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Received：12 September 2019，
Published：28 April 2020
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扶新隆起带扶杨油层经历了近60年的勘探开发依然是松辽盆地南部最主要的油气富集区之一。然而，扶新隆起带构造条件复杂，断层密集，油、气、水分布极其复杂，油气运聚过程及油气富集规律尚不明确，极大制约了进一步油气勘探开发效果。在分析扶新隆起带北坡扶杨油层地层水来源以及纵向上和平面上分布规律基础上，解剖重点区典型的油藏剖面，结合地层压力及烃源岩条件，深入探讨扶新隆起带扶杨油层地层水特征，与油气运聚和富集的耦合关系。垂向上，扶新隆起带水化学可划分为大气水下渗淡化带、压实水淡化带、溶蚀浓缩带、粘土矿物脱水淡化带以及越流浓缩带5个区带；平面上，扶新隆起带新北鼻状构造带和新立鼻状构造带为是两大离心流发生集中越流泄水的区域，形成了高矿化度、高钠氯系数区域与油气富集区高度的一致性。源内成藏区、源边成藏区油源条件较好，地层受扰动深度较深，成藏条件良好。而在源外成藏区部烃源岩成熟度低，含油气流体影响深度较浅，油源条件较差。
After nearly 60 years of exploration and development
Fuyang oil layer in Fuxin Uplift still remains one of the most important hydrocarbon accumulation zones in Southern Songliao Basin.However
the structural setting of Fuxin Uplift is complex:faults are densely developed
the contacts between oil
gas and water layers are extremely complex
and the process of hydrocarbon migration and accumulation and the hydrocarbon enrichment pattern stay to be identified.These factors greatly restrict further efforts made for hydrocarbon exploration and development.Following the analysis of the origin and the vertical and horizontal distribution patterns of formation water in Fuyang oil layer on the northern slope of Fuxin Uplift
we dissected the typical reservoir profiles in key areas
and made an in-depth discussion on the coupling relations between formation water characteristics and hydrocarbon migration
accumulation and enrichment in Fuyang oil layer in Fuxin Uplift in combination with analysis of formation pressure and source rocks.Vertically
five hydrochemical zones can be identified in Fuxin Uplift:diluted zones from meteoric water percolation
diluted zone from compaction
concentrated zone from dissolution
diluted zone from clay mineral dehydration
as well as concentrated zone from over flow.In the plane
the Xinbei and Xinli nose-like structural zones in the study area are the areas where two major centrifugal flows converge and result in cross-formational flow
leading to the high consistency between zones of high salinity and high sodium chloride coefficient and zones of hydrocarbon enrichment.The oil source conditions are relatively better in the intra-source and near-source hydrocarbon accumulation zones
and the depth of hydrocarbon-bearing fluid disturbance is deeper
favorable for hydrocarbon accumulation.However
the source rocks in out-of-source hydrocarbon accumulation zones are low in maturity
and the depth of hydrocarbon-bearing fluid disturbance is shallow
unfavorable for hydrocarbon accumulation.
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