石油学报 ›› 2012, Vol. 33 ›› Issue (3): 361-366.DOI: 10.7623/syxb201203003

• 地质勘探 • 上一篇    下一篇

准噶尔盆地油水层无机地球化学响应与识别

曹 剑 1 王绪龙 2 胡文瑄 1 张越迁 2 唐 勇 2 向宝力 2   

  1. 1 南京大学地球科学系 江苏南京 210093; 2 中国石油新疆油田公司 新疆克拉玛依 834000
  • 收稿日期:2011-10-19 修回日期:2011-12-16 出版日期:2012-05-25 发布日期:2012-07-20
  • 通讯作者: 曹 剑
  • 作者简介:曹 剑,男,1978年10月生,2005年获南京大学博士学位,现为南京大学地球科学系副教授,主要从事石油地质学及有机地球化学的研究和教学工作。
  • 基金资助:

    国家重点基础研究发展规划(973)项目(2012CB214803)和国家自然科学基金项目(No.40872086和No.41072090)资助。

The inorganic geochemical response to oil/water intervals in Junggar Basin and its application

CAO Jian 1 WANG Xulong 2 HU Wenxuan 1 ZHANG Yueqian 2 TANG Yong 2 XIANG Baoli 2   

  • Received:2011-10-19 Revised:2011-12-16 Online:2012-05-25 Published:2012-07-20

摘要:

油气水层识别目前通常采用测录井方法,有时也结合一些有机地球化学研究,但在遇到复杂油气运聚时出现了不确定性,带来了经济损失和勘探风险。为探索新的解决途径,以准噶尔盆地腹部陆西地区为例,基于烃-水-岩相互作用机理,通过无机地球化学方法,提出了两项比较有效的响应与识别标志,分别是储层烃-水-岩相互作用特征及其典型成岩矿物的原位地球化学组成,相比而言,全岩地球化学组成反映的是一种“平均”信息,因而识别效果不佳。在研究区,自油层、油水同层、水层、干层,依次储层含油气丰度逐渐降低,与油气充注相关的溶蚀作用逐渐减弱,典型是方解石和长石类碱性矿物在酸性含油气流体作用下的溶蚀;而成岩矿物组合特征亦有变化,高岭石、高岭石-黄铁矿-赤铁矿、菱铁矿-绿泥石、绿泥石分别指示4类产层。4类产层中成岩方解石的Mn元素丰度(MnO质量分数平均值)一般要分别>2.5%、2.0%~2.5%、1.5%~2.0%、<1.0%。这些具体指标可应用于研究区油气勘探实践,同时思路和方法可供同类工作借鉴参考。

关键词: 油气成藏, 油水层, 无机地球化学, 油藏地球化学, 成岩作用, 准噶尔盆地

Abstract:

Generally, the identification of oil, gas and water intervals is made mainly through interpreting logging data and sometimes in combination with organic geochemical methods. This, however, often meets large uncertainties when complex petroleum migration and accumulation occur. Consequently, economic loss and exploration risk arise. In order to make an approach to solving this issue in other ways, we made an inorganic geochemical investigation based on the interaction mechanism among reservoir hydrocarbons, water and rocks. The case study in the Luxi area of the central Junggar Basin implied two relatively effective parameters for the identification of oil, gas and water intervals, i.e., diagenetic features of the interaction and the in-situ geochemical composition of representative diagenetic minerals. While the whole-rock geochemical composition of minerals, by contrast, is only a reflection of the average and mixing information on the complex interaction, and thus cannot be used to distinguish different intervals effectively. In the study area, the abundance of hydrocarbons decreases gradually in order of oil, oil-water, water and dry intervals and so does the dissolution related to hydrocarbon charge. Typically, alkaline minerals including calcite and feldspar are dissolved by the action of acidic hydrocarbon-bearing fluid. In addition, the assemblage of diagenetic minerals also varies with different intervals. Kaolinite, kaolinite-pyrite-hematite, siderite-chlorite and chlorite are indicative of the four different intervals, respectively. The abundance of element Mn (an average MnO content) in diagenetic calcites is commonly >2.5%, 2.0%~2.5%, 1.5%~2.0% and <1.0 % for the four intervals, respectively. These parameters could be applied to the regional petroleum exploration, and this approach has also general implications for studies to distinguish oil/gas/water intervals elsewhere.

Key words: hydrocarbon accumulation, oil/water interual, inorganic geochemistry, reservoir geochemistry, diagenesis, Junggar Basin