Jones, Timothy D., Maguire, Ross R., van Keken, Peter E., Ritsema, Jeroen, and Koelemeijer, Paula. Subducted oceanic crust as the origin of seismically slow lower-mantle structures. Retrieved from https://par.nsf.gov/biblio/10206646. Progress in Earth and Planetary Science 7.1 Web. doi:10.1186/s40645-020-00327-1.

Jones, Timothy D., Maguire, Ross R., van Keken, Peter E., Ritsema, Jeroen, & Koelemeijer, Paula. Subducted oceanic crust as the origin of seismically slow lower-mantle structures. Progress in Earth and Planetary Science, 7 (1). Retrieved from https://par.nsf.gov/biblio/10206646. https://doi.org/10.1186/s40645-020-00327-1

Jones, Timothy D., Maguire, Ross R., van Keken, Peter E., Ritsema, Jeroen, and Koelemeijer, Paula. "Subducted oceanic crust as the origin of seismically slow lower-mantle structures". Progress in Earth and Planetary Science 7 (1). Country unknown/Code not available. https://doi.org/10.1186/s40645-020-00327-1. https://par.nsf.gov/biblio/10206646.

@article{osti_10206646,
place = {Country unknown/Code not available}, title = {Subducted oceanic crust as the origin of seismically slow lower-mantle structures}, url = {https://par.nsf.gov/biblio/10206646}, DOI = {10.1186/s40645-020-00327-1}, abstractNote = {}, journal = {Progress in Earth and Planetary Science}, volume = {7}, number = {1}, author = {Jones, Timothy D. and Maguire, Ross R. and van Keken, Peter E. and Ritsema, Jeroen and Koelemeijer, Paula}, editor = {null} }