鄂尔多斯盆地富县地区上三叠统延长组砂质碎屑流沉积特征及其油气勘探意义
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摘要
通过岩芯观测、地震解释和测井分析,结合薄片观察、粒度分析以及各种资料的综合分析,对鄂尔多斯盆地南部富县地区上三叠统延长组沉积相类型及特征进行深入研究,提出长9—长6油层组存在砂质碎屑流沉积。结合盆地沉积背景及其演化规律,探讨了砂质碎屑流沉积的成因机制,详细论述了砂质碎屑流沉积的沉积特征,建立了砂质碎屑流的沉积模式。研究表明砂质碎屑流砂体主要由块状粉细砂岩和含泥砾粉细砂岩两种成因相构成,其成因是三角洲前缘砂体在外界触发力作用下,滑动崩塌而形成。分析了砂质碎屑流沉积与油气的分布关系,实践表明砂质碎屑流沉积体是下生上储或下储上生的油藏类型,属于典型的岩性油气藏,构成了该区深水区域的良好岩性圈闭储集体。
According to the analysis for cores,seismic interpretation and well-logging,the authors have thoroughly studied the sedimentary facies types and characters of Yanchang Formation of the Upper Triassic in the south Ordos Basin with thin sections and grain size analysis and a great deal of indoor testing data.The authors have proposed that the sedimentary facies type of Chang 9 to Chang 6 of Yanchang Formation is sandy debris flows.With basin sedimentary and evolutionary background,the genetic mechanism of the sand debris flows have been discussed,and detailed studies have been made on the rock types and sedimentary structures of the sandy debris flows,build up relevant sedimentary models.The results indicate that the sandy debris flows deposit is composed of two genetic facies of massive-bedded siltsand and packsand and mud pebble siltsand and packsand,which indicate deposition from delta-front sand during slip and slump under outside function of energy.Relationship between sandy debris flow depositional systems and distribution of oil and gas are elaborated in detail.It is considered that sandy debris flow deposits are injection migration oil-gas accumulation types and classic lithologic hydrocarbon reservoir,which are the most favorable sedimentary facies belt for the generation of Yanchang Formation reservoirs.
According to the analysis for cores,seismic interpretation and well-logging,the authors have thoroughly studied the sedimentary facies types and characters of Yanchang Formation of the Upper Triassic in the south Ordos Basin with thin sections and grain size analysis and a great deal of indoor testing data.The authors have proposed that the sedimentary facies type of Chang 9 to Chang 6 of Yanchang Formation is sandy debris flows.With basin sedimentary and evolutionary background,the genetic mechanism of the sand debris flows have been discussed,and detailed studies have been made on the rock types and sedimentary structures of the sandy debris flows,build up relevant sedimentary models.The results indicate that the sandy debris flows deposit is composed of two genetic facies of massive-bedded siltsand and packsand and mud pebble siltsand and packsand,which indicate deposition from delta-front sand during slip and slump under outside function of energy.Relationship between sandy debris flow depositional systems and distribution of oil and gas are elaborated in detail.It is considered that sandy debris flow deposits are injection migration oil-gas accumulation types and classic lithologic hydrocarbon reservoir,which are the most favorable sedimentary facies belt for the generation of Yanchang Formation reservoirs.
引文
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2蒋恕,王华,Paul Weimer.深水沉积层序特点及构成要素[J].地球科学-中国地质大学报,2008,33(6):825-833[Jiang Shu,WangHua,Paul Weime.Sequence stratigraphy characteristics and sedimen-tary elements in deepwate[J].Earth Science-Journal of China Univer-sity of Geoscience,2008,33(6):825-833]
3甘克文.我国海上油气勘探前景及邻国关系问题简析[J].石油科技论坛,2005,6(3):27-29[Gan Kewen.China’s offshore oil andgas exploration prospect and analysis on the problems between neighbor-ing countries[J].Oil Forum,2005,6(3):27-29]
4李祥辉,王成善,金玮,等.深海沉积理论发展及其在油气勘探中的意义[J].沉积学报,2009,27(1):77-86[Li Xianghui,WangChengshan,Jin Wei,et al.A review on deep-sea sedimentation theory:Significances to oil-gas exploration[J].Acta Sedimentologica Sinica,2009,27(1):77-86]
5邹才能,赵政璋,杨华,等.陆相湖盆深水砂质碎屑流成因机制与分布特征——以鄂尔多斯盆地为例[J].沉积学报,2009,12(6):1065-1075[Zou Caineng,Zhao Zhengzhang,Yang Hua,et al.Geneticmechanism and distribution of sandy debris flows in terrestrial lacustrinebasin[J].Acta Sedimentologica Sinica,2009,12(6):1065-1075]
6 Shanmugam G.50 years of the turbidite paradigm(1950s-1990s)deep-water processes and facies models:a critical perspective[J].Marineand Petroleum Geology,2000,17:285-342
7 Bouma A H,Devries M B,Stone C G.Reinterpretation of depositionalprocesses in a classic flysch sequence(Pennsylvanian JackforkGroup),Ouachita Mountains,Arkansa sand Oklahoma:discussion[J].AAPG Bulletin,1997,81(3):470-472
8 Coussot P,Meunier M.Recognition,classification and mechanical de-scription of debris flows[J].Earth-Sci Rev,1996,40(3-4):209-227
9 Dasgupta P.Sediment gravity flow-the conceptual problems[J].EarthScience Review,2003,62(3-4):265-281
10 Bouma A H.Sedimentology of Some Flysch Deposits:a Graphic Ap-proach to Facies Interpretation[M].Amsterdam:Elsevier,1962
11 Shanmugan G.High-density turbidity current:are they sandy debrisflows?[J].Journal of Sedimentary Research,1996,66(1):2-10
12 Shanmugam G.Deep-marine tidal bottom currents and their reworkedsands in submarine canyons:implications for sand distribution.Den-ver,Colorado:American Association of Petroleum Geologists AnnualConvention Abstracts,2001:184
13 Shanmugam G,Moiola R J.Reinterpretation of depositional processesin a classic flysch sequence(Pennsylvanian Jackfork Group),Ouachi-ta Mountains,Arkansas and Oklahoma[J].AAPG Bulletin,1995,79:672-695
14 Shanmugam G.Ten turbidite myths[J].Earth-Science Reviews,2002,58:311-341
15张兴阳,罗顺社,何幼斌.沉积物重力流深水牵引流沉积组合——鲍玛序列多解性探讨[J].江汉石油学院学报,2001,23(1):1-4[Zhang Xingyang,Luo Shunshe,He Youbin.Deposit as-semblage of gravity flow and traction current in deep water:A study ofthe multiple interpretation of the Bouma sequence[J].Journal ofJianghan Petroleum Institute,2001,23(1):1-4]
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