Sun Guoqiang, Ma Jinye, Wang Haifeng, Chen Ji, Zhang Yongshu, Jia Yanyan, Zhang Shengyin, Shi Ji'an. Characteristics and significances of carbonate cements in northern Mahai region,northern margin of Qaidam Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2012, 34(2): 134-139. doi: 10.11781/sysydz201202134
Citation: Sun Guoqiang, Ma Jinye, Wang Haifeng, Chen Ji, Zhang Yongshu, Jia Yanyan, Zhang Shengyin, Shi Ji'an. Characteristics and significances of carbonate cements in northern Mahai region,northern margin of Qaidam Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2012, 34(2): 134-139. doi: 10.11781/sysydz201202134

Characteristics and significances of carbonate cements in northern Mahai region,northern margin of Qaidam Basin

doi: 10.11781/sysydz201202134
  • Received Date: 2011-06-29
  • Rev Recd Date: 2012-02-07
  • Publish Date: 2012-03-28
  • Based on lithology,mineralogy and geochemistry,the generation environment and source for carbonate cements in sandstone reservoirs in the lower position of the Paleogene Lower Ganchaigou Formation in the north of the Mahai Uplift which located in the northern margin of the Qaidam Basin were studied systematically.Two types of calcite cements were found,including xenomorphic micrite and hypidiotopic microcrystalline.Their carbon isotope values (δ13C) ranged from -7.1‰ to -3.3‰ with the average of -4.9‰,and the oxygen isotope values (δ18O) ranged from -11.3‰ to -9.6‰ with the average of -10.3‰.The Z-values of paleosalinity ranged from 107.0 to 115.6 and the average value was 112.1.The generation of carbonate cements in sandstone reservoirs in the study area might be related to the decarboxylation of organic matters during the early diagenetic stage.A little organic carbon also participated in the reaction.Diagenetic fluids mainly came from clast and atmospheric freshwater.

     

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  • [1]
    Boles J R.Carbonate cementation in Tertiary sandstones,San Joaquin basin,California[J].Spec Publs Int Ass Sediment,1998,26:261-284.
    [2]
    Antar A W,Earle F M.Origin of giant calcite cemented concretions,Temple Member,Qasr El Sagha Formation(Eocene),Faiyum depression,Egypt[J].Journal of Sedimentary Research,2001,71(1):70-81.
    [3]
    王春梅,裴昌蓉.利用负胶结物投点图评价西湖凹陷古近系砂岩储层[J].断块油气田,2010,17(1):52-54.
    [4]
    张立强,罗晓容.准噶尔盆地高压带碳酸盐胶结层的分布及特征[J].石油实验地质,2011,33(4):388-391.
    [5]
    孙玉善,申银民,徐迅.应用成岩岩相分析法评价和预测非均质性储层及其含油性:以塔里木盆地哈得逊地区为例[J].沉积学报,2002,20(1):55-59.
    [6]
    Carlos R,Rafaela M,Karl R,et al.Facies-related disgenesis and multiphase siderite cementation and dissolution in the reservoir sandstones of the Khatatba Formation,Egypt's western desert[J].Journal of Sedimentary Research,2001,71(3):459-472.
    [7]
    Macaula Y C I,Haszeldine R S,Fallick A E.Distribution,chemistry,isotopic composition and origin of diagenetic carbonates:Magnus Sandstone,North Sea[J].Journal of Sedimentary Petrology,1993,63:33-43.
    [8]
    Mostafa F,Harrison T M,Grove M.In situstable isotopic evidence for protracted and complex carbonate cementation in a petroleum reservoir,NorthColes Levee,San Joaquin basin,California,USA[J].Journal of Sedimentary Research,2001,71(3):444-458.
    [9]
    Friedman I,O’Neil J R.Complilation of stable isotope fractionation factors of geochemical interest[M]//Fleisher M,ed.Data of Geochemistry.6th ed. Reston,Virginia:USGS,1977:60.
    [10]
    Ortoleva P J.Basin compartments and seals:AAPG Memoir 61[M].Tulsa:AAPG Press,1994:477.
    [11]
    Rosenbaum J M,Sheppard S M F.An isotopicstudy of siderites, dolomites, and ankerites at high temperature[J].Geochimica et Cosmochimica Acta,1986,50:1147-1150.
    [12]
    黄思静.锶同位素地层学在碎屑岩成岩研究中的应用[J].沉积学报,2002,20(3):359-366.
    [13]
    McBride E F,Parea G C.Origin of highly elongate,calcite-cemented concretions in some Italian coastal beach and dunesands[J].Journal of Sedimentary Research,2001,71(1):82-87.
    [14]
    王琪,禚喜准,陈国俊,等.延长组砂岩中碳酸盐胶结物氧碳同位素组成特征[J].天然气工业,2007,27(10):28-32.
    [15]
    王芙蓉,何生,杨兴业.中扬子海相碳酸盐岩中方解石脉成岩环境研究[J].石油实验地质,2011,33(1):56-60.
    [16]
    刘殿鹤,李凤杰,郑荣才,等.柴北缘西段古近系下干柴沟组沉积相特征分析[J].天然气地球科学,2009,20(6):847-853.
    [17]
    孙国强,谢梅,张永庶,等.柴北缘马北地区下干柴沟组下段沉积特征及演化[J].岩性油气藏,2011,23(6):56-61.
    [18]
    陈吉,谢梅,史基安,等.柴北缘马北地区下干柴沟组储层特征[J].天然气地球科学,2011,22(5):821-826.
    [19]
    汪立群,徐凤银,庞雄奇,等.马海-大红沟凸起油气勘探成果与柴达木盆地北缘的勘探方向[J].石油学报,2005,26(3):21-26.
    [20]
    王琪,郝乐伟,陈国俊,等.白云凹陷珠海组砂岩中碳酸盐胶结物的形成机理[J].石油学报,2010,31(4):554-560.
    [21]
    蔡观强,郭锋,刘显太,等.东营凹陷沙河街组沉积岩碳氧同位素组成的古环境记录[J].地球与环境,2009,37(4):347-354.
    [22]
    刘德良,孙先知,李振生,等.鄂尔多斯盆地奥陶系白云岩碳氧同位素分析[J].石油实验地质,2006,28(2):155-161.
    [23]
    Hudson J D.Stable isotopes limestone lithification[J].Journal of Geological Society,1977,133(4):637-660.
    [24]
    Suess E,Whiticar M J.Methane-derived CO2 in pore fluids expelled from the Oregon subduction zone[J].Palaeogeography,Palaeoclimatology,Palaeoecology,1989,71(1-4):119-136.
    [25]
    Surdam R C,Crossey L J,Hagen E S.Organic-inorganic interactions and sandstone diagenesis [J].AAPG Bulletin,1989,73:1-23.
    [26]
    王大锐.油气稳定同位素地球化学[M].北京:石油工业出版社,2000:137-196.
    [27]
    张秀莲.碳酸盐岩中氧、碳稳定同位素与古盐度、古水温的关系[J].沉积学报,1985,3(4):17-28.
    [28]
    傅启龙.库车盆地西北缘下第三系碳氧同位素特征及成岩环境[J].地层学杂志,1996,20(4):280-283.
    [29]
    邵龙义,窦建伟,张鹏飞.西南地区晚二叠世氧、碳稳定同位素的古地埋意义[J].地球化学,1996,25(6):575-580.
    [30]
    Keith M H,Weber J N.Isotopic composition and environmental classification of selected limestones and fossils[J].Geochim Cosmochim Acta,1964,28:1787-1816.(编辑 徐文明)
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