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⇱ Peng, J.-T., Hu, R.-Z., Burnard, P.G. (2003) Samarium–neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit (Hunan, China): the potential of calcite as a geochronometer. Chemical Geology, 200 (1) 129-136 doi:10.1016/s0009-2541(03)00187-6


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Peng, J.-T., Hu, R.-Z., Burnard, P.G. (2003) Samarium–neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit (Hunan, China): the potential of calcite as a geochronometer. Chemical Geology, 200 (1) 129-136 doi:10.1016/s0009-2541(03)00187-6

Reference TypeJournal (article/letter/editorial)
TitleSamarium–neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit (Hunan, China): the potential of calcite as a geochronometer
JournalChemical Geology
AuthorsPeng, J.-T.Author
Hu, R.-Z.Author
Burnard, P.G.Author
Year2003 (October)Volume200
Issue1
PublisherElsevier BV
DOIdoi:10.1016/s0009-2541(03)00187-6Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID293004Long-form Identifiermindat:1:5:293004:0
GUID0
Full ReferencePeng, J.-T., Hu, R.-Z., Burnard, P.G. (2003) Samarium–neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit (Hunan, China): the potential of calcite as a geochronometer. Chemical Geology, 200 (1) 129-136 doi:10.1016/s0009-2541(03)00187-6
Plain TextPeng, J.-T., Hu, R.-Z., Burnard, P.G. (2003) Samarium–neodymium isotope systematics of hydrothermal calcites from the Xikuangshan antimony deposit (Hunan, China): the potential of calcite as a geochronometer. Chemical Geology, 200 (1) 129-136 doi:10.1016/s0009-2541(03)00187-6
In(2003, October) Chemical Geology Vol. 200 (1) Elsevier BV


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