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PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds

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Page 1: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 2: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 3: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 4: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 5: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 6: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 7: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 8: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 9: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 10: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 11: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 12: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 13: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 14: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 15: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 16: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 17: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 18: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 19: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 20: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 21: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 22: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 23: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 24: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 25: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 26: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds
Page 27: PowerPoint Presentation2. Temperature of lithosphere derived from half-space cooling model 3. Viscosity depends exponentially on temperature contrast of > 1015 viscosity bounds

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