石油与天然气地质 ›› 2017, Vol. 38 ›› Issue (3): 489-498.doi: 10.11743/ogg20170308

• 油气地质 • 上一篇    下一篇

塔中地区深层寒武系盐下白云岩储层特征及主控因素

倪新锋1,2, 黄理力1,2, 陈永权3, 郑剑锋1,2, 熊益学3, 朱永进1,2, 杨鹏飞3, 李昌1,2   

  1. 1. 中国石油 杭州地质研究院, 浙江 杭州 310023;
    2. 中国石油 碳酸盐岩储层重点实验室, 浙江 杭州 310023;
    3. 中国石油 塔里木油田分公司, 新疆 库尔勒 841000
  • 收稿日期:2015-12-31 修回日期:2017-01-16 出版日期:2017-06-28 发布日期:2017-07-10
  • 作者简介:倪新锋(1978-),男,博士,高级工程师,沉积学与含油气盆地分析。E-mail:nixf_hz@petrochina.com.cn。
  • 基金资助:
    国家科技重大专项(2016ZX05004-002);中国石油股份公司重大科技专项(2014E-32)。

Characteristics and main controlling factors of the Cambrian pre-salt dolomite reservoirs in Tazhong Block,Tarim Basin

Ni Xinfeng1,2, Huang Lili1,2, Chen Yongquan3, Zheng Jianfeng1,2, Xiong Yixue3, Zhu Yongjin1,2, Yang Pengfei3, Li Chang1,2   

  1. 1. Hangzhou Institute of Geology, PetroChina, Hangzhou 310023, China;
    2. Key Laboratory of Carbonate Reservoir, PetroChina, Hangzhou, Zhejiang 310023, China;
    3. Tarim Oilfield Company, PetroChina, Korla, Xinjiang 841000, China
  • Received:2015-12-31 Revised:2017-01-16 Online:2017-06-28 Published:2017-07-10

摘要: 塔中地区东部深层寒武系盐下白云岩勘探取得重大发现,但针对该层系白云岩储层的研究尚属空白。利用钻井、岩心、薄片、扫描电镜、测井及三维地震资料,对塔中寒武系盐下白云岩产层的储层类型、特征、主控因素及展布规律开展探索性研究,认为塔中寒武系盐下白云岩主要发育颗粒滩相白云岩储层和潮坪相膏云岩储层。颗粒滩相白云岩储层主要发育在下寒武统肖尔布拉克组以及中寒武统沙依里克组上段,岩性以台内藻砂屑滩相颗粒白云岩、藻白云岩及粉细晶白云岩为主,明显受岩相控制,形成于准同生期,并受后期层间岩溶作用改造优化。潮坪相膏云岩储层主要发育在中寒武统阿瓦塔格组及沙依里克组下段,岩性以含膏云岩、泥粉晶云岩、膏云质角砾岩为主,明显受岩相及裂缝控制,形成于准同生期,并受后期有机酸溶蚀作用形成微孔型储层。目前而言,下寒武统肖尔布拉克组台内藻砂屑滩相颗粒白云岩储层是最现实的勘探领域。

关键词: 储层特征, 盐下白云岩, 寒武系, 塔中地区, 塔里木盆地

Abstract: Studies on the Cambrian pre-salt dolomite reservoirs is still rare in eastern Tarim Basin,although the exploration there has made great discovery. Research on reservoir types and characteristics,main controlling factors and distributions of the Cambrian pre-salt dolomite reservoirs were presented on the basis of drilling data,cores,thin section SEPM,logging and 3-D seismic data. The results show that grain dolomite reservoir of beach facies and gypsodolomite reservoir of tidal flat facies are two main reservoirs in the pre-salt dolomite of Cambrian in Tazhong Block,Tarim Basin. The former exists in the Lower Cambrian Xiaoerbulake Formation and the Middle Cambrain Upper Shayilike Formation. Lithologies include algae granular dolomite from shoals in platform proximate,algae dolomite and silty crystalline dolomite,and were mainly controlled by facies. The reservoir quality are mostly inherited from deposition and the porosity was improved by the later interlayer Karst processes. The latter mainly exists in the Middle Cambrian Awatage Formation and Middle Cambrain Lower Shayilike Formation. Lithology include gypsiferous dolostone,silty crystalline dolomite,gypsodolomite breccia and they were controlled by both petrography and later fracturing. For its microporous reservoir,the matrix formed during deposition while micropores formed due to later organic acid dissolution. Nowadays,the favorable objectives are most likely to be grain dolomite reservoirs of beach facies in Lower Cambrian Xiaoerbulake Formation.

Key words: reservoir characteristics, pre-salt dolomite, Cambrian, Tazhong Block, Tarim Basin

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