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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>ce="Times New Roman">ck; mso-font-kerning: 18.0pt" lang=EN-US>40ck; mso-font-kerning: 18.0pt" lang=EN-US>Ar/39Ar Isotopic Dating of the Glaucophane in Caiduo Caka, Central Qiangtang Area, Northern Tibet, China and Its Geological Significanceck; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>ce prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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>Hydrocarbon Geochemical Fields and Anomalies Regions in the ce prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ce w:st="on">ceName w:st="on">NorthceName> ceName w:st="on">Yellow SeaceName> ceType w:st="on">BasinceType>ce>ce prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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>The Climate Change during 128.11-119.05 Ma Recorded by the Susceptibility of the Sediments of Liupanshan Groupce prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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>Application of Slope Break Controlled Deposition Theory in Oil & Gas Exploration in ce prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ce w:st="on">Bongor Basin, country-region w:st="on">Chadcountry-region>ce>ce prefix = o ns = "urn:schemas-microsoft-com:office:office" />
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