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Pyrite framboids and their development: a new conceptual mechanism

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Abstract

It has been suggested that the two morphologies of sedimentary pyrite, framboids and euhedra, may reflect two distinct pathways of pyrite formation. Framboids form indirectly via iron monosulphides, whereas euhedra form from direct precipitation from solution. A third pathway which is bridging these two forms is proposed here, namely the continuous growth from a monosulphide globule through framboids to a euhedral single crystal. It is also suggested that framboids probably occur over a range of three orders of magnitude, from the least complex microframboids through framboids to polyframboids.

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Authors and Affiliations

  1. Institute of Geological Sciences, Jagiellonian University, ul. Oleandry 2A, 30-063, Cracow, Poland

    Z. Sawlowicz

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Dedicated to Professors G. C. Amstutz and L. G. Love for their unrivalled contribution to the knowledge of pyrite framboids

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Sawlowicz, Z. Pyrite framboids and their development: a new conceptual mechanism. Geol Rundsch 82, 148–156 (1993). https://doi.org/10.1007/BF00563277

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