Cumulate Thermobarometry

Lead Research Organisation: University of Bristol
Department Name: Earth Sciences

Abstract

The Lesser Antilles volcanic arc provides an unusually complete and accessible case study of an active island arc subduction zone, formed by the subduction of the American plate under the eastern edge of the Caribbean plate since at least the Eocene. The arc offers a worldclass opportunity to explore subduction zone processes in a relatively simple intraoceanic setting.
Arc-magmatism processes take place at depth and must be inferred through information available at the surface. A major source of such information is the nature and composition of magmatic rocks, which may either be erupted as lava from the volcanoes, or crystallized within the volcanic plumbing system, carried to the surface by ascending magma, and erupted as xenoliths within it. Both lavas and xenoliths reflect aspects of the processes that take place between the melting of volatile-rich magma in the mantle wedge above the subducting plate, and the eruption of lavas on the surface.
An important category of xenoliths, known as cumulates, are formed from crystals that grew in a cooling magma, sank and accumulated at the bottom of the magma chamber, thereby indicating magma storage at discrete locations in the volcanic system. The cumulate sequences that are parental to these xenoliths lie at an unknown depth in the Earth's crust, but must contain extensive information encoded in the compositions of their crystals and captured bubbles of melt. This information includes hints about the source of the magma from which the cumulates crystallized, and its mixing with other magmas during storage and transport. Investigators are currently obliged to make inferences based on the population of cumulate xenoliths, without having a coherent picture of the parental cumulate sequences at depth under the arc, or the relationships of the various cumulate samples to each other.
In this study we will attempt to gain a coherent understanding of distribution of buried cumulate sequences, both laterally along the arc and at depth. Previous work by the PI and co-workers has detailed the variation in the mineralogy, textural appearance and composition of cumulate xenoliths erupted along the arc; these are interpreted as showing that, towards the north of the arc, the magma chambers feeding the individual volcanoes tend to lie at shallower levels, and the magmas contain a higher proportion of water. Small but important gaps remain in sampling of cumulate xenoliths along the 750km length of the arc, and we propose to rectify these.
A new method is required to derive precise depths and temperatures of cumulate crystallization from compositions of minerals in the xenoliths. We will make use of a large database of experiments with products that approximately mimic the observed cumulate xenoliths; we will supplement it with additional experiments, to ensure that the full observed range of cumulate compositions and mineralogies has been obtained under controlled conditions of pressure, temperature, volatile content and oxygen fugacity. We will then calibrate thermodynamic models against the database, representing each of the observed mineral phases. The models will characterize the variation of composition with the controlled conditions among mineral phases in equilibrium. They will be calibrated with a view to being able to recover the experimental conditions via a rigorous statistical analysis.
The finished models will then be applied to the database of natural samples, with the aim of building up an approximate three-dimensional picture of the subsurface magma storage system based on the samples that reach the surface. In principle this information may be combined with and verified against seismic imaging, which uses seismicity to probe crustal structure, and also with radiometric dating to provide a time-dimension to the analysis. The models and interpretations derived from this project will be relevant to a number of other subduction zone settings worldwide.

Planned Impact

1. Who might benefit from this research?

The goal of this study is to develop tools that allow the precise estimation of cumulate PT conditions, using a thermodynamic approach. Application of such tools to an unprecedented, large set of cumulates of the Lesser Antilles arc shall place valuable constraints on the different models that exist at present for continental crust formation. Our tools will also have widespread applicability to other igneous cumulates and to geophysical studies of crustal structure, and can therefore be helpful for hazard assessments. The project has value for GCSE-level school classes in Physical Geography. Subduction zones themselves provide perhaps the most exiting tectonic setting to be taught at schools, as they mark the sites of the world's most explosive volcanoes, the largest earthquakes and associated hazards (tsunamis), as well as some of the largest base metal deposits.

Various UK-based and international beneficiaries can hence be distinguished:

(a) Academic beneficiaries

(b) Volcanic surveys and observatories

(c) General public

2. How might they benefit form this research?

(a) Academic beneficiaries: see separate section.

(b) Volcanic surveys and observatories: We anticipate that our tools will eventually be applicable to other arcs that erupt similar volcanic and cumulate compositions. Hence, our tool will be most very valuable for volcanologists that asses volcanic hazards in observatories and surveys, given that PT estimates of magma chamber cannot be routinely extracted at present.

(c) General public: We will engage in a public outreach activities, including participation in open days, and getting involved in an active programme of outreach activities to schools. As part of this plan, we anticipate in conveying a 10 minute film suitable for pupils up to and including GCSE level, to be distributed free to schools. The video production company "Back to the Planet" (http://www.backtotheplanet.co.uk/), specialising in environmental and social issues, is keen to see a short film made of our work. Our contacts there would support us with advice on achieving high-quality, high-interest footage for relatively low cost with minimal environmental impact. We believe that such a state-of-the-art movie on subduction zone geodynicamic will ensure that pupils gain a much better understanding on how the earth works. By targeting students before GCSE and A-level choices are made it is hoped to ensure that those with the motivation to study earth sciences and adequately equipped to do so.

Publications

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Cooper GF (2016) Plutonic xenoliths from Martinique, Lesser Antilles: evidence for open system processes and reactive melt flow in island arc crust. in Contributions to mineralogy and petrology. Beitrage zur Mineralogie und Petrologie

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Stamper C (2014) Oxidised phase relations of a primitive basalt from Grenada, Lesser Antilles in Contributions to Mineralogy and Petrology

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Ziberna L (2017) Multiple-reaction geobarometry for olivine-bearing igneous rocks in American Mineralogist

 
Description We have developed a technique for recovering the pressure and temperature of rocks containing a specific mineral assemblage. This thermobarometer relies on a thermodynamic database that we have optimised for application to cumulate igneous rocks containing the mineral assemblage: olivine + clinopyroxene + plagioclase + spinel. The thermobarometer has widespread applicability and wil be especially useful in reconstructing the structure of arc crust as revealed by erupted crustal xenoliths.
Exploitation Route The thermobarometer is available using online tools to enhance wide usage. The original researcher on the project is currently at Bayreuth University in Germany and is extending the methods to take into account amphibole.
Sectors Environment

 
Description The findings have been used to constrain magmatic differentiation beneath subduction zones for use in developing models of porphyry copper mineralisation
First Year Of Impact 2017
Sector Other
Impact Types Economic