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松辽盆地南部红岗油田青山口组砂岩中片钠铝石的形成温度 被引量:2

Formation Temperature of Dawsonite from Qingshankou Formation in the Honggang Oilfield,Southern Songliao Basin
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摘要 主要以松辽盆地南部红岗油田富含片钠铝石砂岩的红143和红146井为研究对象,通过普通薄片鉴定、茜素红-S染色、扫描电镜、能谱分析、显微测温等分析方法,对研究区含片钠铝石砂岩的成岩共生序列,尤其是流体包裹体均一温度进行了详细的研究。红岗油田成岩共生序列为:黏土矿物→石英次生加大边→方解石→片钠铝石→铁白云石→石英愈合微裂隙。通过流体包裹体测温得出:方解石胶结物的均一温度峰值在110~120℃;石英愈合微裂隙的均一温度峰值在130~140℃。片钠铝石的形成温度介于上述两者之间,在120~130℃。通过与国内外已有的研究成果相比较发现:经过岩浆改造后的砂岩中的片钠铝石的形成温度较低,在25~150℃;以子矿物产于包裹体中的片钠铝石的形成温度相对较高,在250~340℃。红岗油田片钠铝石属于第一种情况,形成温度较低,在120~130℃这个温度区间内。扫描电镜和能谱分析显示,形态上,红岗油田片钠铝石(形成温度在120~130℃)主要为针状,乌尔逊凹陷片钠铝石(形成温度在78.56~115.02℃)的片钠铝石主要为针柱状;化学成分上,红岗油田的片钠铝石与乌尔逊凹陷的片钠铝石相比,前者富Si,贫Na、Al和O,后者富Na、Al和O,贫Si。 This article mainly use the Hong-143 and Hong-146 well that rich in dawsonite-bearing sandstones as reaearch objiects.According to the analysis of conventional thin sections,alizarin red-staining,SEM,INCA energy spectromete,micro-thermometry,the diagenetic paragenesis succession of dawsonite-bearing sandstones,in particular,the homogenization tempreature of fluid inclusion have been studied in detail.The diagenetic paragenesis of the Honggang Oilfield is clay minerals→secondary quartz overgrowths→calcite→dawsonite→ankerite→quartz healing microfracture.On the basis of intensive micro-thermometry,the peak of the homogenization tempreature is 110~120℃ in the calcite;while 130~140℃ in the quartz healing microfracture.The formation temperature of dawsonite is between calcite and quartz healing microfracture,which is 120~130℃.Comparing with research results at home and abroad,the formation temperature of dawsonite that is transformed by magma is relatively low,which is 25~150℃.The formation temperature of dawsonite that appeared in the inclusion as daughter mineral is relatively high,which is 250~340℃.The dawsonite in the southern Songliao Basin belong to the first situation,the formation temperature is relatively low,which is 120~130℃.Scanning electron microscopy and energy spectrum analysis shows that the dawsonite of Hong gang oil filed(The formation of temperature between 120~130℃) is mainly needle-like,the chemical composition is rich in Si,poor in Na,Al and O;the dawsonite of Wuerxun Depression(The formation of temperature between 78.56~115.02℃) is mainly columnar pin,chemical composition is rich in Na,Al and O,poor in Si.
出处 《沉积学报》 CAS CSCD 北大核心 2011年第2期293-302,共10页 Acta Sedimentologica Sinica
基金 国家自然科学基金项目(批准号:40672074) 教育部博士点基金项目(编号:20070183137)联合资助
关键词 红岗油田 片钠铝石 愈合微裂隙 流体包裹体 均一温度 形成温度 Honggang Oilfield dawsonite healing microfracture fluid inclusion homogenization tempreature formation temperature
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  • 1Gunter W D, Wiwchar B, Perkins E H. Aquifer disposal of CO2-rich greenhouse gases: extension of the time scale of experiment for CO2-sc- questering reactions by geochemical modeling[J]. Mineral Petrology, 1997, 59:120-137.
  • 2Biniam Zerai, Beverly Z, Saylor G M. Computer simulation of CO2 trapped through mineral precipitation in the Rose Run Sandstone, Ohio [ J]. Apphed Geochemistry, 2006, 21 : 223-240.
  • 3Xu T, Apps J A, Pruess K. Mineral sequestration of carbon dioxide in a sandstone shale system [J]. Chemical Geology, 2005, 217:298-317.
  • 4Baker J C, Bai G P, Hamilton PJ, et al. Continental-scale magmatic carbon dioxide seepage recorded by dawsonite in the Bowen-Gunnedah- Sydney basin system, eastern Australia[J]. Journal of Sedimentary Re- search, 1995,65 (3) : 522-530.
  • 5Watson M N, Zwingmann N, Lemon N M. The Ladbroke Grove-Kat- nook carbon dioxide natural laboratory: A recent CO2 accumulation in a lithic sandstones reservoir[ J]. Energy, 2004, 29 : 1457-1466.
  • 6刘立,高玉巧,曲希玉,蒙启安,高福红,任延广,朱德丰.海拉尔盆地乌尔逊凹陷无机CO_2气储层的岩石学与碳氧同位素特征[J].岩石学报,2006,22(8):2229-2236. 被引量:41
  • 7Worden R H, Dawsonite cement in the Triassic Lam Formation, Shab- wa basin, Yemen : A natural analogue for a potential mineral product of subsurface CO2 storage for greenhouse gas reduction [ J ]. Marine and Petroleum Geology, 2006, 23:61-77.
  • 8Heritsch H. Dawsonite as a product of low-hydrothermal transformation of a volcanic breccia from a borehole in eastern Styria (Austria) [ J]. Neus Jahrbuch far Mineralogie, Monatshefte, 1975,8:360-368.
  • 9Goldbery R, Loughnan F C. Dawsonite and nordstrandite in Permian Berry Formation of the Sydney Basin, New Wales [ J ]. Australia Sedi- mentology, 1970, V. 24,P. 565-579.
  • 10杜韫华.一种次生的片钠铝石[J].地质科学,1982,(1):434-436.

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