Wu, Sin-Mei, Huang, Hsin-Hua, Lin, Fan-Chi, Farrell, Jamie, and Schmandt, Brandon. Extreme seismic anisotropy indicates shallow accumulation of magmatic sills beneath Yellowstone caldera. Retrieved from https://par.nsf.gov/biblio/10462668. Earth and Planetary Science Letters 616.C Web. doi:10.1016/j.epsl.2023.118244.

Wu, Sin-Mei, Huang, Hsin-Hua, Lin, Fan-Chi, Farrell, Jamie, & Schmandt, Brandon. Extreme seismic anisotropy indicates shallow accumulation of magmatic sills beneath Yellowstone caldera. Earth and Planetary Science Letters, 616 (C). Retrieved from https://par.nsf.gov/biblio/10462668. https://doi.org/10.1016/j.epsl.2023.118244

Wu, Sin-Mei, Huang, Hsin-Hua, Lin, Fan-Chi, Farrell, Jamie, and Schmandt, Brandon. "Extreme seismic anisotropy indicates shallow accumulation of magmatic sills beneath Yellowstone caldera". Earth and Planetary Science Letters 616 (C). Country unknown/Code not available. https://doi.org/10.1016/j.epsl.2023.118244. https://par.nsf.gov/biblio/10462668.

@article{osti_10462668,
place = {Country unknown/Code not available}, title = {Extreme seismic anisotropy indicates shallow accumulation of magmatic sills beneath Yellowstone caldera}, url = {https://par.nsf.gov/biblio/10462668}, DOI = {10.1016/j.epsl.2023.118244}, abstractNote = {}, journal = {Earth and Planetary Science Letters}, volume = {616}, number = {C}, author = {Wu, Sin-Mei and Huang, Hsin-Hua and Lin, Fan-Chi and Farrell, Jamie and Schmandt, Brandon}, }