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ARGIN: 0cm 0cm 0pt; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-pagination: widow-orphan; mso-outline-level: 2" class=MsoNormal>ana; COLOR: black; FONT-SIZE: 10pt" lang=EN-US>A Comparative Analysis of Submarine Eruptive and Subaerial Eruptive Volcaniclsatic Reservoir on Characteristics of Reservoir and Reservoir Forming Dominated Factors: Taking Carboniferous Volcaniclsatic Reservoir in amespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ace w:st="on">aceName w:st="on">SantanghuaceName> aceType w:st="on">BasinaceType>ace> as an Exampleack; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>amespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />

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ARGIN: 0cm 0cm 0pt; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-pagination: widow-orphan; mso-outline-level: 2" class=MsoNormal>ana; COLOR: black; FONT-SIZE: 10pt" lang=EN-US>A Comparative Analysis of Submarine Eruptive and Subaerial Eruptive Volcaniclsatic Reservoir on Characteristics of Reservoir and Reservoir Forming Dominated Factors: Taking Carboniferous Volcaniclsatic Reservoir in amespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ace w:st="on">aceName w:st="on">SantanghuaceName> aceType w:st="on">BasinaceType>ace> as an Exampleack; FONT-SIZE: 12pt; mso-font-kerning: 18.0pt; mso-bidi-font-family: 宋体" lang=EN-US>amespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />

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