Source composition - PowerPoint PPT Presentation

Silicate Earth

Silicate Earth. Primitive mantle Present-day mantle Crust Oceanic crust Continental crust. Reservoir Volume Mass Mass % (10 27 cm 3 ) (10 27 g) Earth 1.083 5.98 100 Core 0.175 1.88 31.5 Mantle 0.899 4.08 68.1 Crust (continental) 0.00842 0.0236 0.4

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Asymmetry Dependence of the Nuclear Caloric Curve

Asymmetry Dependence of the Nuclear Caloric Curve. Nuclear Caloric Curve: Background &amp; Motivation The Measurement: Reconstructing Highly Excited Nuclei &amp; Extracting Their Temperatures Result: Temperature Decreases Linearly with Increasing Asymmetry.

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