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(2011) δ13C, δ18O and deposition rate of tufa in Xiangshui River, SW China: implications for land-cover change caused by climate and human impact during the late Holocene. Special Publication, 352. Geological Society of London. 85-96 doi:10.1144/sp352.7

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Titleδ13C, δ18O and deposition rate of tufa in Xiangshui River, SW China: implications for land-cover change caused by climate and human impact during the late Holocene
ReportSpecial Publication
Year2011Volume352
PublisherGeological Society of London
DOIdoi:10.1144/sp352.7Search in ResearchGate
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Mindat Ref. ID437640Long-form Identifiermindat:1:5:437640:2
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Full Reference(2011) δ13C, δ18O and deposition rate of tufa in Xiangshui River, SW China: implications for land-cover change caused by climate and human impact during the late Holocene. Special Publication, 352. Geological Society of London. 85-96 doi:10.1144/sp352.7
Plain Text(2011) δ13C, δ18O and deposition rate of tufa in Xiangshui River, SW China: implications for land-cover change caused by climate and human impact during the late Holocene. Special Publication, 352. Geological Society of London. 85-96 doi:10.1144/sp352.7
In(2011) Special Publication Vol. 352. Geological Society of London

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