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From Migmatites to Plutons: Power Law Relationships in the Evolution of Magmatic Bodies

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Abstract

Magma is generated by partial melting from micrometre-scale droplets at the source and may accumulate to form >100 km-scale plutons. Magma accumulation thus spans well over ten orders of magnitude in scale. Here we provide measurements of migmatitic leucosomes and granitic veins in drill cores from the Estonian Proterozoic basement and outcrops at Masku in SW Finland and Montemor-o-Novo, central Portugal. Despite the differences in size and number of measured leucosomes and magmatic veins, differences in host rock types and metamorphic grades, the cumulative width distribution of the studied magmatic leucosomes/veins follows a power law with exponents usually between 0.7 and 1.8. Published maps of the SE Australian Lachlan Fold Belt were used to investigate the distribution of granitoid pluton sizes. The granites occupy ca. 22 % of the 2.6 × 105 km2 area. The cumulative pluton area distributions show good power law distributions with exponents between 0.6 and 0.8 depending on pluton area group. Using the self-affine nature of pluton shapes, it is possible to estimate the total volume of magma that was expelled from the source in the 2.6 × 105 km2 map area, giving an estimated 0.8 km3 of magma per km2. It has been suggested in the literature that magma batches in the source merge to form ever-bigger batches in a self-organized way. This leads to a power law for the cumulative distribution of magma volumes, with an exponent m V between 1 for inefficient melt extraction, and 2/3 for maximum accumulation efficiency as most of the volume resides in the largest batches that can escape from the source. If m V ≥ 1, the mass of the magma is dominated by small batches; in case m = 2/3, about 50 % of all magma in the system is placed in a single largest batch. Our observations support the model that the crust develops a self-organized critical state during magma generation. In this state, magma batches accumulate in a non-continuous, step-wise manner to form ever-larger accumulations. There is no characteristic length or time scale in the partial melting process or its products. Smallest melt segregations and >km-scale plotuns form the end members of a continuous chain of mergers of magma batches.

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Notes

  1. "Melt" is pure molten (liquid) rock, while "magma" refers to liquid melt that may contain floating solid crystals or entrained pieces of solid rock. In this paper we use the term "magma" throughout.

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Acknowledgments

This study was supported by the Estonian Ministry of Education and Research target research project no. SF0140016s09 and by grant no. 8963 (ESF) to AS.

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  1. Institute of Geology, Tallinn University of Technology, Ehitajate tee 5, Tallinn, 19086, Estonia

    Alvar Soesoo

  2. Department of Geosciences, Eberhard Karls University Tübingen, Wilhelmstr. 56, 72074, Tübingen, Germany

    Paul D. Bons

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Soesoo, A., Bons, P.D. From Migmatites to Plutons: Power Law Relationships in the Evolution of Magmatic Bodies. Pure Appl. Geophys. 172, 1787–1801 (2015). https://doi.org/10.1007/s00024-014-0995-4

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