Boni, M., & Bechstädt, T. (2000). Hydrothermal dolomites in SW Sardinia (Italy): Evidence for a widespread late-Variscan fluid flow event. Sedimentary geology, 131(3), . https://doi.org/10.1016/S0037-0738(99)00131-1
Chicago Style (17th ed.) CitationBoni, Maria, and Thilo Bechstädt. "Hydrothermal Dolomites in SW Sardinia (Italy): Evidence for a Widespread Late-Variscan Fluid Flow Event." Sedimentary Geology 131, no. 3 (2000). https://doi.org/10.1016/S0037-0738(99)00131-1.
MLA (9th ed.) CitationBoni, Maria, and Thilo Bechstädt. "Hydrothermal Dolomites in SW Sardinia (Italy): Evidence for a Widespread Late-Variscan Fluid Flow Event." Sedimentary Geology, vol. 131, no. 3, 2000, https://doi.org/10.1016/S0037-0738(99)00131-1.
Warning: These citations may not always be 100% accurate.