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  "path": "/editor-highlights/long-term-and-recent-activity-of-the-brenner-fault-finally-reconciled",
  "publishedAt": "2026-03-19T18:25:13.000Z",
  "site": "https://eos.org",
  "tags": [
    "Editors' Highlights",
    "Alps",
    "Earth science",
    "faults",
    "Geochemistry, Geophysics, Geosystems",
    "seismology",
    "Argante et al. [2026]"
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  "textContent": "Polarized-light microscope images of thin sections (thin rock slices) from calc-schists collected at increasing distance from the main Brenner Fault (footwall). Deformation is cataclastic (brittle) near the fault and mylonitic (ductile) about 2 kilometers away. Near the fault, cataclasis overprints earlier mylonitic fabrics, producing hybrid deformation. Foliation is visible in all samples. Credit:  Argante et al. [2026], Figure 4",
  "title": "Long-Term and Recent Activity of the Brenner Fault Finally Reconciled"
}