锶同位素在塔河古岩溶期次划分中的应用

张涛; 云露; 邬兴威; 叶德胜

doi:10.11781/sysydz200503299

锶同位素在塔河古岩溶期次划分中的应用

doi: 10.11781/sysydz200503299

1.
中国石化石油勘探开发研究院, 北京, 100083
2. 西北石油局规划院, 乌鲁木齐, 830011
3. 中国地质大学, 北京, 100083

基金项目: “十五”国家科技攻关项目(2003BA613A-03-01).

详细信息

作者简介:
张涛(1973- ),男(汉族),河南南阳人,高级工程师、硕士,主要从事储层评价及油藏描述研究工作.

中图分类号: P597.1
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- 被引次数: 0
出版历程
- 收稿日期: 2004-05-29
- 修回日期: 2005-03-08
- 刊出日期: 2005-05-25

THE APPLICATION OF STRONTIUM ISOTOPES IN DIVISION OF PALEOKARST STAGES IN TAHE OIL FIELD

1.
Research Institute of Exploration & Production, SINOPEC, Beijing 100083, China
2. Design and Planning Institute of Northwest Petroleum Bureau, SINOPEC, Urumqi, Xinjiang 830011, China
3. China University of Geoscience, Beijing 100083, China

摘要

摘要: 塔河油田主要是与不整合面有关的奥陶系碳酸盐岩岩溶缝洞型油藏,储层经历多期岩溶作用的叠加改造,因此岩溶期次的划分识别与不同期次岩溶分布范围的确定对塔河油田下一步勘探至关重要.通过近几年的探索,认为锶同位素比值是区分加里东中期和海西早期岩溶的一种有效方法,其应用原理是,地质历史中的任何时间全球范围内海水的锶同位素组成都是均一的,海水⁸⁷Sr/⁸⁶Sr比值随时间变化.结合塔河地区加里东期与海西早期岩溶地层水中⁸⁷Sr/⁸⁶Sr比值存在差异的地质背景和实验分析数据,可以对塔河古岩溶期次进行识别预测,探讨其分布模式,为塔河油田外扩提供地质依据.
- 锶同位素 /
- 岩溶期次 /
- 塔河油田 /
- 奥陶系
Abstract: Tahe oilfield is an Ordovician carbonate rock fissure vug oil pool which is mainly related to unconformity.Its reservoir rock is reformed by superimposition of multistages karstification,so it is very important to identify paleo-karstification stages and confirm distribution of different stage of karstfication reservoir for further exploration.Through recent years exploration,it is thought that the ratio of ⁸⁷Sr/⁸⁶Sr is an effective indicator distingishing middle Caledonian stage of karstification reservoir from early Hercynian stage of karstification reservoir.Its theory is that strontium isotope composition in the global ocean water at any one time in geologic history is homogeneous,that is,⁸⁷Sr/⁸⁶Sr value in ocean water changes timely.Combined with the geological setting that ⁸⁷Sr/⁸⁶Sr value in Caledonian stage of karstification reservoir is different from ⁸⁷Sr/⁸⁶Sr value in Hercynian stage of karstification reservoir and the experimental data,Pa-leokarstification reservoir stages is identified and predicted,and distribution pattern in Tahe oilfield is discussed in the paper,which provides geological evidence for further petroleum exploration in Tahe oilfield.
- Strontium isotope /
- Paleo-karstification stages /
- Tahe oilfield /
- Ordovician

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参考文献(15)

[1]	向芳,王成善.锶同位素在沉积学中的应用新进展[J].地质地球化学,2001,29(1):79～82
[2]	郑荣才,陈洪德,张哨楠.川东黄龙组古岩溶储层的稳定同位素和流体性质[J].地球科学-中国地质大学学报,1997,22(4):424～428
[3]	王敦则,黎玉战,俞仁连.塔里木盆地塔河油田下奥陶统油藏特征及成藏条件分析[J].石油实验地质,2003,25(2):122～128
[4]	顾忆.塔里木盆地北部塔河油田油气藏成藏机制[J].石油实验地质,2000,22(4):307～311
[5]	闫相宾,韩振华,李永宏.塔河油田奥陶系油藏的储层特征和成因机理探讨[J].地质论评,2002,48(6):619～626
[6]	王恕一.塔里木盆地塔河油田下奥陶统碳酸盐岩的深埋溶蚀作用及其对储集体的影响[J].石油实验地质,2003,25(增刊):557～561
[7]	蔡立国,钱一雄,刘光祥等.塔河油田及邻区地层水成因探讨[J].石油实验地质,2002,24(1):57～60
[8]	Wickman F E.Isotope rations:a clue to the age of certain marine sediments[J].Geol,1948,(56):61～66
[9]	Hodell D A,Mead G A,Mueller P A.Varition in the strontium isotopic composition of seawater (8Ma to present):implications for chemical weathering rates and dissolved fluxes to the ocaens[J].Chen Geo (Isot Geosci Sect),1990,(80):291～307
[10]	黄思静,石和,刘杰等.锶同位素地层学研究进展[J].地球科学进展,2001,16(2):194～200
[11]	Palmer MR,Elderfield H.Sr isotopic composition of sea water over the past 75 a[J].Naturre,1985,314:526～528
[12]	Raymo M E,Ruddiman W F.Tectonic forcingg of late Cenozonic climate[J].Nature,1992,359:117～122
[13]	刘文,李永宏,张涛.塔河油田奥陶系碳酸盐岩沉积相及地层学研究[J].石油实验地质,2002,24(2):104～109
[14]	叶德胜,王根长,林忠民等.塔里木盆地北部寒武-奥陶系碳酸盐岩储层特征及油气前景[M].成都:四川大学出版社,2000.50～51
[15]	马红强.盐水包裹体在成岩作用中的应用-以塔河油田下奥陶统碳酸盐岩为例[J].石油实验地质,2003,25(增刊):601～606