style="MARGIN: 0cm 0cm 0pt; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-pagination: widow-orphan; mso-outline-level: 2" class=MsoNormal>style="FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-bidi-font-family: 宋体; mso-font-kerning: 18.0pt" lang=EN-US>Hf Isotopic Compositions of Zircons from 2.7 Ga Metasedimentary Rocks and Biotite-Plagioclase Gneiss in the Mengjiatun Formation Complex, ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on"><st1:PlaceName w:st="on">Westernst1:PlaceName> <st1:PlaceName w:st="on">Shandongst1:PlaceName> <st1:PlaceType w:st="on">Provincest1:PlaceType>st1:place>ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />

style="MARGIN: 0cm 0cm 0pt; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-pagination: widow-orphan; mso-outline-level: 2" class=MsoNormal>style="FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-bidi-font-family: 宋体; mso-font-kerning: 18.0pt" lang=EN-US>Hf Isotopic Compositions of Zircons from 2.7 Ga Metasedimentary Rocks and Biotite-Plagioclase Gneiss in the Mengjiatun Formation Complex, ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on"><st1:PlaceName w:st="on">Westernst1:PlaceName> <st1:PlaceName w:st="on">Shandongst1:PlaceName> <st1:PlaceType w:st="on">Provincest1:PlaceType>st1:place>ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />

style="MARGIN: 0cm 0cm 0pt; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-pagination: widow-orphan; mso-outline-level: 2" class=MsoNormal>style="FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-bidi-font-family: 宋体; mso-font-kerning: 18.0pt" lang=EN-US>Application of Radioisotope Geochronology in Study on Sedimentation Rate of Tidal Flat of ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on"><st1:PlaceName w:st="on">Chongmingst1:PlaceName> <st1:PlaceType w:st="on">Islandst1:PlaceType>st1:place>ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />

style="MARGIN: 0cm 0cm 0pt; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-pagination: widow-orphan; mso-outline-level: 2" class=MsoNormal>style="FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-bidi-font-family: 宋体; mso-font-kerning: 18.0pt" lang=EN-US>Application of Radioisotope Geochronology in Study on Sedimentation Rate of Tidal Flat of ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on"><st1:PlaceName w:st="on">Chongmingst1:PlaceName> <st1:PlaceType w:st="on">Islandst1:PlaceType>st1:place>ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />