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地质学报  2006 

塔里木盆地热液活动地质地球化学特征及其对储层影响

, PP. 245-253

Keywords: 塔里木盆地,碳酸盐岩,热液,矿物组合,溶蚀

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Abstract:

塔里木盆地二叠纪时发生了强烈的岩浆-火山作用,与之相关的热液流体沿着断裂、裂缝以及不整合面活动,并与所经碳酸盐岩围岩发生反应,使围岩发生不同程度的溶蚀改造,主要表现在:1热液溶蚀和热褪色现象显著;2沉淀生成多种热液矿物组合,如萤石-石英组合、闪锌矿-绿泥石-方解石组合,重晶石-石英-黄铁矿-菱铁矿组合等;3热液作用区域碳酸盐岩成分发生了明显的变化,主要表现为Fe、Mn、Si等元素含量的升高,比正常灰岩高出几倍至几十倍。上述特点与岩溶作用和成岩溶蚀作用特征明显不同。对典型钻孔碳酸盐岩储层研究表明,无论灰岩还是白云岩,在热液作用下都会产生大量的微小溶蚀孔洞,储层物性得到明显的改善,因此热液作用是影响储层物性不可忽视的重要因素。

References

[1]  Zhang Kang.2001.Type of Tahe Oil field and exploration play in carbonate of Tarim Basin.Acta Petrolei Sinica,22(4):1~6 (in Chinese with English abstract).
[2]  Zhu Dongya,Hu Wenxuan,Song Yucai,Jin Zhijun.2005.Fluoritization characteristics in Tz45 well and its effents on carbonate reservoir in Tarim Basin.Journal of Petrology and Minerology,24(3):205~215.
[3]  陈汉林,贾承造.1997.塔里木盆地地质热事件研究.科学通报,42(10):1096~1099.
[4]  贾承造.1997.中国塔里木盆地构造特征与油气.北京:石油工业出版社,156~165.
[5]  金之钧,张刘平,扬雷,胡文王宣.2002.沉积盆地深部流体的地球化学特征及油气成藏效应初探.地球科学--中国地质大学学报,27(6):659~665.
[6]  林忠民.2002.塔里木盆地塔河油田奥陶系大型油气藏形成条件.地质论评,48(4):372~376.
[7]  赵霞.2000.塔里木盆地塔中45井及柯坪西克尔萤石成因的讨论.西北地质,33(3):5~8.
[8]  朱东亚,胡文王宣,宋玉财,金之钧.2005.塔里木盆地塔中45井油藏萤石化特征及其对储层的影响.岩石矿物学杂志,24(3):205~215.
[9]  Davis E E,Mottl M,Fisher A,Baker K,et al.1992.Ocean Drilling Program,Initial Reports,139.College Station,Texas.
[10]  Hedenquist J W,Henley R W.1985.The important of CO2 on freezing point measurements of fluid inclusions:evidence from active geothermal systems and implications for epithermal ore deposition.Economic Geology,80:1379~1405.
[11]  Jia Chengzao.1997.Structure characteristics and oil and gas in Tarim Basin of China.Beijing:Petroleum Industry Press,156~165 (in Chinese).
[12]  Jin Zhijun,Zhang Liuping,Yang Lei,Hu Wenxuan.2002.Primary study of geochemical features of deep fluids and their effectiveness on oil/gas reservoir formation in sedimental basin.Earth Science-Journal of China University of Geoscience,27(6):659~665 (in Chinese with English abstract).
[13]  Li Ping,Chen Jingshan,Wang Zhenyu.2003.Study on types of Ordovician carbonate reservoir and constrains of carbonate reservoir formation.Gas Exploration and Development,26(1):37~42 (in Chinese).
[14]  Qian Yixiong,Chen Yao,Ma Hongqiang,Chen Qianglu.2004.Chemical analysis and origin of calcite filled in fracture and cave with in Ordovician carbonate in Tahe Oil field,Xinjiang.Acta Sedimentica Sinica,22(1):6~12 (in Chinese with English abstract).
[15]  Sillitoe R H.1989.Gold deposits in Western Pacific island arcs:the magmatic connection.Economy Geology Monography,6:274~291.
[16]  Simoneit B R T,Leif R N,Sturz A A,Sturdivant A E,Gieskes J M.1992b.Geochemistry of shallow sediments in Guaymas Basin,Gulf of California:Hydrothermal gas and oil migration and effects of mineralogy.Organic Geochemistry,18:765~784.
[17]  Stoffregen R.1987.Genesis of acid-sulfate alteration and Au-Cu-Ag mineralization at Summitville,Colorado.Economic Geology,82:1575~1591.
[18]  Zhao Xia.2000.Origin of fluorite in Kepingxikeer and Well Tz45 in Tarim Basin.Northwest Geology,33(3):5~8 (in Chinese with English abstract).
[19]  http://aapg.confex.com/aapg/da2004/techprogram/S2388.htm.
[20]  黎平,陈景山,王振字.2003.塔中地区奥陶系碳酸盐岩储层形成控制因素及储层类型研究.天然气勘探与开发,26(1):37~42.
[21]  钱一雄,陈跃,马宏强,陈强路.2004.新疆塔河油田奥陶系碳酸盐岩溶洞、裂隙中方解石胶结物元素分析与成因.沉积学报,22(1):6~12.
[22]  张景廉,金之钧,等.2001.塔里木盆地深部地质流体与油气藏的关系.新疆石油地质,22(5):371~375.
[23]  张抗.2001.塔河油田性质和塔里木碳酸盐岩油气勘探方向.石油学报,22(4):1~6.
[24]  Chen Hanlin,Jia Chengzao.1997.Studies on geothermal events in Tarim Basin.Chinese Science Bulletin,42(10):1096~1099 (in Chinese).
[25]  Gieskes J M,Simoneit B R T,Goodfellow W D,Baker P A,Mahn C.2002.Hydrothermal geochemistry of sediments and pore waters in Escanaba Trough-ODP Leg 169.Applied Geochemistry,17:1435~1456.
[26]  Inoue A.1995.Formation of clay minerals in hydrothermal environments.In:Velde B,ed.Origin and mineralogy of clays-clays in the environment.Berlin:Springer Verlag.
[27]  Lein A Y,Sagalevitch A M.2000.The "black smokers" at the Rainbow field-The region of the high scale abiogenic synthesis of the methane.Priroda,9:44~54.
[28]  Lin Zhongmin.2002.Formation conditions of large-scale oil/gas pool in Ordocian carbonate rock in the Tahe Oil Field,Tarim Basin.Geological Review,48(4):372~376 (in Chinese with English abstract).
[29]  Peresypkin V I,Lein A Y,Bogdanov Y A,Bortnikov N S.1999.The lipids of hydrothermal formations on the area 14°45N and 29°N,Mid-Atlantic Ridge.Oceanologiya,39:258~269.
[30]  Shock E L.1992.Chemical environments of submarine hydrothermal systems.Origins Life Evolution Biosphere,22:67~107.
[31]  Simoneit B R T,Goodfellow W D,Franklin J M.1992a.Hydrothermal petroleum at the seafloor and organic matter alteration in sediments of Middle Valley,Northern Juan de Fuca Ridge.Applied Geochemistry,7:257~264.
[32]  Simoneit B R T,Lein A Y,Peresypkin V I,Osipov G A.2003.Composition and origin of hydrothermal petroleum and associated lipids in the sulfide deposits of the Rainbow Field (Mid-Atlantic Ridge at 36°N).Geochimica et Cosmochimica Acta,68(10):2275~2294.
[33]  Zhang Jinglian,Jin Zhijun,et al.2001.The correlations between deep fluids and oil reservoirs in Tarim Basin.Xinjiang Petroleum Geology,22(5):371~375 (in Chinese).

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