Petrological Recording of Mantle-Magmatic COB>2 Leakage on a Large-Scale in Honggang Anticline, Southern ce prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />ce w:st="on">ceName w:st="on">Songliao ceName> ceType w:st="on">Basin ceType> ce>
详细信息
- 责任者：Liu Li (College of Earth Sciences ; Jilin University ; Changchun 130061 ; China) ; Liu Na
- 刊名：Journal of Jilin University
- 出版年：2011
- 卷期：41(2)
- 关键词：二氧化碳 ; carbon dioxide ; 成藏模式 ; pool-formed model ; 松辽平原 ; Songliao Plain
- 页码：p.411-420
- 图表：6 illus., 1 plate, 2 tables, 35 refs.
- 分类号：1003
- issnNo：ISSN1671-5888
- isbnNo：CN22-1343/P
摘要
ChDivSummary name="EnDivSummary">The petrological records of mantle-magmatic COB>2 leakage, which occurred in Honggang anticline, southern Songliao basin, can be revealed by studing on spatial distribution and the occurrence of dawsonite cements and also the characteristics of fluid inclusions in dawsonite-bearing sandstones. In Honggang anticline, dawsonite is widespread in Qingshankou Formation, in Quangtou Formation and Yaojia Formation come second. Most of the dawsonite-bearing sandstones do not contain CO2, while some of the dawsonite-bearing layers contain oil. As a consequence, the channel for CO2 leakage is Honggang fault, while the leakage time should be early than the second section of Mingshui Formation.