https://w3id.org/np/RAmQmmhT8YeV7NqkR66tugyDItXnhHRRXjNByTSXQwvOo
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dc:description "The principle of original horizontality can be tested both via paleomagnetic fold tests (which test whether tilting occurred post-deposition) and via modern sedimentological surveys of depositional slope angles. Public paleomagnetic databases (e.g., MagIC) and marine seismic/bathymetric archives allow testing this, though well-known exceptions like cross-beds and clinoforms mean the strict universal phrasing only holds for basin-floor suspension deposits.";
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