Experimental constraints on the fate of subducted upper continental crust beyond the “depth of no return”

详细信息    查看全文

• 作者：Yanfei Zhang^a ; ^b ; ^{yanfzhang@cug.edu.cn" class="auth_mail" title="E-mail the corresponding author} ; Yao Wu^a ; Chao Wang^a ; Lü ; yun Zhu^a ; Zhenmin Jin^a ; ^b
• 关键词：Upper continental crust ; Depth of no return ; Partial melting ; Geochemical heterogeneity ; Second continent
• 刊名：Geochimica et Cosmochimica Acta
• 出版年：2016
• 出版时间：1 August 2016
• 年：2016
• 卷：186
• 期：Complete
• 页码：207-225
• 全文大小：1629 K

文摘

The subducted continental crust material will be gravitationally trapped in the deep mantle after having been transported to depths of greater than ∼250–300 km (the “depth of no return”). However, little is known about the status of this trapped continental material as well as its contribution to the mantle heterogeneity after achieving thermal equilibrium with the surrounding mantle. Here, we conduct an experimental study over pressure and temperature ranges of 9–16 GPa and 1300–1800 °C to constrain the fate of these trapped upper continental crust (UCC). The experimental results show that partial melting will occur in the subducted UCC along normal mantle geotherm to produce K-rich melt. The residual phases composed of coesite/stishovite + clinopyroxene + kyanite in the upper mantle, and stishovite + clinopyroxene + K-hollandite + garnet + CAS-phase in the mantle transition zone (MTZ), respectively. The residual phases achieve densities greater than the surrounding mantle, which provides a driving force for descent across the 410-km seismic discontinuity into the MTZ. However, this density relationship is reversed at the base of the MTZ, leaving the descended residues to be accumulated above the 660-km seismic discontinuity and may contribute to the “second continent”. The melt is ∼0.6–0.7 g/cm³ less dense than the surrounding mantle, which provides a buoyancy force for ascent of melt to shallow depths. The ascending melt, which preserves a significant portion of the bulk-rock rare earth elements (REEs), large ion lithophile elements (LILEs), and high-filed strength elements (HFSEs), may react with the surrounding mantle. Re-melting of the metasomatized mantle may contribute to the origin of the “enriched mantle sources” (EM-sources). Therefore, the deep subducted continental crust may create geochemical/geophysical heterogeneity in Earth’s interior through subduction, stagnation, partial melting and melt segregation.