塔里木盆地轮古东地区油气相态及饱和度的主控因素MAIN CONTROLLING FACTORS OF THE PETROLEUM PHASE STATES AND THEIR SATURATIONS IN LUNGUDONG AREA OF TARIM BASIN
陈洪旭,周东升,黄晓伟,陈英豪
CHEN Hongxu,ZHOU Dongsheng,HUANG Xiaowei,CHEN Yinghao
摘要(Abstract):
塔里木盆地轮古东地区的油气主要为凝析气藏,但与常规凝析气藏又有所不同,且不同凝析气藏间饱和状态也存在差异。研究认为:轮古东凝析气藏具有"气干油重"的特征,可分为未饱和、饱和两种凝析气藏,未饱和凝析气藏主要分布在走滑断裂附近和充注强度大的区域,饱和凝析气藏主要分布在断裂不发育和充注强度较弱的区域;凝析气藏相态的主控因素是经历多期成藏、发育大型深部断裂、充注强度变化及良好的盖层保护。
The petroleum in Lungudong area of Tarim Basin is produced from condensate gas reservoirs,but comparing with the conventional ones,there are a certain differences among the saturation conditions of different condensate gas reservoirs.The studies show that the condensate gas reservoirs in Lungudong have the features of " dry gas and heavy oil" and can be divided into unsaturated and saturated condensate gas reservoirs.The former is mainly distributed nearby the strike-slip faults and the area with strong infilled intensity;the latter is principally accumulated in the areas with less-developed faults and weak-infilled intensity;the main controlling factors on the phase states of the condensate gas reservoirs are presented as follows:multi-period accumulation and enrichment,large well-developed deep fractures,charges of the infilled intensity and much better caprock preservation.
关键词(KeyWords):
塔里木盆地;轮古东地区;油气相态;饱和度;主控因素;凝析气藏
Tarim Basin;Lungudong area;petroleum phase state;saturation;main controlling factor;condensate gas reservoir
基金项目(Foundation): 高校基本科研业务费专项资金项目“TSR对碳酸盐岩储层流体的影响研究”(2652013066)
作者(Author):
陈洪旭,周东升,黄晓伟,陈英豪
CHEN Hongxu,ZHOU Dongsheng,HUANG Xiaowei,CHEN Yinghao
参考文献(References):
- [1]周兴熙.库车油气系统油气藏相态分布及其控制因素[J].天然气地球科学,2004,15(3):205-213.
- [2]朱光有,张水昌,梁英波.四川盆地深部海相优质储集层的形成机理及其分布预测[J].石油勘探与开发,2006,33(2):161-166.
- [3]康志江,邸元,赵艳艳,等.缝洞型油藏洞穴内流体流动特征[J].大庆石油地质与开发,2014,33(3):82-85.
- [4]张水昌,朱光有.四川盆地海相天然气富集成藏特征与勘探潜力[J].石油学报,2006,27(5):1-8.
- [5]付广,李颖,石娜.天然气富集的相态转变条件及对成藏的贡献[J].大庆石油地质与开发,2009,28(1):1-5.
- [6]赵文智,朱光有,苏劲,等.中国海相油气多期充注与成藏聚集模式研究:以塔里木盆地轮古东地区为例[J].岩石学报,2012,28(3):9-21.
- [7]刘静江,李梅,刘慧荣.塔里木盆地轮古东奥陶系凝析气藏成因类型[J].新疆石油地质,2006,27(2):181-183.
- [8]王福焕,王振宇,张云峰,等.轮古东奥陶系断裂特征及其对油气成藏的控制作用[J].中国石油勘探,2011,16(1):15-20.
- [9]陈践发,徐永昌,黄第藩.塔里木盆地东部地区天然气地球化学特征及成因探讨(之二)[J].沉积学报,2001,19(1):141-144.
- [10]王兆云,赵文智,张水昌,等.深层海相天然气成因与塔里木盆地古生界油裂解气资源[J].沉积学报,2009,27(1):153-163.
- [11]王红军,赵文智,胡国艺.塔里木盆地海相成因天然气的两种聚集模式[J].科学通报,2006,52(增刊1):167-173.
- [12]黄第藩,赵孟军,刘宝泉,等.塔里木盆地东部天然气成因类型及其成熟度判识[J].中国科学:D辑地球科学,1996,26(4):365-372.
- [13]侯大力,罗平亚,孙雷,等.近临界凝析气藏动态相态行为[J].大庆石油地质与开发,2014,33(1):86-91.
- [14]王建宝,郭汝泰,肖贤明,等.塔里木盆地轮南低隆起早古生代油气藏形成的期次与时间研究[J].沉积学报,2002,20(2):320-325.
- [15]Krooss B M,Leythaeuser D,Lillack H.Nitrogen-rich natural gases,qualitative and quantitatire aspects of natural gas accumulation in reservoirs[J].Erdol and kohle-Erdgas-petrochemie,1993,46(7-8):271-276.
- [16]Behar F,Kressmann S,Rudkiewicz J L,et al.Experimental simulation in confined system and kinetic modeling of kerogen and oil cracking[J].Org Geochem,1991,19(1-3):173-189.
- [17]Dahl J E,Moldowan J M,Peters K E,et al.Diamondoid hydrocarbons as indicators of natural oil cracking[J].Nature,1999,399(6731):54-57.
- [18]Danesh A.PVT and phase behaviour petroleum reservoir fluids[M].Elsevier:Amsterdam,1998:108-113.
- [19]王晓梅,张水昌.轮南地区天然气分布特征及成因[J].石油与天然气地质,2008,29(2):204-209.
- [20]武富礼,赵靖舟,吴少波,等.塔里木北部轮台凸起凝析气藏成藏年代分析[J].地质科学,2002,37(增1):73-80.
- [21]Zhu Guangyou,Jin Qiang,Zhang Shuichang,et al.Distribution Characteristics of Effective Source Rocks and Their Controls on Hydrocarbon Accumulation:A case Study from the Dongying Sag[J].Acta Geologica Sinica,2004,78(6):1275-1288.
- [22]赵孟军,张水昌.塔里木盆地天然气成因类型及成藏条件[J].中国石油勘探,2004,6(2):27-31.
- [23]Pepper A S,Dodd T A.Simple kinetic models of petroleum formation.PartⅡ:oil-gas cracking[J].Mar Petrol Geol,1995,(12)3:321-340.
- [24]朱光有,赵文智,梁英波,等.中国海相沉积盆地富气机理与天然气的成因探讨[J].科学通报,2007,52(增1):46-57.
- [25]王福焕,王振宇,张云峰,等.轮古东奥陶系断裂特征及其对油气成藏的控制作用[J].中国石油勘探,2011,16(1):15-20.
- [26]潘文庆,赵孟军,张宝民,等.塔里木盆地轮西地区奥陶系潜山油藏:一个海西期充注并降解的稠油油藏成藏实例分析[J].地质科学,2008,43(2):321-332.
- [27]王文军,付广,陈仕宇.区域性盖层对不同运移方向油气运聚的控制作用[J].大庆石油地质与开发,2015,34(1):1-6.
- [28]杨殿军.超压对泥岩盖层封闭各种相态天然气的作用研究[J].大庆石油地质与开发,2008,(27)2:12-15.
- [29]戴金星,陈践发,钟宁宁,等.中国大气田及其气源[M].北京:科学出版社,2003.
- [30]Laytheauser D,Schaefer R G,Pooch H.Diffusion of light hydrocarbons in subsurface sedimentary rocks[J].AAPG Bulletin,1983,67(6):889-895.
- 塔里木盆地
- 轮古东地区
- 油气相态
- 饱和度
- 主控因素
- 凝析气藏
Tarim Basin - Lungudong area
- petroleum phase state
- saturation
- main controlling factor
- condensate gas reservoir