detrital remanent magnetization
Quick Summary
Detrital remanent magnetization (DRM) is a type of permanent magnetism found in rocks. It occurs when small magnetic mineral grains settle into a sedimentary matrix. It is hypothesized that these tiny grains align themselves with the Earth's magnetic field during deposition, before the rock is fully consolidated. This acquired magnetism is thought to persist even as the rock is altered and compacted later. DRM is a specific form of depositional remanent magnetization (DRM), which is acquired by clastic sediments as fine particles settle in water bodies. The Earth's magnetic field influences the orientation of these grains, creating a preferred direction of magnetization.12
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