Publication Date:
2019
Description:
〈span〉〈div〉Abstract〈/div〉The Outer Hebridean islands of Scotland host a ∼200 km long fault zone that was active between 1100 and 250 Ma, during which a belt of fault rock several kilometres wide was created. The fault zone hosts crush breccias, phyllonite, mylonite and pseudotachylyte. The latter unit is frequently found in major fault zones and within meteorite impact structures. Although pseudotachylyte is widely believed to be a product of frictional melting within the fault zone, there is still controversy over the specific formational mechanisms. For this study pseudotachylyte was collected from the southern block of the Outer Hebrides Fault Zone. A recently developed geochemical mixing model was applied to reconstruct the geochemistry of the pseudotachylyte matrix using locally available lithologies. The results demonstrate that pseudotachylyte could be derived from local country rock, though some mixing was necessary to provide accurate reconstructions, suggesting a degree of mixing between melts derived from different protoliths. Petrographic observations identified additional characteristics of melt transportation, including transported clasts, aligned fragments, melt segregation, and injection of melt into tensile fractures. The latter likely served as the transport mechanism, drawing melt into low pressure, tensile structures that developed adjacent to the melt forming zones within the fault plane.〈strong〉Supplementary material:〈/strong〉〈a href="https://doi.org/10.6084/m9.figshare.c.4567931"〉https://doi.org/10.6084/m9.figshare.c.4567931〈/a〉〈/span〉
Print ISSN:
0370-291X
Topics:
Geosciences
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