西南石油大学学报(自然科学版) ›› 2006, Vol. 28 ›› Issue (3): 48-52.DOI: 10.3863/j.issn.1000-2634.2006.03.015
• 地质勘探 • 上一篇 下一篇
吕儒明1,2,陈宗太2,汪彦1,陈明瞩2,周移兴2,李光恒2,伍佳明2
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通讯作者:
Lu Ru-ming,CHEN Zong-tai,WANG Yan, et al.
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摘要: 根据研究区的基本资料和相应成果,在分析保山盆地基本构造格局的基抽上,发现因保山盆地主控断层的西边在盆地演化过程中一直处于隆升状态,从而造成不同地带砾岩的分布和含1存在差异,在钻浏井、地震资抖中的体现也不相同。通过多种方法对永铸街气田的主物源方向进行论证后,认为永铸街气田的物源来自西边。
关键词: 物源分析, 岩性, 地震相剖面, 羊邑组, 保山盆地
Abstract: Basing on the analysis to the basic tectonics framework of Baoshan Basin, this paper has studied the basic data and on Baoshan Basin, and found that the west of the main fault in Baoshan Basin have been rising during the development of basin. So the distribution and the content of conglomerate were different, and its geological phenomenon in the data of drillingoutcrop 。logging and seismal section in different area. By studing with a few methods, we have such a conclusion that the main sediment source of Yongzhujie Gas Field was from the west
Key words: analysis of sediment resource, rock character, seism facies section, Yangyi Formation, Baoshan Basin
中图分类号:
TE111.3
吕儒明;陈宗太;汪彦;陈明瞩;周移兴;李光恒;伍佳明. 保山盆地永铸街气田沉积物源分析[J]. 西南石油大学学报(自然科学版), 2006, 28(3): 48-52.
Lu Ru-ming;CHEN Zong-tai;WANG Yan;et al. . THE ANALYSLS OF SEDIIVVIENT SOURCE OF YONG-ZHUJIE GAS FIELD IN BAOSHAN BASIN[J]. 西南石油大学学报(自然科学版), 2006, 28(3): 48-52.
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http://journal15.magtechjournal.com/Jwk_xnzk/CN/Y2006/V28/I3/48