Cite
Xenotime-hematite aggregates on opaline filaments: evidence for biomineralization in weathered siliciclastic rocks, Capanema, Quadrilátero Ferrífero of Minas Gerais, Brazil.
MLA
Cabral, Alexandre, et al. “Xenotime-Hematite Aggregates on Opaline Filaments: Evidence for Biomineralization in Weathered Siliciclastic Rocks, Capanema, Quadrilátero Ferrífero of Minas Gerais, Brazil.” International Journal of Earth Sciences, vol. 101, no. 1, Jan. 2012, pp. 377–83. EBSCOhost, https://doi.org/10.1007/s00531-011-0663-1.
APA
Cabral, A., Koglin, N., Seabra Gomes, A., & Lehmann, B. (2012). Xenotime-hematite aggregates on opaline filaments: evidence for biomineralization in weathered siliciclastic rocks, Capanema, Quadrilátero Ferrífero of Minas Gerais, Brazil. International Journal of Earth Sciences, 101(1), 377–383. https://doi.org/10.1007/s00531-011-0663-1
Chicago
Cabral, Alexandre, Nikola Koglin, Antônio Seabra Gomes, and Bernd Lehmann. 2012. “Xenotime-Hematite Aggregates on Opaline Filaments: Evidence for Biomineralization in Weathered Siliciclastic Rocks, Capanema, Quadrilátero Ferrífero of Minas Gerais, Brazil.” International Journal of Earth Sciences 101 (1): 377–83. doi:10.1007/s00531-011-0663-1.