APA (7th ed.) Citation

Clemens, J. D., & Stevens, G. (2026). Most ordinary granitic magmas are born as charnockites or become charnockites during magma ascent: Evidence for the prior existence of orthopyroxene and implications of high magma temperatures and inefficient crystal-melt separation. Mineralogy & Petrology, 120(2), 381. https://doi.org/10.1007/s00710-026-00990-0

Chicago Style (17th ed.) Citation

Clemens, John D., and Gary Stevens. "Most Ordinary Granitic Magmas Are Born as Charnockites or Become Charnockites During Magma Ascent: Evidence for the Prior Existence of Orthopyroxene and Implications of High Magma Temperatures and Inefficient Crystal-melt Separation." Mineralogy & Petrology 120, no. 2 (2026): 381. https://doi.org/10.1007/s00710-026-00990-0.

MLA (9th ed.) Citation

Clemens, John D., and Gary Stevens. "Most Ordinary Granitic Magmas Are Born as Charnockites or Become Charnockites During Magma Ascent: Evidence for the Prior Existence of Orthopyroxene and Implications of High Magma Temperatures and Inefficient Crystal-melt Separation." Mineralogy & Petrology, vol. 120, no. 2, 2026, p. 381, https://doi.org/10.1007/s00710-026-00990-0.