D. Biltekin, "The mineralogical and geochemical composition of Holocene sediments from Lake Hazar, Elazığ, Eastern Turkey: implications for weathering, paleoclimate, redox conditions, provenance, and tectonic setting ," Turkish Journal Of Earth Sciences , vol.28, no.5, pp.760-785, 2019
Biltekin, D. 2019. The mineralogical and geochemical composition of Holocene sediments from Lake Hazar, Elazığ, Eastern Turkey: implications for weathering, paleoclimate, redox conditions, provenance, and tectonic setting . Turkish Journal Of Earth Sciences , vol.28, no.5 , 760-785.
Biltekin, D., (2019). The mineralogical and geochemical composition of Holocene sediments from Lake Hazar, Elazığ, Eastern Turkey: implications for weathering, paleoclimate, redox conditions, provenance, and tectonic setting . Turkish Journal Of Earth Sciences , vol.28, no.5, 760-785.
Biltekin, Demet. "The mineralogical and geochemical composition of Holocene sediments from Lake Hazar, Elazığ, Eastern Turkey: implications for weathering, paleoclimate, redox conditions, provenance, and tectonic setting ," Turkish Journal Of Earth Sciences , vol.28, no.5, 760-785, 2019
Biltekin, Demet. "The mineralogical and geochemical composition of Holocene sediments from Lake Hazar, Elazığ, Eastern Turkey: implications for weathering, paleoclimate, redox conditions, provenance, and tectonic setting ." Turkish Journal Of Earth Sciences , vol.28, no.5, pp.760-785, 2019
Biltekin, D. (2019) . "The mineralogical and geochemical composition of Holocene sediments from Lake Hazar, Elazığ, Eastern Turkey: implications for weathering, paleoclimate, redox conditions, provenance, and tectonic setting ." Turkish Journal Of Earth Sciences , vol.28, no.5, pp.760-785.
@article{article, author={Demet Biltekin}, title={The mineralogical and geochemical composition of Holocene sediments from Lake Hazar, Elazığ, Eastern Turkey: implications for weathering, paleoclimate, redox conditions, provenance, and tectonic setting }, journal={Turkish Journal Of Earth Sciences}, year=2019, pages={760-785} }