孟祥超;徐洋;韩守华;陈能贵;邹志文;郭华军;

• 1:中国石油杭州地质研究院

摘要(Abstract)：

为明确中拐地区上乌尔禾组浊沸石胶结物展布规律及其与产能的关系,指导中拐地区优质储层预测,分析铸体薄片、黏土矿物、试油结果及区域地层展布.结果表明:中拐地区上乌尔禾组储层以浊沸石胶结为主,且与溶孔含量及产能呈正相关,存在可多保留3%～8%的孔隙度.浊沸石分布受控于砂体沉积微相类型、距P2w碱性水介质源距离,平面上主要发育在湖岸线附近及水下扇三角洲前缘相带,垂向上主要分布于叠置的主河道砂体内.JL2-J205一线以东的水下分流河道区带浊沸石较发育,靠近酸源凹陷有通源断裂沟通,为浊沸石溶孔优质储层发育区,钻探油气显示良好,勘探潜力巨大.

关键词(KeyWords)：中拐地区;上乌尔禾组(P3w);浊沸石;主河道;分支河道;河口坝

Abstract:

Keywords:

基金项目(Foundation):中国石油股份公司勘探生产分公司专项(2012ZX0716-02)

作者(Author):孟祥超;徐洋;韩守华;陈能贵;邹志文;郭华军;

Email:

参考文献(References)：

• [1]李丕龙,冯建辉,陆永潮,等.准噶尔盆地构造沉积与成藏[M].北京:地质出版社,2010.Li Pilong,Feng Jianhui,Lu Yongchao,et al.Structure,sedimentation and reservoir in Junggar basin[M].Beijing:Geology Press,2010.

• [2]雷振宇,卞德智.准噶尔盆地西北缘扇体形成特征及油气分布规律[J].石油学报,2005,26(1):8-12.Lei Zhenyu,Bian Dezhi.Characteristics of fan forming and oil-gas distribution in north western margin of Junggar basin[J].Acta Pe-trolei Sinica,2005,26(1):8-12.

• [3]雷振宇,鲁兵,蔚远江,等.准噶尔盆地西北缘构造演化与扇体形成和分布[J].石油与天然气地质,2005,26(1):86-91.Lei Zhenyu,Lu Bing,Wei Yuanjiang,et al.Tectonic evolution and development and distribution of fans on northwestern edge ofJunggar basin[J].Oil&Gas,2005,26(1):86-91.

• [4]宋永东,戴俊生,吴孔友.准噶尔盆地西北缘乌夏断裂带构造特征与油气成藏模式[J].西安石油大学学报:自然科学版,2009,24(3):17-24.Song Yongdong,Dai Junsheng,Wu Kongyou.Study on the structural features and hydrocarbon accumulation modes of Wuxia faultbelt in the northwest margin of Junggar basin[J].Joumal of Xi'an Shiyou University:Natural Science Edition,2009,24(3):17-24.

• [5]李军,王炜,王书勋.青西油田沉凝灰岩储集特征[J].新疆石油地质,2006,27(3):288-289.Li Jun,Wangwei,Wang Shuxun.Reservoir feature of congeal-limestone in Qingxi oilfield[J].Xinjiang Petroleum Geology,2006,27(3):288-289.

• [6]陈奋雄,李军,师志龙,等.准噶尔盆地西北缘车—拐地区三叠系沉积相特征[J].大庆石油学院学报,2012,36(2):23-26.Chen Fenxiong,Li Jun,Shi Zhilong,et al.Sedimentary facies feature of triassic in Cheguai region,northwestern of Junggar basin[J].Journal of Daqing Petroleum Institute,2012,36(2):23-26.

• [7]杨晓萍,张宝民,雷振宇,等.含油气盆地中浊沸石的形成与分布及其对油气勘探的意义[J].石油地质,2006(2):35-37.Yang Xiaoping,Zhang Baomin,Lei Zhenyu,et al.Formation process and distribution and its exploration significance of laumontite inoil&gas basin[J].Petroleum Geology,2006(2):35-37.

• [8]卢文忠,朱国华,李大成,等.川中地区侏罗系下沙溪庙组浊沸石砂岩储层的发现及意义[J].沉积储层,2004(5):54-56.Lu Wenzhong,Zhu Guohua,Li Dacheng,et al.Discovery and significance of laumontite reservoir in J2x,Chuanzhong region[J].Deposition and Reservoir,2004(5):54-56.

• [9]肖序常,汤耀庆.新疆北部大地构造特征[M].北京:地质出版社,2008.Xiao Xuchang,Tang Yaoqing.Tectonic feature in northern Xinjiang[M].Beijing:Geology Press,2008.

• [10]梁云海,李文铅.新疆准噶尔造山带多旋回开合构造特征[J].地质通报,2008,23:279-285.Liang Yunhai,Li Wenqian.Tectonic feature of multi circle open-close in orogenetic region,Junggar basin[J].Geology Circular,2008,23:279-285.

• [11]管树巍,李本亮,侯连华,等.准噶尔盆地西北缘下盘掩伏构造油气勘探新领域[J].石油勘探与开发,2008,35(1):17-22.Guan Shuwei,Li Benliang,Hou Lianhua,et al.New hydrocarbon exploration areas in footwall covered structures in northwesternmargin of Junggar basin[J].Petroleum Exploration and Development,2008,35(1):17-22.

• [12]范存辉,支东明,秦启荣,等.准噶尔盆地小拐地区佳木河组储层特征及主控因素[J].大庆石油学院学报,2012,36(2):48-51.Fan Cunhui,Zhi Dongming,Qin Qirong,et al.Reservoir feature and master control factor of P1jin Xiaoguai region,Junggar basin[J].Journal of Daqing Petroleum Institute,2012,36(2):48-51.

• [13]况军,齐雪峰.准噶尔前陆盆地构造特征与油气勘探方向[J].新疆石油地质,2006,27(1):5-9.Kuang Jun,Qi Xuefeng.The structural characteristics and oil-gas explorative direction in Junggar foreland basin[J].Xinjiang Petro-leum Geology,2006,27(1):5-9.

• [14]刘海涛,蒲秀刚,张光亚,等.准噶尔盆地白家海地区侏罗系扇三角洲沉积体系[J].大庆石油学院学报,2010,34(6):38-40.Liu Haitao,Pu Xiugang,Zhang Guangya,et al.Fan-delta sedimentary system of jurassic in Baijiahai region,Junggar basin[J].Journal of Daqing Petroleum Institute,2010,34(6):38-40.

• [15]伊振林,回琇,张保国,等.克拉玛依油田六中区克下组沉积微相分析[J].大庆石油学院学报,2011,35(6):24-26.Yi Zhenlin,Hui Xiu,Zhang Baoguo,et al.Sedimentary facies analysis of T2k1in middle 6th district,Kelamay oilfield[J].Journal ofDaqing Petroleum Institute,2011,35(6):24-26.

• [16]杨晓萍,裘怿楠.鄂尔多斯盆地上三叠统延长组浊沸石形成机理、分布规律与油气关系[J].沉积学报,2002,20(4):630-632.Yang Xiaoping,Qiu Yinan.Formation process and distribution of laumontite in Yanchang formation upper triassic of Ordos basin[J].Acta Sedimentologica Sinica,2002,20(4):630-632.

• [17]白清华,柳益群,樊婷婷.鄂尔多斯盆地上三叠统延长组浊沸石分布及其成因分析[J].西北地质,2009,42(2):102-105.Bai Qinghua,Liu Yiqun,Fan Tingting.Distribution and formation process of laumontite in Yanchang formation(upper triassic),Ordos basin[J].Northwestern Geology,2009,42(2):102-105.

• [18]曾广策,朱云海,叶德隆.晶体光学及光性矿物学[M].北京:中国地质大学出版社,2008.Zeng Guangce,Zhu Yunhai,Ye Delong.Crystal optics and light-nature mineralogy[M].Beijing:Geology University of China Press,2008.

• [19]吴海瑞.松辽盆地乾北地区青三段沉积微相发育特征及其对岩性油藏的控制作用[J].大庆石油学院学报,2011,35(4):9-11.Wu Hairui.Development feature of sedimentary facies and its control to lithology reservoir in Qing 3th group,Qianbei region ofSongliao basin[J].Journal of Daqing Petroleum Institute,2011,35(4):9-11.