Natural Gas Geoscience ›› 2019, Vol. 30 ›› Issue (11): 1551-1559.doi: 10.11764/j.issn.1672-1926.2019.07.019

Previous Articles     Next Articles

Characteristic of provenance and their control over sand bodies in Shahezi Formation of Xujiaweizi fault depression, Songliao Basin

Xue-zhen Liu1(),Xue-yan Wang1,An-ning Zhong2,Ying-chun Yang1,Shi-xiang Zhang2,Xiang Zhou2   

  1. 1. The 1st Geophysical Exploration Company in Daqing, Bureau of Geophysical Prospecting, Daqing 163000, China
    2. Exploration and Production Research Institute, Daqing Oilfield Company, Daqing 163712, China
  • Received:2019-04-15 Revised:2019-07-24 Online:2019-11-10 Published:2019-12-03

Abstract:

The characteristic of parent rock in different tectonic unit was investigated according to the composition of clastic rock, heavy mineral and conglomerate. The main direction of different tectonic units was established based on special reflection analysis, and their impacts on the distribute and quality of sand bodies were clarified. The result is that, the parent rock in Anda area is mainly acid volcanic rock which comes from Anda Sag, and the parent rock in Xuxi Depression is mainly acid and intermediate-basic volcanic rock which comes from the central uplift. The parent rock in Songzhan area and Xudong Depression is intermediate-basic volcanic and metamorphic rocks that comes from Xudong slop. The scale of provenance in sleep slop such as Anda area and Xuxi Depression is less than that in gentle slope belt such as Songzhan area and Xudong Depression, therefore, the sedimentary facies in Anda area and Xuxi Depression are small fan delta which was developed along with Xuxi fault, and isolated from the other. While the sedimentary facies in Songzhan area and Xudong Depression is braided river delta in large scale, with a small thickness and wide area. The size of sandstone in sleep slop are greater than that in gentle slope belt, which makes the sandstone have a stronger ability to resist the compaction, and lots of primary pores can be reserved at a higher burial depth, while for the sandstone in gentle slope belt with a greater content of rock debris and smaller size, in that case, a great deal of porosity have been lost because of serious compact and primary pore can hardly be found in gentle slope belt. But organic acids get into reservoir and corrode rock debris, generate masses of dissolution pores which is the key factor why quality of sandstone in gentle slope belt is higher than that in sleep slope.

Key words: Provenance analysis, Heavy mineral, Sedimentary system, Shahezi Formation, Xujiaweizi fault depression

CLC Number: 

  • TE122.1

Fig.1

Tectonic area distribute of Xujiaweizi fault depression"

Fig.2

The type of sandstone in difference tectonic unit of Xujiaweizi fault depression"

Table 1

Compose of detrital mineral and conglomerate in different tectonic unit of Xujiaweizi fault depression"

构造单元碎屑矿物组合/%变质岩/个岩浆岩/个沉积岩/个
石英长石岩屑流纹岩英安岩安山岩玄武岩

安达

地区

12~3624.30(31)10~4328.39(31)18~5547.31(31)2~239(15)1~134.4(15)0~71.4(15)0~82.4(15)0~229(15)0~112.4(15)

宋站

地区

10~6024.20(40)7~3322.95(40)26~6652.84(40)0~146.25(21)1~136.75(21)0~134.75(21)0~269.25(21)0~41.75(21)0~62.5(21)

徐西

凹陷

3~2821.34(35)12~3632.51(35)17~5846.14(35)0~193.22(31)1~2347.31(31)0~339.56(31)5~4817.22(31)0~41.22(31)

徐东

凹陷

5~4427.78(65)12~4921.11(65)25~6251.11(65)0~319.2(17)0~4914.2(17)0~9224.2(17)0~14137.6(17)0~20.8(17)0~92.4(17)

Fig.3

Characteristic of heavy mineral assemblages in difference tectonic unit of Xujiaweizi fault depression"

Fig.4

The typical source response seismic reflection structure profile and incised valley characteristics in Xujiaweizi fault depression(profile position is shown in Fig.5)"

Fig.5

Distribute of incised valley and sedimentary facies from SQ2 in Shahezi Formation in Xujiaweizi fault depression"

Fig.6

Contour of ZTR index from Shahezi Formation in Xujiaweizi fault depression"

Fig.7

Sedimentary profile of Shahezi Formation fromWell DS401 to Well S3 in Xujiaweizi fault depression(profile position is shown in Fig.5)"

Fig.8

Sedimentary facies of Well Dashen 4(a) Well and Songshen 4(b) in Xujiaweizi fault depression"

Fig.9

Relationship between cement and interstitial volume in difference tectonic unit of Xujiaweizi fault depression"

Fig.10

Relationship between porosity and burial depth in difference tectonic unit of Xujiaweizi fault depression"

1 WangMin,SunYefeng,WangWenguang,et al.Gas generation characteristics and resource potential of the deep source rock in Xujiaweizi fault depression,northern Songliao Basin[J].Natural Gas Geoscience,2014,25(7):1011-1018.
王民,孙业峰,王文广,等.松辽盆地北部徐家围子断陷深层烃源岩生气特征及天然气资源潜力[J].天然气地球科学,2014,25(7):1011-1018.
2 CaiQuansheng,HuMingyi,HuZhonggui,et al.Sedimentary filling evolution of small-scale lake basins during intensive faulting: An example from the Shahezi Formation of Songzhan region in Xujiaweizi fault depression,Songliao Basin[J].Oil & Gas Geology,2017,38(2):975-984.
蔡全升,胡明毅,胡忠贵,等.强烈断陷期小型湖盆沉积充填演化特征——以松辽盆地徐家围子断陷宋站地区沙河子组为例[J].石油与天然气地质,2017,38(2):975-984.
3 SuChaoguang,ZhongWeiping.An analysis on the provenance of the Neogene Shawan Formation in the Chepaizi Uplift of the Junggar Basin[J].Oil & Gas Geology,2010,31(5):648-655.
苏朝光,仲维萍.准噶尔盆地车排子凸起新近系沙湾组物源分析[J].石油与天然气地质,2010,31(5):648-655.
4 ZhaoHongge,LiuChiyang. Approaches and prospects of provenance analysis[J].Acta Sedimentologica Sinica, 2003,21(3):409-415.
赵红格,刘池洋.物源分析方法及研究进展[J].沉积学报,2003,21(3):409-415.
5 BaiXuefeng,LiangJiangping,ZhangWenjing,et al.Geologic conditions, resource potential and exploratory direction of deep gas in the northern Songliao Basin[J].Natural Gas Geoscience, 2018,29(1):1443-1454.
白雪峰,梁江平,张文婧,等.松辽盆地北部深层天然气地质条件、资源潜力及勘探方向[J].天然气地球科学,2018,29(1):1443-1454.
6 YangHua,LiuZiliang,ZhuXiaomin,et al.Provenance and depositional systems of the Upper Trassic Yanchang Formation in the southweastern Ordos Basin,China[J].Earth Science Frontiers, 2013,20(2):10-18.
杨华,刘自亮,朱筱敏,等.鄂尔多斯盆地西南缘上三叠统延长组物源与沉积体系特征[J].地学前缘,2013,20(2):10-18.
7 ShanXiang,ZouZhiwen,MengXiangchao,et al.Provence analysis of Triassic Baikouquan Formation in the area around Mahu Depression,Junggar Basin[J].Acta Sedimentologica Sinica, 2016,34(5):930-939.
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[J].沉积学报,2016,34(5):930-939.
8 MortonA C,WhithamA G,FanningC M. Provenance of Late Cretaceous to Paleocene submarine fan sendstones in the norwegian Sea: Integration of heavy mineral,mineral chemical and zircon age data[J].Sedimentary Geology,2005,182(1-4):3-28.
9 LiSitian,PanYuanlin,LuYongchao,et al.Key techonlogy of prospecting and exploration of subtle traps in lacustrine fault basin:Sequence stratigraphic researches on the basin of high resolution seismic survey[J].Earth Science, 2002,27(5):592-598.
李思田,潘元林,陆永潮,等.断陷湖盆隐蔽油藏预测及探勘的关键技术—高精度地震探测基础上的层序地层学研究[J].地球科学,2002,27(5):592-598.
10 YuanXiaoqiang,YaoGuangqing,JiangPing,et al.Provenance analysis for Liushagang Formation of Wushi Depression,Beibuwan Basin,the South China Sea[J].Earth Science, 2017,42(11):2040-2054.
袁晓蔷,姚光庆,姜平,等.北部湾盆地乌石凹陷东部流沙港组物源分析[J].地球科学,2017,42(11):2040-2054.
11 GaoChonglong,JiYouliang,JinJun,et al.Development model of sedimentary system and reservoir under valley-monadnock paleotopography during buried stage of paleouplift: Case study of 1st member of K1q in Shinan area, hinterland of Junggar Basin[J].Natural Gas Geoscience, 2018,29(8):1120-1137.
高崇龙,纪友亮,靳军,等.古隆起埋藏期沟谷残丘地貌下沉积体系及油气藏发育模式——以准噶尔盆地腹部石南地区清水河组一段为例[J].天然气地球科学,2018,29(8):1120-1137.
12 MortonA C,HallsworthC R.Identifying provenance specific features of detrital heavy mineral assemblages in sandstones[J].Sedimentray Geology,1994,90(3):241-256.
13 ZhouXiang,HeSheng,ChenZhaoyou,et al.Diagenesis and diagenetic facies of low porosity and permeability sandstone in member 8 of Yanchang Formation in Daijiaping area,Ordos Basin[J].Oil & Gas Geology, 2016,37(2):155-164.
周翔,何生,陈召佑,等.鄂尔多斯盆地代家坪地球延长组长8段低孔渗砂岩成岩作用及成岩相[J].石油与天然气地质,2016,37(2):155-164.
[1] Liu Yong-fu, Xia Hui, Sun Qi, Lin Chang-song, Zhao Hai-tao, Li Hao, Huang La-mei, Zhang Zhi-yuan. Sequence stratigraphy and depositional evolution of the Bashijiqike Formation  in the western Tabei Uplift,Tarim Basin [J]. Natural Gas Geoscience, 2019, 30(1): 62-73.
[2] Zhang Da-zhi. Characterization of microscopic pore structure of tight sandstone reservoirs through nitrogen adsorption experiment: Case study of Shahezi Formation in Xujiaweizi Fault Depression,Songliao Basin,China [J]. Natural Gas Geoscience, 2017, 28(6): 898-908.
[3] Zhang Guang-quan,Hu Xiang-yang,Sun Bing,Jia Yue-wei. Sedimentary characteristics and controlling factors of gas condensate reservoir of Ying Ⅳ formation in Longfengshan Gasfield,Songliao Basin,China [J]. Natural Gas Geoscience, 2017, 28(4): 502-513.
[4] Liu Chao. Source rocks and tight conglomerate gas resource potential evaluation in Shahezi Formation of Xujiaweizi Depression, Songliao Basin [J]. Natural Gas Geoscience, 2017, 28(3): 429-438.
[5] Guo Shuai,Chen Ying,Zeng Qing-bo,Yang Hai-zhang,Han Yin-xue,Ji Mo,Shen Huai-lei,Guo Jia,Zhao Zhao. Provenance evolution of delta and the effects on reservoir quality in sandstones of theupper Enping Formation in the north of Baiyun Sag,Pearl River Mouth Basin [J]. Natural Gas Geoscience, 2017, 28(10): 1527-1536.
[6] Han Yin-xue,Wang Long-ying,Yang Dong-sheng,Zeng Qing-bo,Bai Hai-qiang,Guo Shuai,Yang Xiang-hua. Southern provenance supply of Zhuhai Formation and its significance on oil and gas accumulation in Baiyun Sag,Pearl River Mouth Basin [J]. Natural Gas Geoscience, 2017, 28(10): 1537-1545.
[7] . The method and application of using generalized-ΔLgR technology to predict the organic carbon content of continental deep source rocks [J]. Natural Gas Geoscience, 2016, 27(1): 149-155.
[8] LONG Li-wen,LI Xiang-bo,LIU Guang-lin,LIAO Jian-bo,ZHAO Yuan-yuan,LI Zhi-yong. Reservoir Petrology and Geological Significance ofDeep Water Sandstone of Chang 6 Formation in Ordos Basin [J]. Natural Gas Geoscience, 2015, 26(4): 634-640.
[9] XIAO Chuan-tao,XIAO Sheng,YE Fei,LIANG Wen-jun. Slope-break Zone and Its Controls on Lithologic Reservoirof Kunbei-Alaer Area,Qaidam Basin [J]. Natural Gas Geoscience, 2015, 26(11): 2085-2092.
[10] WANG Xin-xin,ZHENG Rong-cai,YAN Guo-qiang,WANG Chang-yong,CHEN Hao-ru. The Mudstone Sedimentary Environment and Provenance Analysis Based on the Geochemical Evidence of Rare Earth Elements:Take Chang 9 Oil-bearing Layerin Longdong Area of Ordos Basin as an Example [J]. Natural Gas Geoscience, 2014, 25(9): 1387-1394.
[11] WANG Min,SUN Ye-feng,WANG Wen-guang,WANG Yan,SHI Lei. Gas Generation Characteristics and Resource Potential of the Deep Source Rockin Xujiaweizi Fault Depression,Northern Songliao Basin [J]. Natural Gas Geoscience, 2014, 25(7): 1011-1018.
[12] LIN Hong,LI Feng-jie,LI Lei,YANG Yu-chuan,LI Jun-wu. Characteristics of Paleogene Heavy Mineral andIts Source in Northern Margin of Qaidam Basin [J]. Natural Gas Geoscience, 2014, 25(4): 532-541.
[13] LI Yu-ying, FU Xiao-fei, ZHANG Ming-xue. Fault Deformation Features and Reservoir controlling Mechanisms of Xujiaweizi Fault Depression in Songliao Basin [J]. Natural Gas Geoscience, 2012, 23(6): 979-988.
[14] . Provenance Analysis of Clastic Rocks in the Cretaceous Bashijiqike Formation at Kuqa Depression [J]. Natural Gas Geoscience, 2012, 23(6): 1025-1033.
[15] SHI Zhen-Sheng, WANG Xiu-Qin, WU Chang-Jiang. The Heavy Minerals and Provenances of the Upper Triassic Xujiahe Formation in Sichuan Basin [J]. Natural Gas Geoscience, 2011, 22(4): 618-627.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] . STUDIES ON THE OIL & GAS RESERVOIR FORMATION CONDITIONS AND EXPLORATION BEARI NG IN DABAN TOWN SUB-DEPRESSION OF CHAIWOPU DEPRESSION[J]. Natural Gas Geoscience, 2005, 16(1): 20 -24 .
[2] SHAO Rong, YE Jiaren, CHEN Zhangyu . THE APPLICATION OF FLUID INCLU SION IN OIL SYSTEM RESEARCH, FAULT DEPRESION BASIN[J]. Natural Gas Geoscience, 2000, 11(6): 11 -14 .
[3] HE Jiaxiong, LI Mingxing, CHEN Weihuang . GEOTEMPERATURE FIELD AND UP- WELLING ACTION OF HOT FLOW BODY AND ITS RELATIONSHIP WITH NATURAL GAS MIGRATION AND ACCUMULATION IN YINGGEHAI BASIN[J]. Natural Gas Geoscience, 2000, 11(6): 29 -43 .
[4] . [J]. Natural Gas Geoscience, 2000, 11(4-5): 57 -67 .
[5] . SIGNIFICANCE OF STUDING FAULT SEAL IN HYDROCARBON ACCUMULATION SYSTEM ANALYSIS[J]. Natural Gas Geoscience, 2000, 11(3): 1 -8 .
[6] .  APPLICATION OF VSP TECHNOLOGY IN THE DEVELOPMENT AND DEPLOYMENT RESEARCH IN COM PLICATED FAULT BLOCK RESERVOIR JIN 612[J]. Natural Gas Geoscience, 2005, 16(1): 117 -122 .
[7] MA Lixiang . CONCEPT AND STUDING STATUS OF PETROPHYSICAL FLOW UNIT IN PETROLEUM EXPLORATION AND DEVELOPMENT[J]. Natural Gas Geoscience, 2000, 11(2): 30 -36 .
[8] DU Le-tian. THE FIVE GAS SPHERES OF THE EARTH AND NATURAL GAS EXPLOITATION FROM MIDDLE CRUST[J]. Natural Gas Geoscience, 2006, 17(1): 25 -30 .
[9] ZHOU Shi-xin; ZOU Hong-liang; XIE Qi-lai, JIA Xin-liang. ORGANIC-INORGANIC INTERACTIONS DURING THE FORMATION OF OILS IN S EDIMENTARY BASIN[J]. Natural Gas Geoscience, 2006, 17(1): 42 -47 .
[10] CAO Hua,GONG Jing-jing,WANG Gui-feng. THE CAUSE OF OVERPRESSURE AND ITS RELATIONSHIP WITH RESERVOIR FORMING[J]. Natural Gas Geoscience, 2006, 17(3): 422 -425 .