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ARGIN: 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>The Mechanism of Secondary Porosity in Oligocene Reservoir in Southern amespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ace w:st="on">Shwebo Basin, Myanmarace>amespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
ARGIN: 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>Reservoir Types and Secondary Pore Evolution of Lower Cretaceous in Tanzhuang Sag of the Southern amespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ace w:st="on">aceName w:st="on">NorthaceName> aceName w:st="on">ChinaaceName> aceType w:st="on">BasinaceType>ace>amespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />