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柴达木盆地西部扎哈泉地区油气成藏过程
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  • 英文篇名:Hydrocarbon Charge History of Zhahaquan Area,Western Qaidam Basin
  • 作者:王琳 ; 吴海 ; 王科 ; 桂丽黎 ; 袁莉 ; 王鹏 ; 袁海莉
  • 英文作者:WANG Lin;WU Hai;WANG Ke;GUI Li-li;YUAN Li;WANG Peng;YUAN Hai-li;Research Institute of Petroleum Exploration & Development,PetroChina;Key Laboratory of Basin Structure and Petroleum Accumulation,China National Petroleum Corporation;Research Institute of Petroleum Exploration & Development,PetroChina Qinghai Oilfield Company;
  • 关键词:扎哈泉地区 ; 油气成藏期次 ; 流体包裹体 ; 定量颗粒荧光 ; 柴达木盆地西部
  • 英文关键词:Zhahaquan area;;hydrocarbon accumulation period;;fluid inclusion;;quantitative grain fluorescence;;western Qaidam Basin
  • 中文刊名:KXJS
  • 英文刊名:Science Technology and Engineering
  • 机构:中国石油勘探开发研究院;中国石油天然气集团公司盆地构造与油气成藏重点实验室;中国石油青海油田公司勘探开发研究院;
  • 出版日期:2017-12-08
  • 出版单位:科学技术与工程
  • 年:2017
  • 期:v.17;No.431
  • 基金:国家油气重大专项(2016ZX0003);; 中石油科学研究与技术开发项目(2016E-0101)资助
  • 语种:中文;
  • 页:KXJS201734032
  • 页数:8
  • CN:34
  • ISSN:11-4688/T
  • 分类号:208-215
摘要
扎哈泉地区为柴达木盆地西部典型的致密油勘探区。通过储层定量颗粒荧光、包裹体岩相学、显微测温等分析技术,结合埋藏史和热史,对油气动态演化过程进行分析。扎哈泉地区油藏原油属中等密度常规原油,但储层的QGF-E、TSF荧光光谱特征显示该区原油既有轻质-中质原油,又有重质原油存在。储层中主要发育两类烃包裹体,早期主要为黄色荧光油包裹体,晚期主要发育蓝绿-淡蓝色荧光油包裹体。通过测定伴生盐水包裹体均一温度及埋藏史和热史分析认为,扎哈泉地区主要经历了下油砂山组沉积末期(13 Ma)的原油充注和狮子沟组沉积早期(6 Ma)至今的原油充注以及油藏向上覆地层调整过程。
        The Zhahaquan area is a typical tight-oil exploration area in the western Qaidam Basin. The dynamic evolution and accumulation of oil and gas is studied deeply by the analysis of reservoir quantitative grain fluorescence( QGF),fluid inclusions petrography and micro-temperature measurement,and then combined with the burial and thermal history of this area. The crude oil in reservoirs of Zhahaquan area is medium-density conventional oil,while the results of QGF-E and TSF indicate that both light-medium density oil and heavy density oil are existed in reservoir. Two types of hydrocarbon fluid inclusions are mainly developed in this area,earlier oil inclusions with yellow fluorescence and later oil inclusions with blue green-light blue fluorescence. Based on the analysis of the homogenization temperature of inclusions and the burial and thermal history,it is concluded that there are two stages of hydrocarbon charging,of which the first charging time was around 13 Ma,which corresponded to the end of the deposition of Lower Youshashan Formation,the second charging time was about 6 Ma,which corresponded to the early deposition of Shizigou Formation.
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