滚动勘探中薄层砂体厚度的预测研究及应用

来源 :地球物理学进展 | 被引量 : 0次 | 上传用户:a542886140
下载到本地 , 更方便阅读
声明 : 本文档内容版权归属内容提供方 , 如果您对本文有版权争议 , 可与客服联系进行内容授权或下架
论文部分内容阅读
随着渤海地区勘探程度日趋成熟,位于渤海海域南部的渤南矿区在贯彻以寻找大中型油气田为目标的同时,兼顾在成熟油田周边寻找滚动目标的勘探.滚动目标主要以浅层的构造加岩性目标为主,目标层段主要分布在明上段和明下段,其中明上段的河流-平原相为砂泥岩互层,明下段的平原-河流相为泥岩夹砂岩,储层厚度横向变化快.目前地震上的砂体厚度预测在极限分辨率内,即超过四分之一地震波长的砂体厚度预测不准确.本文首先从经典的楔状模型出发,通过正演得出砂体厚度与峰值频率的相关规律.进而以成熟油田的丰富井资料为基础,基于多口生产井的统计,研究峰值频率和砂体不同厚度间的关系,从而拟合出适合目标区的线性关系式.研究表明当储层含纯油层时会降低砂体的峰值频率,而含水时会提高砂体的峰值频率,因此在经验公式拟合时需要对井点按流体进行分类.在成熟油田周边寻找滚动目标,可以在同等地质条件下拟合一个经验公式,从而实现目标区的厚度预测. With the exploration in Bohai area becoming more and more mature, the Bo’nan mining area in the southern Bohai Sea area is pursuing the goal of finding large and medium-sized oil and gas fields, taking into consideration the prospecting of rolling targets in the periphery of mature oilfields.The rolling targets are mainly shallow structures The target intervals are mainly located in the upper part of Ming and the lower part of Ming. The river-plains facies in the upper part of Ming Ming are interbedded with sand-mudstone. The plains-fluvial facies in the lower part of Ming-Ming are mudstone-sandstone with rapid lateral thickness changes. At present, the prediction of sand body thickness on earthquakes is inaccurately predicted in the limit resolution, ie the thickness of sand body over one quarter of the seismic wavelength is not accurate.In this paper, starting from the classic wedge model, the sand body thickness and peak frequency Then based on the data of rich wells in mature oilfield, the relationship between the peak frequency and different thickness of sand body is studied based on the statistics of multi-well production wells to fit the linear relationship suitable for the target area.Research shows that when Reservoirs containing pure oil will reduce the peak frequency of the sand body, and water will increase the peak frequency of the sand body, so the empirical formula fitting need to press the well point fluid Categorize. Looking at the surrounding rolling target mature fields, can fit an empirical formula in the same geological conditions, in order to achieve the predicted target zone thickness.
其他文献
1986年冬至1987年夏,我们将日本长崎县谏早市农业高等学校同学会副会长八江正吉先生赠送的19种菜籽在校内试种.每品种试种6~20米~2,定植于新植柑桔园间.试种结果,有8种表现较
第三届国际显示会议于1983年10月3日至5日在日本神户召开。6日与会代表到大阪参观了83年全日本电子工业展览会。我国电子工业部派了三人代表小组出席了会议,会后参观了日立
目的:盾构隧道在成层土中掘进时,地下水渗流容易引起盾构开挖面失稳破坏。本文提出考虑地下水渗流的机动场模型,探讨成层土中地下水渗流规律,研究渗流对开挖面稳定性的影响,
请下载后查看,本文暂不支持在线获取查看简介。 Please download to view, this article does not support online access to view profile.
期刊
  前寒武纪条带状铁建造(Banded Iron Formations,简称BIF)是早前寒武纪地球特殊环境的产物[1],多赋存于早前寒武古老变质岩系之中,通常指全铁含量大于15%,具有由富铁矿物(
云南省永平—巍山地区是我国西南"三江"地区重要的成矿区,区域上属于兰坪-思茅成矿带,是我国重要的铜金铅锌多金属成矿区,区内分布着各类中型多金属矿床.本文根据流体包裹体
会议
江西冷水坑银铅锌矿床位于华南地块北东缘的武夷隆起区,在构造上受鹰潭—安远深断裂及鹰潭—瑞昌区域性大断裂控制.冷水坑银铅锌矿床是我国重要的银铅锌矿床之一,前人对矿床
一柱香金矿床位于四川省甘孜州康定县舍联乡,是大渡河金成矿带近年来发现的具有较大规模的金矿床之一.矿床地质特征简介一柱香金矿床位于扬子地台西缘,康滇地轴北端,属川滇南
韭菜坪金矿床位于大渡河金矿成矿带北部,分布在前震旦系康定杂岩中.区域地球化学研究表明,韭菜坪所在的康定杂岩分布区是一个金相对富集的地球化学区,具有形成金矿的区域地球
会议