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e="TEXT-INDENT: -7pt; MARGIN: 0cm 0cm 0pt 7pt; mso-char-indent-count: -.5" class=MsoNormal>e="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>e="Times New Roman">The Upper Age Limitation of Mesozoic Lithospheric Thinning in NE Chinae="FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold; mso-hansi-font-family: ’Times New Roman’; mso-ascii-font-family: ’Times New Roman’">：e="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>e="Times New Roman">Chronology Restriction of Yingcheng Formation in espace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />e w:st="on">eName w:st="on">SongliaoeName> eType w:st="on">BasineType>e>espace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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e="TEXT-INDENT: -7pt; MARGIN: 0cm 0cm 0pt 7pt; mso-char-indent-count: -.5" class=MsoNormal>e="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>e="Times New Roman">The Upper Age Limitation of Mesozoic Lithospheric Thinning in NE Chinae="FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold; mso-hansi-font-family: ’Times New Roman’; mso-ascii-font-family: ’Times New Roman’">：e="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 0pt; mso-bidi-font-weight: bold" lang=EN-US>e="Times New Roman">Chronology Restriction of Yingcheng Formation in espace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />e w:st="on">eName w:st="on">SongliaoeName> eType w:st="on">BasineType>e>espace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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e="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>e="Times New Roman">The Distribution and Characteristics of Lacustrine Sedimentation from espace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />eName w:st="on">AncienteName> eName w:st="on">HigheName> eName w:st="on">LeveleName> eType w:st="on">LakeeType> at the North Foot ofe w:st="on">  Bayankala Mt., e>e="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>e="Times New Roman">e w:st="on">e w:st="on">Qinghai Provincee>, egion w:st="on">Chinaegion>e> espace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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e="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>e="Times New Roman">The Distribution and Characteristics of Lacustrine Sedimentation from espace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />eName w:st="on">AncienteName> eName w:st="on">HigheName> eName w:st="on">LeveleName> eType w:st="on">LakeeType> at the North Foot ofe w:st="on">  Bayankala Mt., e>e="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>e="Times New Roman">e w:st="on">e w:st="on">Qinghai Provincee>, egion w:st="on">Chinaegion>e> espace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
7.e="Times New Roman">e="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>Paleoenviromental and Paleoclimatic Changes inespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />e w:st="on"> eName w:st="on">Xingkai e w:st="on">eType w:st="on">LakeeType>e>eName>e> Inferred from Stable Carbon and Nitrogen Isotopes of Bulk Organic Matter since e="COLOR: red; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>28 ka B.P.e="COLOR: red; FONT-SIZE: 14pt" lang=EN-US>espace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
8.e="Times New Roman">e="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>Paleoenviromental and Paleoclimatic Changes inespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />e w:st="on"> eName w:st="on">Xingkai e w:st="on">eType w:st="on">LakeeType>e>eName>e> Inferred from Stable Carbon and Nitrogen Isotopes of Bulk Organic Matter since e="COLOR: red; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>28 ka B.P.e="COLOR: red; FONT-SIZE: 14pt" lang=EN-US>espace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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e="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>e="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>e="Times New Roman">Oligocene Lacustrine Stromatolites in the espace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />e w:st="on">eName w:st="on">TuotuoheeName> eType w:st="on">BasineType>e>, Qinghai-Tibetan Plateau: Paleoclimate Conditions Recorded by the Rhythmic Laminationsespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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e="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>e="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>e="Times New Roman">Oligocene Lacustrine Stromatolites in the espace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />e w:st="on">eName w:st="on">TuotuoheeName> eType w:st="on">BasineType>e>, Qinghai-Tibetan Plateau: Paleoclimate Conditions Recorded by the Rhythmic Laminationsespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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