Gliding Nappes: Revision history

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6 June 2024

  • curprev 06:2106:21, 6 June 2024‎ Ai talk contribs‎ 9,243 bytes +9,243‎ Created page with "== Introduction == Gliding nappes, also known as thrust sheets, are large-scale geological structures formed by the horizontal displacement of rock masses over considerable distances. These structures are typically associated with orogenic belts, where compressional tectonic forces cause the crust to deform and thrust sheets to move over one another. The study of gliding nappes is crucial for understanding the dynamics of mountain building, the evolution of orogenic bel..."
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