style="MARGIN: 0cm 0cm 0pt; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-pagination: widow-orphan; 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>Diagenesis and Diagenetic Environments of the Carbonate Rocks from the Middle Jurassic Buqu Formation in the Eastern space prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on"><st1:PlaceName w:st="on">Qiangtangst1:PlaceName> <st1:PlaceType w:st="on">Basinst1:PlaceType>st1:place> on the Qinghai-Tibetan Plateauspace prefix = o ns = "urn:schemas-microsoft-com:office:office" />
- 责任者：Ma Boyong (School of Geosciences and Resources ; China University of Geosciences ; Beijing 100083 ; China) ; Wang Genhou
- 刊名：Sedimentary Geology and Tethyan Geology
- 出版年：2010
- 卷期：30(2)
- 关键词：碳酸盐岩 ; carbonate rocks ; 成岩作用 ; diagenesis ; 羌塘盆地 ; Qiangtang Basin
- 页码：p.11-18
- 图表：3 illus., 1 plate, 18 refs.
- 分类号：0803
- issnNo：ISSN1009-3850
- isbnNo：CN51-1593/P
style="MARGIN: 0cm 0cm 0pt" class=MsoNormal>style="FONT-SIZE: 14pt" lang=EN-US>The diagenesis types of the carbonate rocks from the Middle Jurassic Buqu Formation in the eastern space prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on"><st1:PlaceName w:st="on">Qiangtangst1:PlaceName> <st1:PlaceType w:st="on">Basinst1:PlaceType>st1:place> on the Qinghai-Tibetan Plateau consist of micritization, cementation, compaction-pressure solution, fragmentation and dissolution, of which fragmentation, dissolution and micritization are more common than the others. The results of research in this paper show that the eastern <st1:place w:st="on"><st1:PlaceName w:st="on">Qiangtangst1:PlaceName> <st1:PlaceType w:st="on">Basinst1:PlaceType>st1:place> should be selected as the key prospective area for oil exploration.space prefix = o ns = "urn:schemas-microsoft-com:office:office" />