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ot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>ot;COLOR: black; 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" /><o:p>o:p>
ot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>ot;FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>Petroleum Geological Features of ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ceName w:st="on">UpperceName> ceName w:st="on">MagdalenaceName> ceType w:st="on">BasinceType> in country-region w:st="on">ce w:st="on">Colombiace>country-region>ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" /><o:p>o:p>
ot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>ot;FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>Conchostracan Biostratigraphy of the Dadianzi Formation in the ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ceName w:st="on">LuanpingceName> ceType w:st="on">BasinceType>, Northern ce w:st="on">ot;on">Hebei Province, country-region w:st="on">Chinacountry-region>ce> and the Boundary of Continental Jurassic and Cretaceous Strataml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" /><o:p>o:p>
ot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>ot;FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>Geology of Porphyry and Skarn Type Copper Polymetallic Deposits in the Southern Margin of ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ce w:st="on">ceName w:st="on">QaidamceName> ceType w:st="on">BasinceType>ce>ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" /><o:p>o:p>
ot;MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>ot;FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>Palynological Assemblage of Eocene-Oligocene Pollen and Their Biostratigraphic Correlation in Dahonggou, Daqaidam Area, ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ce w:st="on">ceName w:st="on">QaidamceName> ceType w:st="on">BasinceType>ce>ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" /><o:p>o:p>