style="MARGIN: 0cm 0cm 0pt; mso-pagination: widow-orphan; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-outline-level: 2" class=MsoNormal>style="FONT-FAMILY: 宋体; COLOR: black; FONT-SIZE: 12pt; mso-bidi-font-family: 宋体; mso-font-kerning: 18.0pt" lang=EN-US>Exploration Prospects of Carboniferous Hydrocarbon in space prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on"><st1:PlaceName w:st="on">Barkolst1:PlaceName> <st1:PlaceType w:st="on">Basinst1:PlaceType>st1:place> of Xinjiangspace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
style="MARGIN: 0cm 0cm 0pt" class=MsoNormal>space prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:PlaceName w:st="on">style="FONT-SIZE: 14pt" lang=EN-US>Barkolst1:PlaceName>style="FONT-SIZE: 14pt" lang=EN-US> <st1:PlaceType w:st="on">Basinst1:PlaceType> is an interarc basin with small scale, which is located between <st1:PlaceName w:st="on">Karlikst1:PlaceName> <st1:PlaceType w:st="on">Mountainst1:PlaceType> and <st1:place w:st="on"><st1:PlaceName w:st="on">Maiqinwulast1:PlaceName> <st1:PlaceType w:st="on">Mountainst1:PlaceType>st1:place> in Barkol County of Xinjiang. It is a half graben-like basin and the structure is relatively single. The Carboniferous formations are developed in the basin. style="mso-spacerun: yes"> It is possible to be the favorable development area of weathered volcanic rock reservoir. The structure has Hercynian prototype and is further shaped in middle-late Yanshanian, forming the reservoir-cap combination of self-generation and self-storage. It is the favorable area in which the structure-lithology reservoirs are formed.space prefix = o ns = "urn:schemas-microsoft-com:office:office" />