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The tsavorite (gem quality green vanadium grossular) minerogenetic system in East Africa: a case of metamorphic partial melting and lateral secretion

  • CAJG 2018: Topic 10
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Abstract

When supercontinent Rodinia began to break up at ~ 800 Ma, wide rifts formed evolving into a passive margin of the Mozambique Ocean. At one stage, organic-rich pelites with gypsum/anhydrite (the later host rock of tsavorites) were interbedded with siliciclastics, carbonates, and bimodal volcanic rocks. Later, ocean closure, subduction, collision, and welding of various microcontinents and volcanic arcs formed the Mozambique Belt and at ~ 550 Ma, ended with the assembly of supercontinent Gondwana. In East Africa, deformation and metamorphism climaxed at 615–600 Ma. At peak metamorphic conditions, anatexis of siliciclastic metasediments produced abundant metamorphic mobilizates such as pegmatites and quartz veins. In the graphite schist hosting tsavorites, however, partial melting only produced small fractions of a supercritical hydrous liquid, the peculiar corrosive nature of which was due to the reduction of Ca-sulfate by reaction with organic C. Most of this melt/fluid phase remained within the host but migrated over short distances into structural traps of different origin; turbid green grossular crystallized from the melt and transparent tsavorite from residual fluids.

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Acknowledgments

I am grateful to the The Evaluation and Publication Committee of CAJG-2018 Tunisia (www.cajg.org), who invited me to submit this paper; my paper no. 81 having been selected by Springer Editors as one of the best contributions to the 1st Conference of the Arabian Journal of Geosciences, Tunisia 2018 (CAJG-2018).

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Correspondence to Walter Leopold Pohl.

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Responsible Editor: François Roure

This paper was selected from the 1st Conference of the Arabian Journal of Geosciences (CAJG), Tunisia 2018

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Pohl, W.L. The tsavorite (gem quality green vanadium grossular) minerogenetic system in East Africa: a case of metamorphic partial melting and lateral secretion. Arab J Geosci 12, 612 (2019). https://doi.org/10.1007/s12517-019-4744-y

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