High resolution Sm-Nd garnet geochronology reveals the uneven pace of tectonometamorphic processes

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Scientific paper

Chemically zoned garnets provide a record of the changing conditions within the tectonically evolving crust where metamorphic mineral growth occurs. Recent advances in Sm-Nd geochronology of zoned garnets now permit the measurement of a higher resolution temporal record than previously attainable. Here, we present precise (< ± 0.7 million years) Sm-Nd ages from 12 concentric growth zones within a single large garnet from the Austrian Alps. Within a total growth span of 7.55 ± 0.52 (2 SD) million years, the data reveal two brief distinct pulses of accelerated growth (at least 5 times faster than the background growth rate). These pulses correlate with compositional features in the zoned garnet that are indicative of growth in the presence of abundant fluids or abrupt P-T changes. These data show that tectonometamorphic processes leading to garnet growth (such as exhumation, fluid flow, and/or heating) were pulse-like in nature, rather than slow and steady, during the waning stages of the Alpine orogeny 28-20 million years ago.

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