古地理学报 ›› 2008, Vol. 10 ›› Issue (2): 111-123. doi: 10.7605/gdlxb.2008.02.001

• 岩相古地理学及沉积学 •    下一篇

海拉尔盆地乌尔逊凹陷与松辽盆地孤店CO2气田含片钠铝石砂岩的岩石学特征

高玉巧 刘  立曲希玉刘  娜   

  1. 1 内生金属矿床成矿机制研究国家重点实验室  南京大学地球科学系  江苏南京210093
    2 吉林大学地球科学学院  吉林长春130061
  • 出版日期:2008-04-01 发布日期:2008-04-01
  • 作者简介:高玉巧,女,1978年生,2007年6月毕业于吉林大学并获博士学位,现为南京大学地球科学系博士后,主要从事沉积岩石学与储集层地质学方面的研究工作。通讯地址:南京市汉口路22号南京大学地球科学系(210093);联系电话:13851535609;Email:gaoyuqiao1973@sinacom。
  • 基金资助:

    本研究为国家自然科学基金“岩浆成因二氧化碳气藏中储集砂岩的热对流成岩作用(编号:40372060)和“松辽盆地南部含片钠铝石砂岩中的成岩成藏记录研究(编号:40672074)资助的成果

Petrologic characteristics of dawsonitebearing sandstones in Wuerxun Sag of Hailaer Basin and Gudian CO2 Gasfield in Songliao Basin

Gao Yuqiao Liu Li Qu Xiyu Liu Na   

  1. 1 State Key Laboratory for Mineral Deposit Research,Department of Earth Sciences,
        Nanjing University,Nanjing210093,Jiangsu
    2 College of Earth Sciences,Jilin University,Changchun130061,Jilin
  • Online:2008-04-01 Published:2008-04-01
  • About author:Gao Yuqiao,born in 1978,obtained her doctoral degree from Jilin University in June,2007. Now she is a post doctor in Nanjing University,and is mainly engaged in sedimentary petrology and reservoir geology. Tel:13851535609. Email:gaoyuqiao1973@sinacom.

摘要:

海拉尔盆地乌尔逊凹陷南屯组与松辽盆地孤店CO2气田泉头组发育大量含片钠铝石砂岩。通过偏光显微镜、扫描电镜、茜素红-S染色、X射线衍射、电子探针与INCA能谱分析等,对含片钠铝石砂岩的骨架碎屑组分、胶结物与自生矿物、成岩共生序列等岩石学特征进行了系统研究。研究表明,含片钠铝石砂岩的岩石类型为长石砂岩和岩屑长石砂岩,粒度以细粒、细—中粒为主,分选差—中等。砂岩中胶结物主要为次生加大石英、自生石英、片钠铝石、铁白云石和粘土矿物。其中,片钠铝石最高可达砂岩总体积的22%在砂岩中或以放射状、束状、菊花状、杂乱毛发状、毛球状、板状等集合体充填孔隙,或呈束状和板状交代长石和岩屑。电子探针与INCA能谱综合分析表明,片钠铝石主要由Na、Al、O、C等组成。在含片钠铝石砂岩中,成岩共生序列依次为粘土矿物包壳—次生加大石英、自生石英、自生高岭石—油气充注—CO2充注—片钠铝石—铁白云石。其中,CO2注入前形成的自生矿物组合主要为次生加大石英、自生石英和自生高岭石,CO2注入后形成的自生矿物组合主要为片钠铝石和铁白云石。

Abstract:

Both the Nantun Formation in the Wuerxun Sag of the Hailaer Basin and the Quantou Formation in the Gudian CO2 Gasfield in the southern Songliao Basin contain abundant dawsonitebearing sandstones. The petrologic characteristics of these sandstones including the framework clastic composition,cements and authigenic minerals and diagenetic paragenesis succession are investigated through polarizering microscope,scanning electron microscope,alizarin redstaining,Xray diffraction,electron probe and INCA energy spectrum analysis etc. The results show that these sandstones are finegrained or finetomediumgrained,poorly to moderately sorted arkoses and lithic arkoses. The dominant cements are secondary quartz overgrowths,authigenic quartz,dawsonite,ankerite and clay minerals. The amount of dawsonite is higher(up to 22% of the total volume of the sandstones),either as cements,filling intergrain pores as radial,bunchy,rosette,intricately trichoid,spheric and platy collectives,or as replacement of feldspar and lithic grains with bunchy and platy shapes. Dawsonite is mainly composed of elements such as Na,Al,O,and C according to electron probe and INCA energy spectrum analyses. The paragenetic sequence includes(1)clay mineral coatings;(2)secondary quartz overgrowths,authigenic quartz,authigenic kaolinite;(3)petroleum charging;(4)CO2 charging;(5)dawsonite;and (6)ankerite. The authigenic minerals formed before CO2 charging include secondary quartz overgrowths,authigenic quartz and authigenic kaolinite,while the main cements formed after CO2 charging are dawsonite and ankerite.