...
首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >Application of high-resolution 2D-3C seismic for characterization of the perspective Jurassic shale play in Central Poland
【24h】

Application of high-resolution 2D-3C seismic for characterization of the perspective Jurassic shale play in Central Poland

机译:高分辨率2D-3C地震在波兰中部侏罗纪页岩游隙特征描述中的应用

获取原文
获取原文并翻译 | 示例

摘要

Here we show the application of broadband (4-120 Hz) 2D-3C seismic for characterization of the perspective Jurassic shale play in Central Poland. Data were acquired along a network of 250 km 2D profiles using single point, densely spaced receivers (digital 3C sensors) and acquisition was focused on providing both high resolution and broadband seismic that would enable structural imaging and quantitative interpretation of the key stratigraphic horizons in the Mesozoic sedimentary cover. Such acquisition parameters resulted in good quality data and allowed for more flexibility during processing, e.g., unaliased F-K filtering or digital group forming for ground-roll removal. Processing was oriented to preserve relative amplitudes and the broadband character of the dataset as the input for future quantitative interpretation. We obtained a high-resolution stratigraphic image of the target Upper Jurassic (Upper Kimmeridgian-Tithonian) sequence as well as overall structural portrait of this part of Mid-Polish Trough characterized by strong imprint of the salt tectonics. Lateral continuity of particular stratigraphic sequences has been determined and a more precise structural context for deposition and present-day structure of the Upper Kimmeridgian-Tithonian has been established. (C) 2015 Elsevier B.V. All rights reserved.
机译:在这里,我们展示了宽带(4-120 Hz)2D-3C地震在表征波兰中部侏罗纪页岩游动角度方面的应用。使用单点密集间隔的接收器(数字3C传感器)沿250 km 2D剖面网络采集数据,采集的重点在于提供高分辨率地震和宽带地震,这将使构造成像和定量解释关键地层范围成为可能。中生代沉积层。这样的采集参数产生了高质量的数据,并在处理过程中提供了更大的灵活性,例如,无混叠F-K滤波或用于去除地滚的数字组形成。处理的方向是保留数据集的相对振幅和宽带特征,以作为将来定量解释的输入。我们获得了目标上侏罗统(基米底吉安-提通天体)层序的高分辨率地层图像,以及中波谷这一部分的整体结构肖像,其特征是盐构造强烈的烙印。确定了特定地层层序的侧向连续性,并建立了上基默尔第纪-提通纪沉积和当今结构的更精确的结构背景。 (C)2015 Elsevier B.V.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号