Apatite low-temperature chronometry and microstructures across a hydrothermally active fault zone
نویسندگان
چکیده
Low-temperature chronometers offer potential to gain insights into the temporal evolution of hydrothermal systems. The long-lived fault-bound Grimsel pass system (including a fossil and an active part) in Central European Alps serves here as key site test such application. Zircon apatite grains were separated from samples collected along fault transect. resulting zircon (U-Th)/He ages are homogenous profile at 8–9 Ma thus record regional cooling evolution, remaining unaffected by younger activity. In contrast, show three age groups: One Group (1) ca. 5 inside outside zone matches low-temperature part trend, while group (2) with young 1–2 occurs central narrow associated sample (group 3) displays older apparent compared trend. reveal different cathodoluminescence texture trace-element chemistry, which we interpret together growth or re-crystallization within system. Forward 1D modelling He diffusion indicates that should always be reset when exposed hot thermal waters (up ~140 °C) present over ka timescales intermediate temperature (~90 timescales. Combining our measured forward results highlight that, besides trends, local heat anomalies zones very variable space time. Combined geochemistry dating shows occurrence newly-formed apatites crystals, best described geochronometers rather than thermochronometers. Such information is important explore longevity systems spatial distributions anomalies.
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ژورنال
عنوان ژورنال: Chemical Geology
سال: 2022
ISSN: ['0009-2541', '1872-6836']
DOI: https://doi.org/10.1016/j.chemgeo.2021.120633