油气耗散————油气地质研究和资源评价的弱点和难点

doi:10.11743/ogg20080416

Abstract

Abstract:

Hydrocarbon migration may have three results:(1)accumulation,(2)diffusion in rocks and fluids,or (3) loss due to interactions with fluids and surrounding rocks or surface exposure.The latter is defined here as dissipation.The dissipation is most active during hydrocarbon migration and is closely linked to hydrocarbon accumulation,thus study of the phenomenon become an indispensible part of petroleum geology research,and petroleum exploration and resource assessment.Hydrocarbon dissipations can be divided into four types according to the differences of quantity and quality of hydrocarbons before and after dissipation:quantity decrease,phase transformation,composition alteration,and quality conversion,reflectting the differences in environment,conditions and characteristics of dissipation.The quality conversion often occurs at surface or near surface,where hydrocarbons will interact with surrounding rocks,pore fluids or air.The epigenetic products and minerals resulted from these interactions generally have no apparent features of hydrocarbons,but the amount of dissipated hydrocarbons is huge,thus much attention should be given to this phenomenon.These products in combination with direct evidences of hydrocarbon dissipation ( such as seepage,bitumen and heavy oil) can not only serve as an important means to address the puzzle of hydrocarbon dissipation and its scale,but also provide effective clues and significant indicators for tracing hydrocarbon pathways,searching for oil and gas pools,and evaluating the scale of dissipations.This paper analyzes and discusses the types,basic characteristics,geochemical properties,environments of formation and distributions of various epigenetic products related with gas dissipation in the Upper Paleozoic in northeastern Ordos Basin.

Key words: hydrocarbon dissipation, destruction of oil and gas pools, hydrocarbon migration, fluid-rock interaction, epigenetic reductive alteration, Ordos Basin

CLC Number:

TE122.1

Liu Chiyang, Ma Yanping, Wu Bolin, Liu Chao. Weakness and difficulty of petroleum geology study and resource assessment:hydrocarbon dissipation[J]. Oil & Gas Geology, 2008, 29(4): 517-526.

References

[1] 刘池洋.后期改造强烈——中国沉积盆地的重要特点之一[J].石油与天然气地质,1996,17(4):255～261
[2] 刘池洋,赵重远,杨兴科.活动性强、深部作用活跃——中国沉积盆地的两个重要特点[J].石油与天然气地质,2000,21(1):1～6
[3] 刘池洋,杨兴科.改造盆地研究和油气评价的思路[J].石油与天然气地质,2000,21(1):11～14
[4] 王庭斌.中国气藏主要形成、定型于新近纪以来构造运动[J].石油与天然气地质,2004,25(2):127～132
[5] MacGregor D S.Factors controlling the destruction or preservation of giant light oil-fields[J].Petroleum Geoscience,1996,2:197-217
[6] 吕延防,王振平.油气藏破坏机理分析[J].大庆石油学院学报,2001,35(3):5～9
[7] 吴元燕,平俊彪,吕修祥,等.准噶尔盆地西北缘油气藏保存及破坏定量研究[J].石油学报,2002,23(6):24～30
[8] 韩世庆,王守德,胡惟元.黔东麻江古油藏的发现及其地质意义[J].石油与天然气地质.1982,3(4):317～326
[9] 庞雄奇,姜振学,左胜杰.叠合盆地构造变动破坏烃量研究方法探讨[J].地质论评,2002,48(4):384～390
[10] 张俊,庞雄奇,刘洛夫,等.塔里木盆地志留系沥青砂岩的分布特征与石油地质意义[J].中国科学(D辑),2004,34(增刊Ⅰ):169～176
[11] 刘方槐.轻烃在盖层中的扩散研究进展及四川威远气田震旦系气藏的扩散破坏估算[J].天然气地球科学,1992,3(5):11～16
[12] 傅广,吕延芳.大庆长垣以东地区深层天然气扩散系统及损失量研究[J].石油勘探与开发,1999,26(2):101～104
[13] 刘池洋,孙海山.改造型盆地类型划分[J].新疆石油地质,1999,20(2):79～82
[14] Doré A G,Jensen L N.The impact of late Cenozoic uplift and erosion on hydrocarbon exploration:offshore Norway and some other uplifted basins[J].Global and Planetary Change,1996,12(1-4):415-436
[15] 李明诚.石油与天然气运移(第三版)[M].北京:石油工业出版社,2004
[16] 赵重远.石油地质学[M].北京:地质出版社,1979
[17] 李国玉,金之钧.世界含油气盆地图集[M].北京:石油工业出版社,2005
[18] 童崇光.油气田地质学[M].北京:地质出版社,1985.271
[19] 钟宁宁,陈恭洋.煤系气油比分配控制因素及其与大中型气田的关系[M].北京:石油工业出版社,2002
[20] Schumacher D.Hydrocarbon induced alteration of soil sand sediments[A].In:Schumacher D,Abrams M A,eds.Hydrocarbon migration and its near surface expression[C].AAPG Memoir 66,1996.71-89
[21] Schumacher D.Surface geochemical exploration for oil and gas:new life for an old technology[J].The Leading Edge,2000,3:258-261
[22] 马艳萍,刘池阳,王建强,等.盆地后期改造中油气运散的效应-鄂尔多斯盆地东北部中生界漂白砂岩的形成[J].石油与天然气地质,2006,27(2):233～238
[23] 马艳萍,刘池洋,赵俊峰,等.鄂尔多斯盆地东北部砂岩漂白现象与天然气逸散的关系[J].中国科学,2007,37(专辑):127～138
[24] 吴柏林,邱欣卫.论东胜矿床油气逸散蚀变的地质地球化学特点及其意义[J].中国地质,2007,34(3):455～462
[25] Wu Bolin,Liu Chiyang,Wang Jianqiang.Basical characteristics of fluid geologic process of interlayer oxidation zone sandstone-type Uranium deposit[J].Science in China(Series D):Earth Sciences,2007,50(SⅡ):185-194
[26] 吴柏林,王建强,刘池阳,等.东胜砂岩型铀矿形成中天然气地质作用的地球化学特征[J].石油与天然气地质,2006,27(2):225～232
[27] 李子颖,方锡珩,陈安平,等.鄂尔多斯盆地北部砂岩型铀矿目标层灰绿色砂岩成因[J].中国科学,2007,37:139～146
[28] 权建平,樊太亮,徐高中,等.中国北方盆地中油气运移对砂岩型铀矿成矿作用讨论[J].中国地质,2007,34(3):470～477
[29] 冯乔,张小莉,王云鹏,等.鄂尔多斯盆地北部上古生界油气运聚特征及其铀成矿意义[J].地质学报,2006,80(5):748～752
[30] Reeves F.Geology of the Cement oil field,Caddo County Oklahoma[J].US Geological Survey Bulletin,1922,726:41-85
[31] King J W,Austin S R.Some characteristics of roll-type uranium deposits at Gas Hills,Wyoming:US[J].Mining Engineers,1966,18(5):73-80
[32] Levandowski D W,Kaley M E,Silverman S R,et al.Cementation in Lyons sandstone Colorado[J].AAPG Bulletin,1973,57:2 217-2 244
[33] Lamb C F.Painter reservoir field-giant in the Wyoming thrust belt[A].In:Halbouty M T,ed.Giant oil and gas fields of the deca-de 1968-1978[C].AAPG Memoir 30,1980.281-288
[34] Allen R F,Thomas R G.The uranium potential of diagenetically altered sandstones of the Permian Rush Springs Formation,Cement District,Southwestern Oklahoma Econ[J].Economic Geology,1984,79:284-296
[35] Surdam R C,Jiao Z S,MacGowan D B.Redox reactions involving hydrocarbons and mineral oxidants:A mechanism for significant porosity enhancement in sandstones[J].AAPG Bulletin,1993,77:1 509-1 518
[36] Kirkland D W,Denison R E,Rooney M A.Diagenetic alteration of Permian strata at oil fields of south central Oklahoma,USA[J].Marine and Petroleum Geology,1995,12(6):629-644
[37] Shebl M A,Surdam R C.Redox reactions in hydrocarbon clastic reservoirs:experimental validation of this mechanism for porosity enhancement[J].Chemical Geology,1996,132:103-117
[38] Chan M A,Parry W T,Bowman J R.Diagenetic hematite and manganese oxides and fault-related fluid flow in Jurassic sandstones,Southeastern Utah[J].AAPG Bulletin,2000,84(9):1281-1310
[39] Beitler B,Chan M A,Parry W T.Bleaching of Jurassic Navajo sandstone on Colorado Plateau Laramide highs:Evidence of exhumed hydrocarbon supergiants?[J].Geology,2003,31(12):1041-1044
[40] Parry W T,Chan M A,Beitler B.Chemical bleaching indicates episodes of fluid flow in deformation bands in sandstone[J].AAPG Bulletin,2004,88(2):175-191
[41] Chidsey T C.Rocky Mountain gas reservoirs-America's natural gas storehouse:Utah geological survey[J].Survey Notes,1995,27:1-2
[42] Walker T R.A study of global sand seas:Red color in dune sand[A].In:McKee E D,ed.A study of global sand seas[C].US Geological Survey Professional Paper,1979.61-81
[43] Moulton G F.Some features of red bed bleaching[J].American Association of Petroleum Geologists Bulletin,1926,10:304-311
[44] Shebl M A,Surdam R C.Redox reactions in hydrocarbon clastic reservoirs:Experimental validation of this mechanism for porosity enhancement[J].Chemical Geology,1996,132:103-117
[45] Breit G N,Meunier J D.Fliud inclusion and δ¹⁸O,and⁸⁷ Sr/⁸⁶ Sr evidence for the fault-controlled copper mineralization,Lisbon Valley,Utah,and Silck Rock district,Colorado[J].Economic Geology,1990,85:884-891
[46] 王驹,杜乐天.论铀成矿过程中的气还原作用[J].铀矿地质,1995,11(1):19～24
[47] 刘友民.陕甘宁盆地北缘乌兰格尔地区白垩系油苗成因及意义[J].石油勘探与开发,1982,9(3):39～43
[48] 张如良.鄂尔多斯深盆气与铀矿化关系初探[J].铀矿地质,2004,20(4):213～218
[49] 丁万烈.绿色蚀变带的地球化学性质及其找矿意义探讨[J].铀矿地质,2003,19(5):277～282
[50] 任战利,张胜,高胜利,等.伊盟隆起东胜地区热演化史与多种能源矿产的关系[J].石油与天然气地质,2006,27(2):187～193
[51] 陈宏斌,徐高中,王金平,等.鄂尔多斯盆地南缘店头铀矿床矿化特征及其与东胜铀矿床对比[J].地质学报,2006,80(5):724～732
[52] 杨晓勇,罗贤冬,凌明星.鄂尔多斯盆地含铀砂岩碳酸盐胶结物C-O同位素研究及地质意义[J].中国科学技术大学学报,2007,37(8):979～985
[53] 向伟东,方锡珩,李田港,等.鄂尔多斯盆地东胜铀矿床成矿特征与成矿模式[J].铀矿地质,2006,22(5):257～266
[54] 妥进才,张明峰,王先彬.鄂尔多斯盆地北部东胜铀矿区沉积有机质中脂肪酸甲酯的检出及意义[J].沉积学报,2006,24(3):432～439

Weakness and difficulty of petroleum geology study and resource assessment:hydrocarbon dissipation

PDF (PC)

Knowledge

Abstract

Cite this article

share this article

References

Related Articles 15

Recommended Articles

Metrics

[1]	Wei Dang, Jinchuan Zhang, Fengqin Wang, Pei Li, Chang'an Shan, Ruijing Wang. Thermodynamics and kinetics of water vapor adsorption onto shale: A case study of the Permian Shanxi Formation, Ordos Basin [J]. Oil & Gas Geology, 2021, 42(1): 173-185.
[2]	Bojiang Fan, Qiliang Mei, Xiaojun Wang, Yue Meng, Qijiang Huang. Geochemical comparison of mudstone and shale—A case study of the 7^th member of Yanchang Formation in Ansai area, Ordos Basin [J]. Oil & Gas Geology, 2020, 41(6): 1119-1128.
[3]	Zhenglu Xiao, Shijia Chen, Guanglin Liu, Pan Wang, Longxiang Tang, Zhanghao Liu. Further understanding of differential accumulations of oil and water in tight sandstones with limited charging power:A case study of Chang 8 member in Huachi area, Ordos Basin, China [J]. Oil & Gas Geology, 2020, 41(6): 1129-1138.
[4]	Faqi He, Chengchun Liang, Cheng Lu, Chunyan Yuan, Xiaowei Li. Identification and description of fault-fracture bodies in tight and low permeability reservoirs in transitional zone at the south margin of Ordos Basin [J]. Oil & Gas Geology, 2020, 41(4): 710-718.
[5]	Shixiang Li, Xiaobing Niu, Guangdi Liu, Jihong Li, Mingliang Sun, Fuliang You, Haonan He. Formation and accumulation mechanism of shale oil in the 7th member of Yanchang Formation, Ordos Basin [J]. Oil & Gas Geology, 2020, 41(4): 719-729.
[6]	Dingye Zheng, Xiongqi Pang, Fujie Jiang, Tieshu Liu, Xinhe Shao, Longlong Li, Yuying HuYan, Fangxin Guo. Characteristics and physical simulation of the Upper Paleozoic tight gas accumulation in Linxing area, Ordos Basin [J]. Oil & Gas Geology, 2020, 41(4): 744-754.
[7]	Zeng Lianbo, Lyu Peng, Qu Xuefeng, Fan Jianming. Multi-scale fractures in tight sandstone reservoirs with low permeability and geological conditions of their development [J]. Oil & Gas Geology, 2020, 41(3): 449-454.
[8]	Zhao Xiangyuan, Lyu Wenya, Wang Ce, Zhu Shengju, Fan Jianming. Major factors controlling waterflooding-induced fracture development in low-permeability reservoirs—A case study of Chang 6 reservoir in W block in Ansai oilfield,Ordos Basin [J]. Oil & Gas Geology, 2020, 41(3): 586-595.
[9]	Ju Wei, You Yuan, Feng Shengbin, Xu Haoran, Zhang Xiaoli, Wang Shengyu. Characteristics and genesis of bedding-parallel fractures in tight sandstone reservoirs of Chang 7 oil layer,Ordos Basin [J]. Oil & Gas Geology, 2020, 41(3): 596-605.
[10]	Dong Shaoqun, Lyu Wenya, Xia Dongling, Wang Shijia, Du Xiangyi, Wang Tao, Wu Yue, Guan Cong. An approach to 3D geological modeling of multi-scaled fractures in tight sandstone reservoirs [J]. Oil & Gas Geology, 2020, 41(3): 627-637.
[11]	Xiaohan Mei, Qin Zhang, Yayun Wang, Xinsong Wu, Jingyan Liu, Jiahong Zhao, Wuxue Wang. Hydrochemical characteristics of formation water and its relationship with hydrocarbon migration and accumulation in Fuyang oil layer in Fuxin Uplift, Songliao Basin [J]. Oil & Gas Geology, 2020, 41(2): 328-338, 358.
[12]	Zhenjia Cai, Yuhong Lei, Xiaorong Luo, Xiangzeng Wang, Ming Cheng, Lixia Zhang, Chengfu Jiang, Qianping Zhao, Jintao Yin, Likuan Zhang. Characteristics and controlling factors of organic pores in the 7th member of Yanchang Formation shale in the Southeastern Ordos Basin [J]. Oil & Gas Geology, 2020, 41(2): 367-379.
[13]	Cheng Feng, Haitao Fan, Yujiang Shi, Xuekun Chen, Gaoren Li, Zhiqiang Mao. Prediction for the formation water salinity in low-permeability reservoirs with complex wettability: A case study of the Triassic Chang 8¹ member, Longdong area, Ordos Basin [J]. Oil & Gas Geology, 2020, 41(2): 442-448.
[14]	Zhiliang He, Yongsheng Ma, Juntao Zhang, Dongya Zhu, Yixiong Qian, Qian Ding, Daizhao Chen. Distribution, genetic mechanism and control factors of dolomite and dolomite reservoirs in China [J]. Oil & Gas Geology, 2020, 41(1): 1-14.
[15]	Anjiang Shen, Yana Chen, Jianyong Zhang, Xinfeng Ni, Jingao Zhou, Xingning Wu. Characteristics of intra-platform rift in ancient small-scalecratonic platform of China and its implications for hydrocarbon exploration [J]. Oil & Gas Geology, 2020, 41(1): 15-25.