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MARGIN: 0cm 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: 14pt; mso-font-kerning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>ce="Times New Roman">The Discovery of the Mafic-Ultramafic Melange in Kekesha Area of ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ceName w:st="on">DulanceName> ceType w:st="on">CountyceType>, ce w:st="on">East Kunlunce> Region, and Its LA-ICP-MS Zircon U-Pb Ageml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
MARGIN: 0cm 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: 14pt; mso-font-kerning: 18.0pt" lang=EN-US>ce="Times New Roman">Application of Remote Sensing Technique in the Mapping of Cenozoic Geology of the ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ce w:st="on">ceName w:st="on">EastceName> ceName w:st="on">KunlunceName> ceType w:st="on">MountainsceType>ce>ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
MARGIN: 0cm 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>The Composition Comparison of Neoarchaeozoic to Paleoproterozoic Volcanic Rocks and Meta-Pelitic Rocks and Their Geological Significance in Altyn and ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ce w:st="on">East Kunlunce>ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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