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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>ack; FONT-SIZE: 12pt; mso-bidi-font-family: 宋体; mso-font-kerning: 18.0pt" lang=EN-US>Application of Electrical Logging in the Metallic ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ate w:st="on">ace w:st="on">Oreace>ate> Explorationml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
MARGIN: 0cm 0cm 0pt" class=MsoNormal>ack; FONT-SIZE: 14pt" lang=EN-US>ace="Times New Roman">The Distribution of Cenozoic Intrusive Rocks in the Northern ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ace w:st="on">aceName w:st="on">JiangsuaceName> aceType w:st="on">BasinaceType>ace> and Its Geological Significancesml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
MARGIN: 0cm 0cm 0pt" class=MsoNormal>ack; FONT-SIZE: 14pt" lang=EN-US>ace="Times New Roman">Study on the Characters of the Accommodation Change and Hydrocarbon in Upper Xujiahe Formation in the ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ace w:st="on">aceName w:st="on">WesternaceName> aceName w:st="on">SichuanaceName> aceType w:st="on">BasinaceType>ace>ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
MARGIN: 0cm 0cm 0pt; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-pagination: widow-orphan; mso-outline-level: 2" class=MsoNormal>ack; FONT-SIZE: 12pt; mso-bidi-font-family: 宋体; mso-font-kerning: 18.0pt" lang=EN-US>Formation Environment of Triassic Evaporate ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />aceName w:st="on">RockaceName> aceType w:st="on">BasinaceType> and Dolostone Reservoirs in the ace w:st="on">aceName w:st="on">SichuanaceName> aceType w:st="on">BasinaceType>ace>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>ack; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>Late Quaternary Pollen Records and Climate Significance in ml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ace w:st="on">aceName w:st="on">GuangzhouaceName> aceType w:st="on">ProvinceaceType>ace>ml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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