First direct evidence of sedimentary carbonate recycling in subduction-related xenoliths

Carbon in rocks and its rate of exchange with the exosphere is the least understood part of the carbon cycle. The amount of carbonate subducted as sediments and ocean crust is poorly known, but essential to mass balance the cycle. We describe carbonatite melt pockets in mantle peridotite xenoliths f...

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Detalles Bibliográficos
Autores principales: Liu, Yongsheng, He, Detao, Gao, Changgui, Foley, Stephen, Gao, Shan, Hu, Zhaochu, Zong, Keqing, Chen, Haihong
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2015
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4477412/
https://www.ncbi.nlm.nih.gov/pubmed/26100577
http://dx.doi.org/10.1038/srep11547

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4477412/
https://www.ncbi.nlm.nih.gov/pubmed/26100577
http://dx.doi.org/10.1038/srep11547

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