| 鄂尔多斯盆地吴堡地区长6段浊积特征及其石油地质意义 |
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| 引用本文： | 张伟1,刘建朝1,高志亮2,孙少波2. 鄂尔多斯盆地吴堡地区长6段浊积特征及其石油地质意义[J]. 延边大学学报(自然科学版), 2012, 0(2): 64-71 |
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| 作者姓名： | 张伟1 刘建朝1 高志亮2 孙少波2 |
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| 作者单位： | 1.长安大学 地球科学与资源学院,陕西 西安 710054; 2.长安大学 数字油田研究所,陕西 西安 710054 |
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| 摘 要： | 在介绍鄂尔多斯盆地吴堡地区延长组长6段沉积特征的基础上,探讨了该储层物性特征、浊积岩特征、浊积岩分布规律及其对油藏的影响,明确了浊流沉积的石油地质意义。结果表明:鄂尔多斯盆地吴堡地区长6段以发育长石砂岩为主,填隙物成分有方解石、绿泥石、白云母以及少量的石英加大、长石加大等,砂岩储集层孔隙结构具有很强的非均质性; 吴堡地区长6期湖盆沉降趋于稳定,是三角洲的高建设时期; 多水系、多物源的三角洲前缘沉积为深湖浊积扇沉积提供了充足的物质基础; 在吴堡地区东北部三角洲前缘水下分流河道前端发育深湖浊积扇沉积,可区分出中心微相和边缘微相两个沉积微相带,其中浊积扇中心微相以细砂岩、粉砂岩与暗色泥岩呈砂泥互层; 从平面上看,浊积岩砂体非均质性在侧向上逐渐变弱,砂体底部发育厚度较大、成熟度较高的暗色湖相沉积的烃源岩,深湖相的暗色泥岩含有丰富的烃源岩,而浊积岩砂体是由深湖相的暗色泥岩构成,孔渗物性好的区域易于形成良好的上倾尖灭的透镜状岩性油藏。
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| 关 键 词： | 浊流沉积 沉积微相 物性特征 岩性圈闭 长6段 延长组 吴堡地区 鄂尔多斯盆地 |
Turbidity Characteristics and Petroleum Geological Significance of Chang-6 Section in Wubu Area of Ordos Basin |
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| ZHANG Wei1,LIU Jian-chao1,GAO Zhi-liang2,SUN Shao-bo2. Turbidity Characteristics and Petroleum Geological Significance of Chang-6 Section in Wubu Area of Ordos Basin[J]. Journal of Yanbian University (Natural Science), 2012, 0(2): 64-71 |
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| Authors: | ZHANG Wei1 LIU Jian-chao1 GAO Zhi-liang2 SUN Shao-bo2 |
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| Affiliation: | 1. School of Earth Sciences and Resources, Chang'an University, Xi'an 710054, Shaanxi, China; 2. Institute of Digital Oilfield, Chang'an University, Xi'an 710054, Shaanxi, China |
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| Abstract: | Based on the introduction of sedimentary characteristics of Chang-6 Section in Yanchang Formation of Wubu Area, Ordos Basin, the physical property, turbidite characteristics and turbidite distribution of Chang-6 Section and their influence on oil reservoir were analyzed, and the petroleum geological significance of turbidite was discussed. The results showed that the main rock type of Chang-6 Section in Wubu Area of Ordos Basin was feldspathic sandstone, and the composition of interstitial material included calcite, chlorite, white mica and a little quartz overgrowth and feldspar overgrowth, etc.; the anisotropism of pore structure of sandstone reservoir was very strong; the lacustrine basin settlement tended to stable in Chang-6 Section of Wubu Area, and was the high construction period of delta; the delta front sediment, which included multiple water systems and provenances, provided sufficient materials for the deep lacustrine turbidite fan sediment; the front of underwater distributary channel of delta front developed deep lacustrine turbidite fan sediment in the northeast of Wubu Area, and center microfacies and edge microfacies were distinguished in the sediment; packsand and siltite were interbedded with dark mudstone in center microfacies of turbidity fan; in horizontal, the anisotropism of turbidite sandbodies gradually weakened in the lateral direction, and the sandbodies at the bottom developed hydrocarbon source rocks which were dark lacustrine facies sedimentary with higher thickness and maturity; dark mudstone of deep lacustrine facies was rich in hydrocarbon source rock, and turbidite sandbodies were composed of the dark mudstone, so that it was easier to successfully form the updip pinchout and lenticular lithological reservoir in the region with good permeability and porosity property. |
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| Keywords: | turbidity deposition sedimentary microfacies physical property lithologic trap Chang-6 Section Yanchang Formation Wubu Area Ordos Basin |
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