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鄂尔多斯盆地上古生界储层现今地下水动力场及其流体特征
引用本文:金爱民,楼章华,朱蓉,张文正. 鄂尔多斯盆地上古生界储层现今地下水动力场及其流体特征[J]. 高校地质学报, 2002, 8(3): 334-344
作者姓名:金爱民  楼章华  朱蓉  张文正
作者单位:1. 浙江大学海洋科学与工程系,杭州310028; 2. 长庆石油局勘探开发研究院,西安 710021
基金项目:国家九五攻关95-110-01-03专题的部分成果
摘    要:油气的运移、聚集与地下水动力场的形成与演化紧密相关。含油气沉积盆地地下水动力场的理想模式可以归纳为两种,即对称型和不对称型,其中局部地下水动力单元可以划分为:(1)泥岩压水离心流;(2)大气水下渗向心流;(3)越流、越流-蒸发泄水;(4)滞留4种类型。本文试通过讨论鄂尔多斯盆地现今地下水动力场的特征,推断其油气的运移和聚集,这对分析鄂尔多斯盆地上古生界气田的形成,以及资源评价和勘探决策都具有极其重要的意义。

关 键 词:上古生界 储层 鄂尔多斯盆地 地下水动力场 局部水动力单元 油气运移 油气聚集
文章编号:1006-7493(2002)03-334-11
收稿时间:2002-09-20
修稿时间:2002-05-13

A Study on Present Hydrodynamics and Properties of Fluids in Up-Palaeozoic Reservoir of The Ordos Basin
JIN Ai-min,LOU Zhang-hua,ZHU Rong,ZHANG Wen-zheng. A Study on Present Hydrodynamics and Properties of Fluids in Up-Palaeozoic Reservoir of The Ordos Basin[J]. Geological Journal of China Universities, 2002, 8(3): 334-344
Authors:JIN Ai-min  LOU Zhang-hua  ZHU Rong  ZHANG Wen-zheng
Affiliation:1. Department of Ocean Sciences and Engineering, Zhejiang University, Hangzhou 310028, China; 2. Exploration and Development Institute of Changqing Petroleum Adminitration Bureau, Xi'an 710021, China
Abstract:The migration and accumulation of oil-gas are closely related to the generation and evolution 0f the hydrodynamics,which controls the formation and distribution of oil-gas fields. Theoretica1 mode1s of the hydrodynamics for petroliferous sedimentary basins could be classified as two types, i.e; syrnmecal and asymmetrical models. With in a sedimentary basins, four different types of local hydrodynamic units can be recognized:① centrifugal flow caused by mudstone compaction at the depression area,② gravity—induced centripetal flow recharged by meteoric water at the basin edge generally,③ discharge area by cross-formational flow,or cross-formational flow-evaporation,as well as④ stagnation area.For the Ordos basin,the hydrodynamics in the Up-Palaeozoic reservoir is characterized by strong asymmetry,gravity-induced centripetal flow in the northern and eastern ascending areas of the basin,centrifugal flow caused by mudstone compaction in the western-southern declining areas of the basin,and cross-formational flow or cross-formational flow-evaporation in the areas between those areas mentioned above.By studying the migrating power,direction and channels of fluids,such as groundwater and nature gas,we can establish the present hydrodynamic model of the Ordos Basin.Groundwater flows from east to west,and nature gas migrates from west to east,which match with the distribution of fluid potential in the basin.Because of the inhomogeneity in the reservoir, distribution of the local hydrodynamic units follows certain patterns in the basin,which make the hydrodynamics complex.The exploration has also proved the formation and distribution of the hydrodynamics in the basin,because many gas fields have been found in the center of basin and groundwater is primarily located in the northern and eastern of Ordos Basin.
Keywords:Ordos Basin  hydrodynamics  local hydrodynamic units  migration and accumulation of oil-gas
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