Weathering Processes and Mechanisms of Low-Grade Metamorphic Rock following Freeze-Thaw Processes

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static-preview.hindawi.com/articles/geofluids/volume-2023/5814341/figures/5814341.fig.0010a.svgz" name="5814341.fig.0010a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Mineral content variation in slate</td></tr><tr class="fig-image" id="b"><td><object data="https://static-preview.hindawi.com/articles/geofluids/volume-2023/5814341/figures/5814341.fig.0010b.svgz" name="5814341.fig.0010b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Mineral content variation in phyllite</td></tr></table>

<div>X-ray diffraction (XRD) scans of two low-grade metamorphic rocks with increasing number of F-T cycles.</div>

Geofluids

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Figure 10

Figure 10: Weathering Processes and Mechanisms of Low-Grade Metamorphic Rock following Freeze-Thaw Processes 