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The mineralisation is interpreted to have formed from hydrothermal fluid flow, either gravity or tectonically driven, after peak Alleghanian deformation in eastern Tennessee with regional dolomitisation of the host rocks occurring as part of a continuum during the ∼20 Ma prior to and during peak deformation.
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The Mascot–Jefferson City (M-JC) Mississippi Valley-type (MVT) deposits are in the Valley and Ridge province of the Appalachian orogen in East Tennessee.
They have been a major source of zinc for the USA but their age is uncertain and thus their genesis controversial.
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Paleomagnetic breccia tests on clasts at the three sites are negative, indicating that their Ch RM is post-depositional remagnetisation, and a paleomagnetic fold test is negative, indicating that the Ch RM is a remagnetisation, and a post-dates peak Alleghanian deformation.
The unit mean Ch RM direction for the: (a) limestones gives a paleopole at 129°E, 12°N (=3), indicating diagenesis formed a secondary chemical remanent magnetisation during the Late Ordovician–Early Silurian; (b) dolomitic limestones and dolostone host rocks gives a paleopole at 125.3°E, 31.9°N ().
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