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N: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>na; COLOR: black; FONT-SIZE: 10pt" lang=EN-US>Paleoclimatic Significance of Oxygen Isotope Composition of Carbonates from a Sediment Core at namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />n">Bosten n">Lake, n">n">Xinjiang, ntry-region w:st="on">Chinantry-region>nt-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
N: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>nt-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>Distributing Characteristics of Heavy Metal Elements in the Sediment Profiles of namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />n">Bijiang n">River, Western Yunnan, ntry-region w:st="on">n">Chinantry-region>namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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