell) , Fabio Arzilli (University of Manchester) , Giuseppe La Spina (University of Manchester) , Margherita Polacci (University of Manchester) , Biao Cai (University of Manchester) , Margaret E. Hartley (University of Manchester) , Nghia T. Vo (Diamond Light Source) , Robert C. Atwood (Diamond Light Source) , Danilo Di Genova (University of Bristol) , Sara Nonni (University of Manchester Harwell Campus) , Edward W. Llewellin (Durham University) , Mike R. Burton (University of Manchester) , Peter D. Lee (University College London; Research Complex at Harwell)
Co-authored by industrial partner: No

Type: Journal Paper
Journal: Earth And Planetary Science Letters , VOL 568

State: Published (Approved)
Published: August 2021
Diamond Proposal Number(s): 12392

Abstract: Crystallisation is a complex process that significantly affects the rheology of magma, and thus the flow dynamics during a volcanic eruption. For example, the evolution of crystal fraction, size and shape has a strong impact on the surface crust formation of a lava flow, and accessing such information is essential for accurate modelling of lava flow dynamics. To investigate the role of crystallisation kinetics on lava flow behaviour, we performed real-time, in situ synchrotron X-ray microtomography, studying the influence of temperature-time paths on the nucleation and growth of clinopyroxene and plagioclase in an oxidised, nominally anhydrous basaltic magma. Crystallisation experiments were performed at atmospheric pressure in air and temperatures from 1250 °C to 1100 °C, using a bespoke high-temperature resistance furnace. Depending on the cooling regime (single step versus continuous), two different crystal phases (either clinopyroxene or plagioclase) were produced, and we quantified their growth from both global and individual 3D texture analyses. The textural evolution of charges suggests that suppression of crystal nucleation is due to changes in the melt composition with increasing undercooling and time. Using existing viscosity models, we inferred the effect of crystals on the viscosity evolution of our crystal-bearing samples to trace changes in rheological behaviour during lava emplacement. We observe that under continuous cooling, both the onsets of the pāhoehoe-‘a‘ā transition and of non-Newtonian behaviour occur within a shorter time frame. With varying both temperature and time, we also either reproduced or approached the clinopyroxene and plagioclase phenocryst abundances and compositions of the Etna lava used as starting material, demonstrating that real-time synchrotron X-ray tomography is an ideal approach to unravel the final solidification history of basaltic lavas. This imaging technology has indeed the potential to provide input into lava flow models and hence our ability to forecast volcanic hazards.

Journal Keywords: X-ray microtomography; basalt; crystallisation; lava flow

Diamond Keywords: Volcanology

Subject Areas: Earth Science

Instruments: I12-JEEP: Joint Engineering, Environmental and Processing

Discipline Tags:

Earth Sciences & Environment Geology Natural disaster Geochemistry

Technical Tags:

Imaging Tomography