Crustal recycling
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- Subducted Oceanic Crust As the Origin of Seismically Slow Lower-Mantle Structures Timothyd.Jones1*, Ross R
- Subduction Erosion: Rates, Mechanisms, and Its Role in Arc Magmatism and the Evolution of the Continental Crust and Mantle
- Rapid Crustal Growth and Efficient Crustal Recycling in the Early Earth
- 10. the Nitrogen Record of Crust-Mantle Interaction and Mantle
- Mantle Updrafts and Mechanisms of Oceanic Volcanism
- Constraints on Continental Crustal Mass Loss Via Chemical Weathering
- The 2.69 GA Paringa Basalts: Crustal Recycling Into the Asthenosphere Source
- Magmatic Evolution and Crustal Recycling for Neoproterozoic Strongly Peraluminous Granitoids from Southern China: Hf and O Isotopes in Zircon
- Crustal Recycling, Mantle Dehydration, and the Thermal Evolution of Mars A
- Becker, T. W., & Advance Our Understanding of Deep Mantle Reservoir Distributions, and We Discuss How Continental and Steinberger, B
- Stable Isotope Evidence for Crustal Recycling As Recorded by Superdeep Diamonds A.D
- Intraplate Volcanism: Conc Continuing the Discussion of Mantle Plumes in the Previous Two Issues, Alan D Smith Looks at Mantle Models
- 4.12 Physics and Chemistry of Deep Continental Crust Recycling C-TA Lee, Rice University, Houston, TX, USA
- Conservation and Redistribution of Crust During the Indoasian Collision
- Delamination and Recycling of Archaean Crust Caused by Gravitational Instabilities
- Crustal Evolution and Mantle Dynamics Through Earth History
- Rapid Endogenic Rock Recycling in Magmatic Arcs ✉ Jun-Yong Li1,2, Ming Tang2,3, Cin-Ty A
- Chemical Heterogeneity in the Hawaiian Mantle Plume from the Alteration and Dehydration of Recycled Oceanic Crust