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   Some equipment is designed to measure the internal structures of cores and their physical properties, such as moisture content and seismic wave propagation velocities, without destruction.
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   Some equipment is used to investigate how the earth's magnetism has changed over time.
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   Some equipment is designed to measure isotope ratios to enable the study of rock formation periods and sediment deposition environments.

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   Some equipment is used to examine constituent elements and minerals.

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   Some equipment is used to isolate, measure and observe cells.

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