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style="MARGIN: auto 0cm">style="FONT-FAMILY: ’Times New 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 ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:State w:st="on">Zhejiangst1:State> and <st1:PlaceName w:st="on">Fujianst1:PlaceName> <st1:PlaceType w:st="on">Provincesst1:PlaceType>: Implications for the Neoproterozoic Tectonic Setting of <st1:place w:st="on">Northeastern Yangtzest1:place> Blockml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />

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style="MARGIN: auto 0cm">style="FONT-FAMILY: ’Times New 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 ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:State w:st="on">Zhejiangst1:State> and <st1:PlaceName w:st="on">Fujianst1:PlaceName> <st1:PlaceType w:st="on">Provincesst1:PlaceType>: Implications for the Neoproterozoic Tectonic Setting of <st1:place w:st="on">Northeastern Yangtzest1:place> Blockml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />

4.<SPAN style="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>mes New Roman">Quantitative Evaluation of Fracture Distribution in the Down Strike-Slip Fault Zone of Upper Shuaiba Member of Lower Cretaceous, ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on"><st1:City w:st="on">Daleelst1:City>, <st1:country-region w:st="on">Omanst1:country-region>st1:place> ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
5.<SPAN style="COLOR: black; FONT-SIZE: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>mes New Roman">Quantitative Evaluation of Fracture Distribution in the Down Strike-Slip Fault Zone of Upper Shuaiba Member of Lower Cretaceous, ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on"><st1:City w:st="on">Daleelst1:City>, <st1:country-region w:st="on">Omanst1:country-region>st1:place> ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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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>style="FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>On Prof. Leestyle="FONT-FAMILY: 宋体; COLOR: black; 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 Provinceml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />

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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>style="FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>On Prof. Leestyle="FONT-FAMILY: 宋体; COLOR: black; 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 Provinceml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />

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