玛湖地区三叠系克拉玛依组优质砂砾岩储层形成机制

doi:10.12108/yxyqc.20200308

岩性油气藏 ›› 2020, Vol. 32 ›› Issue (3): 82–92.doi: 10.12108/yxyqc.20200308

玛湖地区三叠系克拉玛依组优质砂砾岩储层形成机制

徐子煜¹, 王安², 韩长城¹, 田继军¹, 张军生¹, 刘磊¹, 张楠¹

1. 新疆大学地质与矿业工程学院, 乌鲁木齐 830046;
2. 中国石油测井有限公司华北事业部, 河北任丘 062550

收稿日期:2019-09-19 修回日期:2019-10-23 出版日期:2020-05-21 发布日期:2020-04-30
第一作者:徐子煜(1994-),男,新疆大学在读硕士研究生,研究方向为沉积地质与石油地质。地址:(830046)新疆乌鲁木齐市天山区新疆大学地质与矿业工程学院。Email:811326475@qq.com
通信作者: 韩长城(1984-),男,博士,硕士生导师,主要从事沉积地质与油气地质方面的教学与研究工作。Email:hanchangchen@126.com。
基金资助:
新疆维吾尔自治区天山英才第二期项目“新疆北部侏罗纪巨厚煤层的煤岩特征与煤相演替”（编号：2016-178）资助

Formation mechanism of high-quality sandy-conglomerate reservoir of Triassic Karamay Formation in Mahu area

XU Ziyu¹, WANG An², HAN Changcheng¹, TIAN Jijun¹, ZHANG Junsheng¹, LIU Lei¹, ZHANG Nan¹

1. College of Geology and Mining Engineering, Xinjiang University, Urumqi 830046, China;
2. North China Business Department of Well Logging Co., Ltd., CNPC, Renqiu 062550, Hebei, China

Received:2019-09-19 Revised:2019-10-23 Online:2020-05-21 Published:2020-04-30

摘要/Abstract

摘要： 为明确准噶尔盆地玛湖地区三叠系克拉玛依组优质砂砾岩储层的形成机制，开展了岩心观察、薄片鉴定、测井资料分析、压汞和物性测试和扫描电镜分析，并对优质储层的平面分布和成岩演化进行了综合研究。结果表明：①玛湖地区三叠系克拉玛依组主要为辫状河三角洲相和扇三角洲相沉积，其中分流河道砂砾岩、坝体以及席状砂为主要储集层；② 3种储集体相互叠置，其中在三角洲前缘亚相的水下分流河道砂体发育削截式河道构型和完整式河道构型，储层厚度最大，粒度最粗，储集性最好，而席状砂以粉砂岩为主，厚度较薄，粒度较细，储集性相对较差；③成岩环境对储层孔隙演化具有一定的控制作用，成岩晚期发生的绿泥石沉淀和方解石胶结作用降低了储层物性，从而形成了现今的低孔-特低渗型储层。该研究成果对玛湖地区三叠系克拉玛依组油气勘探具有指导意义。

关键词: 砂砾岩储层, 沉积展布, 成岩环境, 优质储层, 三叠系, 玛湖地区

Abstract: In order to clarify the formation mechanism of high-quality sandy-conglomerate reservoir of Triassic Karamay Formation in Mahu area of Junggar Basin,core observation,thin section identification,logging data analysis,mercury injection and physical property measurement and scanning electron microscope analysis were carried out,meanwhile the plane distribution and diagenetic evolution of high-quality reservoir were studied comprehensively. The results show that:(1) The Karamay Formation in Mahu area is mainly composed of braided river delta facies and fan delta facies,in which distributary channel conglomerates,dam bodies and sheet sands are the main reservoirs.(2) Three kinds of reservoirs are superposed with each other. The underwater distributary channel sands in delta front subfacies develop truncated river channel sand body and multiple sedimentary composite sand body,with the largest reservoir thickness,the coarsest grain size and the best reservoir properties, while sheet sand is mainly siltstone,with thin reservoir thickness,fine grain size and relatively poor reservoir properties.(3) Diagenetic environment has a certain control over the evolution of reservoir pores. The chlorite precipitation and calcite cementation in the late diagenetic stage reduced the reservoir physical properties,thus forming the present low porosity and ultra-low permeability reservoir. The research results have guiding significance for oil and gas exploration of Karamay Formation in Mahu area.

Key words: sandy-conglomerate reservoir, sedimentary distribution, diagenetic environment, high-quality reservoir, Triassic, Mahu area

中图分类号:

TE122

徐子煜, 王安, 韩长城, 田继军, 张军生, 刘磊, 张楠. 玛湖地区三叠系克拉玛依组优质砂砾岩储层形成机制[J]. 岩性油气藏, 2020, 32(3): 82–92.

XU Ziyu, WANG An, HAN Changcheng, TIAN Jijun, ZHANG Junsheng, LIU Lei, ZHANG Nan. Formation mechanism of high-quality sandy-conglomerate reservoir of Triassic Karamay Formation in Mahu area[J]. Lithologic Reservoirs, 2020, 32(3): 82–92.

参考文献

[1] AMTHOR J E,OKKERMAN J. Influence of early diagenesis on reservoir quality of Rotliegende sandstones,northern Netherlands. AAPG Bulletin,1988,82(12):2246-2265.
[2] 杨帆,曹正林,卫延召,等.玛湖地区三叠系克拉玛依组浅水辫状河三角洲沉积特征.岩性油气藏,2019,31(1):30-39. YANG F,CAO Z L,WEI Y Z,et al. Sedimentary characteristics of shallow-water braided delta of Karamay Formation in Mahu area. Lithologic Reservoirs,2019,31(1):30-39.
[3] 唐勇,徐洋,李亚哲,等.玛湖凹陷大型浅水退覆式扇三角洲沉积模式及勘探意义.新疆石油地质,2018,39(1):16-22. TANG Y,XU Y,LI Y Z,et al. Sedimentary model and exploration significance of large-scaled shallow retrogradation fan delta in Mahu depression. Xinjiang Petroleum Geology,2018,39(1):16-22.
[4] 单祥,邹志文,孟祥超,等.准噶尔盆地环玛湖地区三叠系百口泉组物源分析.沉积学报,2016,34(5):930-939. SHAN X,ZOU Z W,MENG X C,et al. Provenance analysis of Triassic Baikouquan Formation in the area around Mahu Depression,Junggar Basin. Acta Sedimentologica Sinica,2016,34(5):930-939.
[5] 谭开俊,王国栋,罗惠芬,等.准噶尔盆地玛湖斜坡区三叠系百口泉组储层特征及控制因素.岩性油气藏,2014,26(6):83-88. TAN K J,WANG G D,LUO H F,et al. Reservoir characteristics and controlling factors of the Triassic Baikouquan Formation in Mahu slope area,Junggar Basin. Lithologic Reservoirs, 2014,26(6):83-88.
[6] 陈启林,黄成刚.沉积岩中溶蚀作用对储集层的改造研究进展.地球科学进展,2018,33(11):1112-1129. CHEN Q L,HUANG C G. Research progress of modification of reservoirs by dissolution in sedimentary rock. Advances in Earth Science,2018,33(11):1112-1129.
[7] 崔明明,李进步,王宗秀,等.辫状河三角洲前缘致密砂岩储层特征及优质储层控制因素:以苏里格气田西南部石盒子组8段为例.石油学报,2019,40(3):279-294. CUI M M,LI J B,WANG Z X,et al. Characteristics of tight sand reservoir and controlling factors of high-quality reservoir at braided delta front:a case study from Member 8 of Shihezi Formation in southwestern Sulige gas field. Acta Petrolei Sinica, 2019,40(3):279-294.
[8] 何文祥,吴胜和,唐义疆,等.河口坝砂体构型精细解剖.石油勘探与开发,2005,32(5):42-46. HE W X,WU S H,TANG Y J,et al. Detailed architecture analyses of debouch bar in Shengtuo Oilfield,Jiyang Depression. Petroleum Exploration&Development,2005,32(5):42-46.
[9] 赵伦,梁宏伟,张祥忠,等.砂体构型特征与剩余油分布模式:以哈萨克斯坦南图尔盖盆地Kumkol South油田为例.石油勘探与开发,2016,43(3):433-441. ZHAO L,LIANG H W,ZHANG X Z,et al. Relationship between sandstone architecture and remaining oil distribution pattern:a case of the Kumkol South oilfield in South Turgay Basion,Kazakstan. Petroleum Exploration&Development,2016, 43(3):433-441.
[10] 金振奎,杨有星,尚建林,等.辫状河砂体构型及定量参数研究:以阜康、柳林和延安地区辫状河露头为例.天然气地球科学,2014,25(3):311-317. JIN Z K,YANG Y X,SHANG J L,et al. Sandbody architecture and quantitative parameters of single channel sandbodies of braided river:Cases from outcrops of braided river in Fukang, Liulin and Yan'an area. Natural Gas Geoscience,2014,25(3):311-317.
[11] 林畅松,施和生,李浩,等.南海北部珠江口盆地陆架边缘斜坡带层序结构和沉积演化及控制作用.地球科学,2018,43(10):3407-3422. LIN C S,SHI H S,LI H,et al. Sequence architecture,depositional evolution and controlling processes of continental slope in Pearl River Mouth Basin,Northern South China Sea. Earth Science,2018,43(10):3407-3422.
[12] 李欢,邹灏,李欣宇,等.准噶尔盆地东缘中侏罗统头屯河组层序地层与沉积演化.沉积与特提斯地质,2018,38(1):41-52. LI H,ZOU H,LI X Y,et al. Sequence stratigraphy and sedimentary evolution of the Middle Jurassic Toutunhe Formation on the eastern margin of the Junggar Basin,Xinjiang. Sedimentary Geology and Tethyan Geology,2018,38(1):41-52.
[13] 张善文,袁静,隋风贵,等.东营凹陷北部沙河街组四段深部储层多重成岩环境及演化模式.地质科学,2008,43(3):576-587. ZHANG S W,YUAN J,SUI F G,et al. Multiple diagenetic environments and evolvement model in deep formation of the 4 th member,Shahejie Formation in the northern Dongying Sag. Chinese Journal of Geology,2008,43(3):576-587.
[14] 李兴,张立强,施辉,等.准噶尔盆地玛湖凹陷百口泉组沉积古环境分析:以玛18井为例.岩性油气藏,2016,28(2):80-85. LI X,ZHANG L Q,SHI H,et al. Sedimentary environment of Lower Triassic Baikouquan Formation in Mahu Sag,Junggar Basin:a case study from Ma 18 well. Lithologic Reservoirs, 2016,28(2):80-85.
[15] 李振华.准噶尔盆地中拐地区佳木河组沉积特征与成岩环境研究.青岛:中国石油大学(华东),2014. LI Z H. The research of sedimentary characteristics and diagenetic environment in Permian Jiamuhe Formation of Zhongguai area in the Junggar Basin. Qingdao:China University of Petroleum (East China),2014.
[16] 秦伟军,谈风其,毛根塔.松辽盆地梨树断陷天然气优质储层的空间类型与形成机理.西安石油大学学报(自然科学版), 2019,34(4):1-7. QIN W J,TAN F Q,MAO G T. Spatial types and formation mechanisms of high-quality natural gas reservoirs in Lishu fault depression,Songliao Basin. Journal of Xi'an Shiyou University (Natural Science Edition),2019,34(4):1-7.
[17] 陈淦.克拉玛依油田储集层中的沸石矿物及其与油气关系.石油学报,1992,13(3):49-56. CHEN G. Zeolite minerals and their relation to oil and gas accumulation in the reservoir formations in Karmay Oilfield. Acta Petrolei Sinica,1992,13(3):49-56.
[18] 邵淑骁,曾溅辉,张善文,等.东营凹陷沙河街组砂岩储层高岭石类型、特征及其成因.沉积学报,2015,33(6):1204-1216. SHAO S X,ZENG J H,ZHANG S W,et al. Types,characteristics and origin of kaolinite in sandstone reservoir of Shahejie Formation,Dongying Sag. Acta Sedimentologica Sinica,2015,33(6):1204-1216.
[19] 谢渊,王剑,李令喜,等.鄂尔多斯盆地白垩系黏土矿物的分布特征及其沉积-成岩环境意义.地质通报,2010,29(1):93-104. XIE Y,WANG J,LI L X,et al. Distribution of the Cretaceous clay minerals in Ordos Basin,China and its implication to sedimentary and diagenetic environment. Geological Bulletin of China,2010,29(1):93-104.
[20] YE D. Porosity of accumulation stage:an important evidence for evaluating evaluating hydrocarbon reservoirs. Oil & Gas Geology,1986,7(3):218-223.
[21] 蔡进功,谢忠怀,田芳,等.济阳坳陷深层砂岩成岩作用及孔隙演化.石油与天然气地质,2002,23(1):84-88. CAI J G,XIE Z H,TIAN F,et al. Diagenesis and pore evolution of deep sandstone in Jiyang Depression. Oil & Gas Geology, 2002,23(1):84-88.
[22] 刘锐娥,孙粉锦,拜文华,等.苏里格庙盒8气层次生孔隙成因及孔隙演化模式探讨.石油勘探与开发,2002,29(4):47-49. LIU R E,SUN F J,BAI W H,et al. An approach to the generating mechanism of secondary pores and pore evolution model of He 8 gas layer in Suligemiao gas field. Petroleum Exploration&Development,2002,29(4):47-49.
[23] 邹志文,李辉,徐洋,等.准噶尔盆地玛湖凹陷下三叠统百口泉组扇三角洲沉积特征.地质科技情报,2015(2):20-26. ZOU Z W,LI H,XU Y,et al. Sedimentary characteristics of the Baikouquan Formation,Lower Triassic in the Mahu Depression,Junggar Basin. Geological Science and Technology Information,2015(2):20-26.
[24] BEARD D C,WEYL P K. Influence of texture on porosity and permeability of unconsolidated sand. AAPG Bulletin,1973,57(2):349-369.
[25] 袁剑英,黄成刚,夏青松,等.咸化湖盆碳酸盐岩储层特征及孔隙形成机理:以柴西地区渐新统下干柴沟组为例.地质论评,2016,62(1):111-126. YUAN J Y,HUANG C G,XIA Q S,et al. The characteristics of carbonate reservoir,and formation mechanism of pores in the saline lacustrine basin:a case study of the lower Eocene ganchaigou formation in western Qaidam Basin. Geological Review,2016,62(1):111-126.

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玛湖地区三叠系克拉玛依组优质砂砾岩储层形成机制

Formation mechanism of high-quality sandy-conglomerate reservoir of Triassic Karamay Formation in Mahu area

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