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cm">w Roman’; FONT-SIZE: 14pt; FONT-WEIGHT: normal; mso-bidi-font-weight: bold" lang=EN-US>Comparison of Protolith Assemblages of Metamorphic Rocks in the Dabie-Sulu Orogen and the Late Mesozoic Magmatic Rock Associations in the Coastal Region of ce prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />w:st="on">Zhejiang and ceName w:st="on">FujianceName> ceType w:st="on">ProvincesceType>: Implications for the Neoproterozoic Tectonic Setting of ce w:st="on">Northeastern Yangtzece> Blockce prefix = o ns = "urn:schemas-microsoft-com:office:office" />

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cm">w Roman’; FONT-SIZE: 14pt; FONT-WEIGHT: normal; mso-bidi-font-weight: bold" lang=EN-US>Comparison of Protolith Assemblages of Metamorphic Rocks in the Dabie-Sulu Orogen and the Late Mesozoic Magmatic Rock Associations in the Coastal Region of ce prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />w:st="on">Zhejiang and ceName w:st="on">FujianceName> ceType w:st="on">ProvincesceType>: Implications for the Neoproterozoic Tectonic Setting of ce w:st="on">Northeastern Yangtzece> Blockce prefix = o ns = "urn:schemas-microsoft-com:office:office" />

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cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>ck; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>On Prof. Leeck; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体">’s Having Misread Debris Flow Deposits as Quaternary Glaciations in the Lushan Area, Jiangxi Provincece prefix = o ns = "urn:schemas-microsoft-com:office:office" />

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cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>ck; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>On Prof. Leeck; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体">’s Having Misread Debris Flow Deposits as Quaternary Glaciations in the Lushan Area, Jiangxi Provincece prefix = o ns = "urn:schemas-microsoft-com:office:office" />

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