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2.<P style="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>mes New Roman">Immiscibility during Mineralization of Yinan Au-Cu-Fe Deposit, ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />place w:st="on">me w:st="on">Shandongme> pe w:st="on">Provincepe>place>: Evidence from Fluid Inclusions and H-O Isotopesml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />p>p>
3.<P style="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>mes New Roman">Immiscibility during Mineralization of Yinan Au-Cu-Fe Deposit, ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />place w:st="on">me w:st="on">Shandongme> pe w:st="on">Provincepe>place>: Evidence from Fluid Inclusions and H-O Isotopesml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />p>p>
4.<P 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>pt; 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" />place w:st="on">me w:st="on">Chongmingme> pe w:st="on">Islandpe>place>ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />p>p>
5.<P 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>pt; 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" />place w:st="on">me w:st="on">Chongmingme> pe w:st="on">Islandpe>place>ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />p>p>
6.<P style="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>mes New Roman">pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>40pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>Ar-39Ar dating and Geochemical Characteristics of the Potassic Lamprophyre in ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />place w:st="on">Linxiang Area, Northeastern Hunanplace> Provinceml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />p>p>
7.<P style="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>mes New Roman">pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>40pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>Ar-39Ar dating and Geochemical Characteristics of the Potassic Lamprophyre in ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />place w:st="on">Linxiang Area, Northeastern Hunanplace> Provinceml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />p>p>
8.<P style="MARGIN: 0cm 0cm 0pt" class=MsoNormal>mes New Roman">pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>The Sediment Flux of the ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />place w:st="on">me w:st="on">Longmenme> me w:st="on">Shanme> me w:st="on">Forelandme> pe w:st="on">Basinpe>place> d; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>duringpt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US> the Late Triassic Epoch and the Uplift and Denudation of the Orogenic Beltpt" lang=EN-US>ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />p>p>
9.<P style="MARGIN: 0cm 0cm 0pt" class=MsoNormal>mes New Roman">pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>The Sediment Flux of the ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />place w:st="on">me w:st="on">Longmenme> me w:st="on">Shanme> me w:st="on">Forelandme> pe w:st="on">Basinpe>place> d; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>duringpt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US> the Late Triassic Epoch and the Uplift and Denudation of the Orogenic Beltpt" lang=EN-US>ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />p>p>
10.<P style="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>New Isoxys (Arthropoda) from the Cambrian Mantou Formation, ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />place w:st="on">me w:st="on">Shandongme> pe w:st="on">Provincepe>place>ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />p>p>
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