松辽盆地矿床地质概况及特征综述
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摘要
松辽盆地作为勘探重点开发地区其地层研究一直备受广大学者关注,本文就众多学者对松辽盆地矿床地质概况及特征进行了部分总结。松辽盆地南部深层火石岭组-营城组分布于众多分割断陷盆地中,以单断的箕状断陷为主,少数为双断的地堑式断陷。众多学者对松辽盆地地区矿层进行了精细研究,利用地球物理特征归纳松辽盆地地层的两次喷发,还有学者运用区域叠置的方法对优质储层进行了可靠预测。
As a key exploration and development area, the stratigraphic study of Songliao Basin has attracted much attention of scholars. This paper summarizes the geological survey and characteristics of deposits in Songliao Basin by many scholars.The deep Huoshiling Formation-Yingcheng Formation in the south of Songliao Basin is distributed in many separated fault basins, mainly single-fault dustpan-like fault depressions, and a few double-fault graben-type fault depressions. Many scholars have studied the ore beds in Songliao Basin in detail, summed up the two eruptions of strata in Songliao Basin by using geophysical characteristics, and made reliable prediction of high-quality reservoirs by using the method of regional superimposition.
As a key exploration and development area, the stratigraphic study of Songliao Basin has attracted much attention of scholars. This paper summarizes the geological survey and characteristics of deposits in Songliao Basin by many scholars.The deep Huoshiling Formation-Yingcheng Formation in the south of Songliao Basin is distributed in many separated fault basins, mainly single-fault dustpan-like fault depressions, and a few double-fault graben-type fault depressions. Many scholars have studied the ore beds in Songliao Basin in detail, summed up the two eruptions of strata in Songliao Basin by using geophysical characteristics, and made reliable prediction of high-quality reservoirs by using the method of regional superimposition.
引文
[1]吉林省地质矿产局.吉林省区域地质志[M].北京:地质出版社,1988:224-230.
[2]吉林省区域地层表编写组.东北区域地层表.吉林省分册[M].北京:地质出版社,1979:71-80.
[3]任延广,朱德丰,万传彪,等.松辽盆地徐家围子断陷天然气聚集规律与下步勘探方向[J].大庆石油地质与开发,2004,23(5):26-29.
[4]李楚琦.关于松辽盆地深部储层岩石特征研究[J].石化技术,2018,25(12):98.
[5]胡佳,王立武,张双杰,皮雄,迟唤昭,刑驰,刘建松.盆地内部火山机构的地质模式建立方法及其应用——以松辽盆地南部地区营城组火山岩为例[J].西安石油大学学报(自然科学版),2018,33(06):18-26.
[6]王腾飞,程日辉,沈艳杰.松辽盆地东南缘营城组流纹岩类型及其在火山岩地层分析中的意义[J].吉林大学学报(地球科学版),2014,44(01):45-55.
[7]徐淑娟,赵泽辉,姜晓华,程宏岗,崔俊峰,贾丽,周文杰.松辽盆地中生代火山岩地球物理特征及分布预测[J].非常规油气,2016,3(03):27-34.
[8]王苗,陆建林,左宗鑫.等.火山—碎屑充填盆地的层序地层学研究:以松辽盆地长岭断陷为例[J].石油实验地质,2016,38(6):796-802.
[9]王璞珺,陈崇阳,张英,等.松辽盆地长岭断陷火山岩储层特征及有效储层分布规律[J].天然气工业,2015,35(8):10-18.
[10]刘哲,单玄龙,衣健.松辽盆地长岭断陷火山岩储层对天然气成藏的控制作用[J].世界地质,2017,36(3):880-888.
[11]陆建林,王果寿,蔡进功,等.长岭断陷火山岩气藏勘探潜力[J].天然气工业,2007,27(8):13-15.
[12]栾颖.梨树断陷营城组沉积特征[J].四川地质学报,2018,38(04):549-551.
[13]范雪松,樊太亮,王宏语.松辽盆地梨树断陷营城组源汇体系研究[J].特种油气藏,2018,25(04):12-17.
[2]吉林省区域地层表编写组.东北区域地层表.吉林省分册[M].北京:地质出版社,1979:71-80.
[3]任延广,朱德丰,万传彪,等.松辽盆地徐家围子断陷天然气聚集规律与下步勘探方向[J].大庆石油地质与开发,2004,23(5):26-29.
[4]李楚琦.关于松辽盆地深部储层岩石特征研究[J].石化技术,2018,25(12):98.
[5]胡佳,王立武,张双杰,皮雄,迟唤昭,刑驰,刘建松.盆地内部火山机构的地质模式建立方法及其应用——以松辽盆地南部地区营城组火山岩为例[J].西安石油大学学报(自然科学版),2018,33(06):18-26.
[6]王腾飞,程日辉,沈艳杰.松辽盆地东南缘营城组流纹岩类型及其在火山岩地层分析中的意义[J].吉林大学学报(地球科学版),2014,44(01):45-55.
[7]徐淑娟,赵泽辉,姜晓华,程宏岗,崔俊峰,贾丽,周文杰.松辽盆地中生代火山岩地球物理特征及分布预测[J].非常规油气,2016,3(03):27-34.
[8]王苗,陆建林,左宗鑫.等.火山—碎屑充填盆地的层序地层学研究:以松辽盆地长岭断陷为例[J].石油实验地质,2016,38(6):796-802.
[9]王璞珺,陈崇阳,张英,等.松辽盆地长岭断陷火山岩储层特征及有效储层分布规律[J].天然气工业,2015,35(8):10-18.
[10]刘哲,单玄龙,衣健.松辽盆地长岭断陷火山岩储层对天然气成藏的控制作用[J].世界地质,2017,36(3):880-888.
[11]陆建林,王果寿,蔡进功,等.长岭断陷火山岩气藏勘探潜力[J].天然气工业,2007,27(8):13-15.
[12]栾颖.梨树断陷营城组沉积特征[J].四川地质学报,2018,38(04):549-551.
[13]范雪松,樊太亮,王宏语.松辽盆地梨树断陷营城组源汇体系研究[J].特种油气藏,2018,25(04):12-17.