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81st EAGE Conference and Exhibition 2019最新文献

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Joint Using PP-Wave and PS-Wave Elastic Impedance to Construct Reservoir Sensitive Elastic Parameters 联合利用pp波和ps波弹性阻抗构建储层敏感弹性参数
Pub Date : 2019-06-03 DOI: 10.3997/2214-4609.201900679
J. Gui, J. Gao, K. Chen, S. Li, H. Wang, Q. Chen
Due to the different seismic amplitude information carried by PP-wave and PS-wave, the sensitive of PP-wave and PS-wave to reservoir are different. The joint using of PP-wave and PS-wave information can reduce the multi-solution of reservoir prediction. The construction of conventional elastic parameters is mainly based on PP-wave seismic information. This study investigates elastic parameter construction by using PP-wave and PS-wave elastic impedance jointly. Based on the previous research on PS-wave elastic impedance, a new form of PS-wave elastic impedance equation which can keep consistency with the PP-wave elastic impedance equation is derived. According to the construction formula of conventional elastic parameters, we use PP-wave and new PS-wave elastic impedance instead of P-wave and S-wave impedance to construct a new kind of elastic parameter with the concept of angle elastic parameter. Compared with the conventional elastic parameters, the angle elastic parameters have incidence angle and PS-wave information and can be used as sensitive indicators of reservoir. Both the model and real data show that the angle elastic parameters have high sensitivity to the beneficial reservoir.
由于pp波和ps波携带的地震振幅信息不同,导致pp波和ps波对储层的敏感性不同。pp波和ps波信息的联合利用,可以减少储层预测的多解性。常规弹性参数的构建主要基于pp波地震信息。本文研究了利用pp波和ps波弹性阻抗共同构建弹性参数的方法。在前人对ps波弹性阻抗研究的基础上,导出了一种与pp波弹性阻抗方程保持一致的ps波弹性阻抗方程。根据传统弹性参数的构造公式,用p波和新型ps波弹性阻抗代替p波和s波阻抗,用角度弹性参数的概念构造了一种新的弹性参数。与常规弹性参数相比,角度弹性参数具有入射角和ps波信息,可作为储层的敏感指标。模型和实测数据均表明,角度弹性参数对有利储层具有较高的敏感性。
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引用次数: 0
Integrated Simultaneous Joint and Full-Waveform Inversion Workflow for Multiphysics Near-Surface Modeling 多物理场近地表建模集成同步联合全波形反演工作流程
Pub Date : 2019-06-03 DOI: 10.3997/2214-4609.201900969
A. Sirtori, M. Mantovani, A. Epifani, F. Miotti
Summary Building a solid starting model remains one of the most challenging tasks for a robust application of full-waveform inversion (FWI). Several aspects can drive the FWI data optimization towards a local minimum of the cost function, such as the lack of low frequency, the offset limitation, and the presence of alternating high-low velocity layering in the stratigraphic sequence. This risk can be mitigated by geophysically preconditioning the FWI starting model, leveraging multiphysics independent measurement through simultaneous joint inversion. In this multiphysics multiscale approach, the seismic information is valuably coupled with non-seismic observations, with the potential benefit of reducing the non-uniqueness of surface geophysics inversions and increasing the robustness and fitness of the input model for FWI.
对于全波形反演(FWI)的稳健应用来说,建立一个可靠的起始模型仍然是最具挑战性的任务之一。有几个方面可以推动FWI数据优化,使成本函数达到局部最小,例如缺乏低频、偏移限制以及地层层序中存在高低速交替分层。通过对FWI启动模型进行物理预处理,通过同时联合反演利用多物理场独立测量,可以降低这种风险。在这种多物理场多尺度方法中,地震信息有效地与非地震观测相结合,减少了地表地球物理反演的非唯一性,提高了FWI输入模型的鲁棒性和适应度。
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引用次数: 1
Research on Spatial Rank Correlation Characteristics of Seismic Exploration Noise 地震勘探噪声空间秩相关特征研究
Pub Date : 2019-06-03 DOI: 10.3997/2214-4609.201901394
H. Lin, S. Li, Y. Li
In seismic exploration, seismic random noise is considered as temporal and spatial random process. Due to the complex environment of desert seismic exploration, the noise shows many different properties, such as: non-Gaussian, weak similarity and low frequency characteristics. Because it is highly unpredictable, it can only be qualitatively analyzed. We improves the Kendall’s rank correlation coefficient combining spatial information to investigate the spatial correlation property of the desert noise. Based on this method, the noise with spatial correlation is statistically calculated. The spatial correlation coefficient of the desert seismic data illustrate that the spatial rank correlation coefficient can reflect the noise spatial structure well and quantify the spatial correlation degree of noise. We find that desert noise has a spatially weak correlation property in which inconsistent noise is the main component. In addition, because there are few surface vegetation in desert areas, wind speed is also an important factor affecting the spatial noise of desert noise. Desert noise shows weaker spatial correlation after wind speed increases.
在地震勘探中,地震随机噪声被认为是一个时空随机过程。由于沙漠地震勘探环境的复杂,其噪声表现出非高斯、弱相似、低频等特征。因为它是高度不可预测的,所以只能进行定性分析。结合空间信息改进Kendall等级相关系数,研究沙漠噪声的空间相关特性。基于该方法,对具有空间相关性的噪声进行统计计算。沙漠地震资料的空间相关系数表明,空间等级相关系数能较好地反映噪声的空间结构,量化噪声的空间相关程度。研究发现,沙漠噪声具有空间弱相关特性,其中不一致噪声是主要成分。此外,由于沙漠地区地表植被较少,风速也是影响沙漠噪声空间噪声的重要因素。风速增大后,沙漠噪声的空间相关性减弱。
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引用次数: 0
Mathematical Morphological Filters and Applications in Seismic Data Denoising 数学形态滤波器及其在地震数据去噪中的应用
Pub Date : 2019-06-03 DOI: 10.3997/2214-4609.201900849
Z. Liu, D. Wheaton, V. Tyagi, B. Wang
Summary Mathematical morphological filtering (MMF) is a powerful tool for image processing based on the shape of the structure element (SE). It was introduced into seismic data processing to suppress noise and enhance signal quality. We explain the basic mathematic morphology concepts with set theory and define the basic and advanced morphological operations in seismic data processing. Unlike conventional seismic filtering techniques, MMF is a nonlinear operator so that it can more effectively isolate and attenuate seismic noise based on their shape differences from the signal. We apply different types of morphological filter on field (and various stages of processed) data to demonstrate their effectiveness for suppression of both coherent and incoherent noise and results in an improvement of signal to noise ratio.
数学形态滤波(MMF)是一种基于结构元素(SE)形状的图像处理工具。将其引入地震数据处理中,以抑制噪声,提高信号质量。用集合理论解释了数学形态学的基本概念,定义了地震数据处理中形态学的基本操作和高级操作。与传统的地震滤波技术不同,MMF是一种非线性算子,因此它可以根据地震噪声与信号的形状差异更有效地隔离和衰减地震噪声。我们将不同类型的形态学滤波器应用于现场(以及处理的各个阶段)数据,以证明它们对抑制相干和非相干噪声的有效性,并导致信噪比的提高。
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引用次数: 1
A Hybrid FWI-JMI for High Resolution Velocity Estimation 一种用于高分辨率速度估计的混合wifi - jmi
Pub Date : 2019-06-03 DOI: 10.3997/2214-4609.201901228
M. Ishak, D. Verschuur, A. R. Ghazali
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引用次数: 1
North Sea Field Application of 4D Bayesian Inversion to Pressure and Saturation Changes 北海油田四维贝叶斯反演在压力和饱和度变化中的应用
Pub Date : 2019-06-03 DOI: 10.3997/2214-4609.201900686
G. Côrte, C. MacBeth, H. Amini
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引用次数: 2
A Hierarchical Carbonate Reservoir Benchmarking Case Study For Reservoir Characterisation, Uncertainty Quantification & History Matching 用于储层表征、不确定性量化和历史匹配的分层碳酸盐岩储层基准案例研究
Pub Date : 2019-06-03 DOI: 10.3997/2214-4609.201901631
J. Gomes, S. Geiger, D. Arnold
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引用次数: 2
Smart Waterflooding of Homogeneous and Heterogeneous Cores from Carbonaceous Reservoir 碳质储层均质和非均质岩心智能水驱
Pub Date : 2019-06-03 DOI: 10.3997/2214-4609.201900717
Jiasheng Hao, Samira Mohammadkhani, K. Feilberg, A. Shapiro
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引用次数: 0
Paleozoic Carbonates Record the 4D evolution of Salt Domes in the Barents Sea 巴伦支海古生代碳酸盐岩记录了盐丘的四维演化
Pub Date : 2019-06-03 DOI: 10.3997/2214-4609.201901559
T. Alves
During the Late Paleozoic, the Barents Sea was at the edge of the Pangea Supercontinent, recording major climatic and oceanographic changes in the large Panthalassa Ocean (Shulgin et al., 2018). These changes preclude major tectonic events in the Urals and further south, in Central Europe (Faleide et al., 1993; Glorstad‐Clark et al., 2010). This paper focuses on a region located ~150 km to the North of Finnmark, in Northern Norway (Fig. 1). It relates, for the first time, how the geometry and distribution of Carboniferous and Permian mounds relates to vertical movements of the Samson Dome, and adjacent platform areas (Fig. 1a). In essence, this work will demonstrated Samson Dome area presented a much different palaeogeography in the Carboniferous and Permian from the present day, hinting at the presence of sheltered (shallow) platform areas away from the salt structures that are imaged, on seismic data, at present (Figs. 1b and 1c). The identification of such sheltered areas suggests that either: a) older salt structures (pillows, ridges) existed away from the Samson Dome and salt was subsequently withdrawn from below them during the Mesozoic, or b) important vertical movements in the Mesozoic led to the subsidence of Paleozoic carbonate platforms.
晚古生代,巴伦支海处于盘古超大陆的边缘,记录了大泛海海洋的主要气候和海洋学变化(Shulgin et al., 2018)。这些变化排除了乌拉尔和中欧更南部的主要构造事件(Faleide et al., 1993;glostad - Clark et al., 2010)。本文的研究重点是位于挪威北部Finnmark北部约150公里处的一个区域(图1)。本文首次阐述了石炭系和二叠纪土丘的几何形状和分布与Samson Dome及其邻近平台区域的垂直运动之间的关系(图1a)。从本质上讲,这项工作将证明Samson Dome地区在石炭纪和二叠纪时期呈现出与现在截然不同的古地理,暗示在目前地震数据成像的盐构造之外存在遮蔽(浅)台地区域(图1b和1c)。对这些遮蔽区域的识别表明:a)较古老的盐构造(枕状、脊状)在远离参孙丘的地方存在,随后在中生代期间盐从其下方被抽走;b)中生代重要的垂直运动导致古生代碳酸盐岩台地下沉。
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引用次数: 1
Development of a Robust Correlation to Determine an Oil Production Rate through Vapor Extraction 通过蒸汽萃取确定产油量的鲁棒相关性的发展
Pub Date : 2019-06-03 DOI: 10.3997/2214-4609.201901650
M. Ahmadi, Z. Chen
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引用次数: 0
期刊
81st EAGE Conference and Exhibition 2019
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