塔东地区英东2井寒武系-奥陶系储层流体地球化学示踪

doi:10.11743/ogg20120607

石油与天然气地质 ›› 2012, Vol. 33 ›› Issue (6): 867-876.doi: 10.11743/ogg20120607

塔东地区英东2井寒武系-奥陶系储层流体地球化学示踪

王东¹, 王国芝^2,3, 刘树根², 丁代淑⁴

1. 中国石化西南油气分公司勘探开发研究院海相所,贵州贵阳 550004;
2. 成都理工大学油气藏地质及开发工程国家重点实验室,四川成都 610059;
3. 成都理工大学地球科学学院,四川成都 610059;
4. 中国石油新疆油田公司石西油田作业区,新疆克拉玛依 834000

收稿日期:2011-07-15 修回日期:2012-09-19 出版日期:2012-12-28 发布日期:2013-01-10
作者简介:王东(1981—),男,硕士,石油地质。
基金资助:
国家重点基础研究发展规划("973"计划)项目(2005CB422106)。

Geochemical tracing of the Cambrian-Ordovician reservoir fluid in Well Yingdong-2,eastern Tarim Basin

Wang Dong¹, Wang Guozhi^2,3, Liu Shugen², Ding Daishu⁴

1. Marine Facies Academy of Exploration & Development Research Institute, Southwest Branch Company, SINOPEC, Guiyang, Guizhou 550004, China;
2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Techno-logy, Chengdu, Sichuan 610059, China;
3. College of Earth Sciences, Chengdu University of Technology, Chengdu, Sichuan 610059, China;
4. Shixi Oil Block, Xinjiang Oil Company, PetroChina, Karamay, Xinjiang 834000, China

Received:2011-07-15 Revised:2012-09-19 Online:2012-12-28 Published:2013-01-10

摘要/Abstract

摘要：

系统分析了英东2井中、上寒武统和中、下奥陶统围岩及裂缝中充填物的碳、氧、锶同位素、稀土元素及流体包裹体等地球化学特征。在此基础上,根据示踪流体的形成期次、来源,划分流体充注的时序关系,探讨流体对储层改造的影响,进而对油气动态保存条件进行探索性评价。流体地球化学研究表明,中、上寒武统和中、下奥陶统存在3期外来壳源富锶流体,其中第一期流体的⁸⁷Sr/⁸⁶Sr比值为0.710 8,第二期流体的⁸⁷Sr/⁸⁶Sr比值介于0.709 8～0.710 0,最晚一期为来自地壳深部的热液流体,其⁸⁷Sr/⁸⁶Sr比值为0.713 8。3期流体对储层的储集性能均起到了破坏性作用,但晚期热液流体在对储层改造的同时具有一定的建设性作用。最早一期流体充注时,中、上寒武统储层具有相对较好的油气保存条件;随后两期流体充注时,中、上寒武统储层不再具有保存油气的能力。流体地球化学示踪为动态了解英东构造带乃至整个塔东地区深部流体活动提供了一个新方法。

关键词: 稀土元素, 流体包裹体, 地球化学示踪, 储层流体, 英东2井, 寒武系, 奥陶系, 塔东地区

Abstract:

The isotopes of carbon,oxygen and strontium,REE,and the geochemical features of the fluid inclusions in the Middle-Upper Cambrian and Middle-Lower Ordovician side-beds and fracture fillings of the well Yingdong-2 were systematically analyzed.Based on the results,we traced phases and sources of the reservoir fluids,determined chronogenesis of fluid charging,explored the impact of the fluids upon reservoir modification and discussed the dynamic preserving conditions for oil and gas in such settings.The geochemical study of the fluids suggests that there are three charging phases of allogenic fluids with abundant Sr from the crust in the Middle-Upper Cambrian and Middle-Lower Ordovician .The fluids charged in the first phase have a ⁸⁷Sr/⁸⁶Sr ratio of 0.710 8,the fluids charged in the second phase have a ⁸⁷Sr/⁸⁶Sr ratio in the range of 0.709 8-0.710 0,and the fluids charged in the last phase are hydrothermal fluid from the deep crust and have a ⁸⁷Sr/⁸⁶Sr ratio of 0.713 8.The fluids charged in these three phases all played a destructive role in the forming of reservoirs,but the hydrothermal fluids charged in the last phase were constructive to the reservoir formation.The Middle-Upper Cambrian reservoirs had relatively better hydrocarbon preserving conditions during the first phase of fluid charging,but lost them when the second and the third phase occurred.Geochemical tracing of fluids provides a new method for dynamic evaluation of deep fluid activities in the Yingdong tectonic belt as well as the whole eastern Tarim Basin.

Key words: REE, fluid inclusion, geochemical tracing, reservoir fluid, Well Yingdong-2, Cambrian, Ordovician, eastern Tarim Basin

中图分类号:

TE122.1

王东,王国芝,刘树根,等. 塔东地区英东2井寒武系-奥陶系储层流体地球化学示踪[J]. 石油与天然气地质, 2012, 33(6): 867-876. doi: 10.11743/ogg20120607 Wang Dong,Wang Guozhi,Liu Shugen,et al. Geochemical tracing of the Cambrian-Ordovician reservoir fluid in Well Yingdong-2,eastern Tarim Basin[J]. Oil & Gas Geology, 2012, 33(6): 867-876. doi: 10.11743/ogg20120607

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塔东地区英东2井寒武系-奥陶系储层流体地球化学示踪

Geochemical tracing of the Cambrian-Ordovician reservoir fluid in Well Yingdong-2,eastern Tarim Basin

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