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1. 发明申请

WO2006031383A3 GEOLOGIC MODELS OF SUBSURFACE SEDIMENTRAY VOLUMES 审中-公开
标题翻译：地表沉积体积的地质模型
公开(公告)号：WO2006031383A3
公开(公告)日：2006-05-11
申请号：PCT/US2005029753
申请日：2005-08-19
申请人： EXXONMOBIL UPSTREAM RES CO , VAN WAGONER JOHN C , DUNN PAUL A , DEFFENBAUGH MAX , AWWILLER DAVID N , SUN TAO , LI DACHANG , HOYAL DAVID C , DONOFRIO CHRIS J
发明人： VAN WAGONER JOHN C , DUNN PAUL A , DEFFENBAUGH MAX , AWWILLER DAVID N , SUN TAO , LI DACHANG , HOYAL DAVID C , DONOFRIO CHRIS J
IPC分类号： G06T17/20
CPC分类号： G01V1/282 , G01V2210/661
摘要： A 3-Dseismic image is used to construct a geologic model specifying the spatially varying grain size distribution, porosity and permeability through the volume 101. The method applies to water laid elastic sedimentary deposits of earth sedentary volumes and involves modeling steps for identifying the outline forms of geologic bodies in geologic data. The outline forms of the geologic deposits and body volume form is used to determine the spatially varying grain size distribution within the sediment deposit and is guided by the modeling assumptions about the nature and behavior of the sediment paleoflow that deposited the sediment volume 109. The geologic sediment volume is based on the grain size distribution of mineralogy and sediment burial history information and is used to determine the rock properties of porosity and permeability within the geological sedimentation deposit 101.
摘要翻译：三维地震图像用于构建一个地质模型，指定空间变化的粒度分布，孔隙度和渗透率通过体积101.该方法适用于地球静止体积的铺放弹性沉积沉积物，并涉及用于识别轮廓形式的建模步骤地质资料中的地质体。地质沉积物和体积形态的轮廓形式用于确定沉积物沉积物内的空间变化的粒度分布，并通过沉积沉积物体积109的沉积物古流的性质和行为的模型假设来指导。地质学沉积物体积基于矿物学和沉积物埋藏历史信息的粒度分布，用于确定地质沉积沉积物中孔隙度和渗透率的岩石性质101。

2. 发明申请

WO2006036389A2 A METHOD FOR EVALUATING SEDIMENTARY BASIN PROPERTIES BY NUMERICAL MODELLING OF SEDIMENTATION PROCESSES 审中-公开
标题翻译：通过数字化建模过程评估沉积盆地性质的方法
公开(公告)号：WO2006036389A2
公开(公告)日：2006-04-06
申请号：PCT/US2005029884
申请日：2005-08-23
申请人： EXXONMOBIL UPSTREAM RES CO , SUN TAO , LI DACHANG , DEFFENBAUGH MAX , HUH CHUN , HOYAL DAVID C , ADAIR NEAL , WU XIAO-HUI , CHARTRAND TIMOTHY A , VAN WAGONER JOHN C
发明人： SUN TAO , LI DACHANG , DEFFENBAUGH MAX , HUH CHUN , HOYAL DAVID C , ADAIR NEAL , WU XIAO-HUI , CHARTRAND TIMOTHY A , VAN WAGONER JOHN C
CPC分类号： G01V1/282 , G01V99/00 , G01V2210/661
摘要： A method is disclosed for simulating the formation of sedimentary deposits. In one embodiment, this method involves, (a) solving a two-dimensional time-dependent map view system of equations for at least flow momentum, flow height, suspended sediment concentration, and entrainment of overlying water, (b) calculating net sediment deposition at each map view location using the flow properties, (c) recording the time-variability of the net sediment deposition.
摘要翻译：公开了一种模拟沉积沉积物形成的方法。在一个实施例中，该方法涉及（a）解决至少流动动量，流动高度，悬浮泥沙浓度和上覆水夹带的方程的二维时间依赖地图视图系统，（b）计算净沉积物沉积在每个地图视图位置使用流动属性，（c）记录净沉积物沉积的时间变异性。

3. 发明申请

WO2006007466A3 HYDRODYNAMICS-BASED GRIDDING GEOLOGIC MODELING (HYDRO-GRIDDING) 审中-公开
标题翻译：基于水力发电的地质建模（水文地质）
公开(公告)号：WO2006007466A3
公开(公告)日：2006-05-04
申请号：PCT/US2005021991
申请日：2005-06-24
申请人： EXXONMOBIL UPSTREAM RES CO , LI DACHANG , SUN TAO , HUH CHUN , DONOFRIO CHRIS J , DEFFENBAUGH MAX , VAN WAGONER JOHN C
发明人： LI DACHANG , SUN TAO , HUH CHUN , DONOFRIO CHRIS J , DEFFENBAUGH MAX , VAN WAGONER JOHN C
IPC分类号： G01V1/00
CPC分类号： G01V1/306 , G01V1/282 , G01V2210/661
摘要： The method for creating geologic subsurface models using hydrodynamics-based gridding (Hydro-Grids) for subsurface volumes and reservoirs (35). Wherein, the vertical grid surfaces are chosen in an unstructured fashion to provide lateral resolution as needed (31). The lateral grid surfaces created represent surfaces of constant geological time based on simulations of the depositional processes of the subsurface volume. The geologic properties are specified within each cell created by the intersections of the vertical and lateral surfaces. The geologic data includes the seismic data, the outcrop studies data and well log data and core data and numerical data, and modeling data and interpreted stratigraphic surfaces based on seismic data. The modeled geologic properties of the subsurface volume include the grain size distribution, the connectivity, and the net to gross data, the porosity, the permeability and the pore pressure.
摘要翻译：使用基于流体动力学网格（Hydro-Grids）为地下体积和储层创建地质地下模型的方法（35）。其中，以非结构化的方式选择垂直网格表面以根据需要提供横向分辨率（31）。基于地下体积沉积过程的模拟，创建的横向网格表面代表恒定地质时间的表面。地质属性在由垂直和侧面的交点创建的每个单元格中指定。地质资料包括地震数据，露头研究数据和测井数据以及核心数据和数值数据，以及基于地震数据的建模数据和解释地层表面。地下体积的模拟地质特征包括粒度分布，连通性，净数与总数，孔隙度，渗透率和孔隙压力。

4. 发明申请

WO2004083896A3 METHOD FOR PREDICTING GRAIN SIZE DISTRIBUTION FROM RESERVOIR THICKNESS 审中-公开
标题翻译：从储层厚度预测颗粒大小分布的方法
公开(公告)号：WO2004083896A3
公开(公告)日：2004-12-29
申请号：PCT/US2004005019
申请日：2004-02-20
申请人： EXXONMOBIL UPSTREAM RES CO , DEFFENBAUGH MAX , HEARD WILLIAM B , HUH CHUN , SUN TAO , HOYAL DAVID C
发明人： DEFFENBAUGH MAX , HEARD WILLIAM B , HUH CHUN , SUN TAO , HOYAL DAVID C
IPC分类号： G01V1/28
CPC分类号： G01V1/306 , G01V1/282 , G01V2210/661
摘要： A method for predicting the grain size distribution at a designated location within a water-lain sedimentary deposit (50) with steps of determining the vertical thickness of the sedimentary deposit at the designated location as well as the vertical thickness and grain size distribution at a second location different from the designated location (52) and determining the distance parameter corresponding to the two locations. And finally the distance parameter is used with the initially determined vertical thickness at both locations and the grain size distribution at the second location is used to calculate the grain size distribution at the designated location (52).
摘要翻译：一种用于预测水沉积沉积物（50）内指定位置的粒度分布的方法，其步骤是确定在指定位置处的沉积物的垂直厚度以及第二次沉积沉积物的垂直厚度和粒度分布位置不同于所述指定位置（52）并且确定与所述两个位置对应的所述距离参数。最后，距离参数与两个位置处初始确定的垂直厚度一起使用，并且第二位置处的粒度分布用于计算指定位置处的粒度分布（52）。

5. 发明申请

WO2004093521A3 METHOD TO DETERMINE PROPERTIES OF A SEDIMENTARY BODY FROM THICKNESS AND GRAIN SIZE DISTRIBUTION AT A POINT WITHIN THE BODY 审中-公开
标题翻译：确定体内物质厚度和粒度分布特征的方法
公开(公告)号：WO2004093521A3
公开(公告)日：2005-10-06
申请号：PCT/US2004008238
申请日：2004-03-18
申请人： EXXONMOBIL UPSTREAM RES CO , DEFFENBAUGH MAX , HOYAL DAVID C , ADAIR NEAL L , HUH CHUN
发明人： DEFFENBAUGH MAX , HOYAL DAVID C , ADAIR NEAL L , HUH CHUN
IPC分类号： E21B20060101 , G01V1/30 , G01V7/00
CPC分类号： G01V1/30 , G01V1/306 , G01V2210/661
摘要： A method to determine the properties of a water-lain sediment body (16) from a measurement of grain size distribution and deposit thickness at one location in the deposited sediment body. Using method modeling steps to determine the flow properties at the measuring location and extrapolating the flow properties back to the fluid inlet through which the depositing flow were emitted and providing computation steps for determining a property of the water-lain sediment throughout the sediment deposit body using modeling of the fluid properties with extrapolated flow properties at the inlet set as the boundary condition.
摘要翻译：通过测量沉积物体中一个位置的粒度分布和沉积厚度，确定水体沉积物体（16）的性质的方法。使用方法建模步骤来确定测量位置处的流动特性并将流动特性外推回到流体入口，通过该流体入口排放沉积流，并提供计算步骤，用于确定整个沉积物沉积体中的水体沉积物的性质，使用在入口设定为外部条件的外推流量特性的流体特性建模。

6. 发明申请

WO2005104003A8 METHOD FOR CONSTRUCTING A GEOLOGIC MODEL OF A SUBSURFACE RESERVOIR 审中-公开
标题翻译：构造地表储层地质模型的方法
公开(公告)号：WO2005104003A8
公开(公告)日：2011-08-11
申请号：PCT/US2005005358
申请日：2005-02-22
申请人： EXXONMOBIL UPSTREAM RES CO , DEFFENBAUGH MAX , DUNN PAUL A
发明人： DEFFENBAUGH MAX , DUNN PAUL A
IPC分类号： E21B49/00 , G01V1/30 , G06G7/48 , G06G7/50
CPC分类号： E21B49/00 , G01V1/301
摘要： The present invention is a method for constructing a geologic model of a subsurface reservoir which is a composite sedimentary body (30) composed of many smaller fundamental sedimentary bodies (32). In one embodiment, the fundamental sedimentary bodies (32) within the composite body (30) are specified by the properties of the flow which built them, including the flow properties that existed at the local inlet (36) of each fundamental body (32). The statistical distribution of these local inlet properties is characterized throughout the fundamental composite sedimentary body (30) using either outline forms of some of the fundamental sedimentary bodies (32) or a well penetration core which samples the composite sedimentary body (30). The geologic model is constructed by placing an appropriate statistical distribution of the fundamental sedimentary bodies (32) into the outline form of the composite sedimentary body (30) so that the grain size distribution and/or other geologic properties are is specified at each point within the composite sedimentary body (30).
摘要翻译：本发明是一种构造地下储层的地质模型的方法，该地下储层是由许多较小的基底沉积体组成的复合沉积体（30）（32）。在一个实施例中，复合体（30）内的基础沉积体（32）由构成它们的流动特性来确定，包括存在于每个基体（32）的局部入口（36）处的流动性质，。这些局部入口性质的统计分布在整个基础复合沉积体（30）中的特点是使用一些基本沉积体（32）的轮廓形式或对复合沉积体（30）进行取样的井渗透芯。地质模型是通过将基础沉积体（32）的适当统计分布放置在复合沉积体（30）的轮廓形式中构成的，以便在每个点内规定粒度分布和/或其他地质特性复合沉积体（30）。

7. 发明申请

WO2008123920A8 SEPARATION AND NOISE REMOVAL FOR MULTIPLE VIBRATORY SOURCE SEISMIC DATA 审中-公开
标题翻译：多个振动源地震数据的分离和噪声去除
公开(公告)号：WO2008123920A8
公开(公告)日：2009-03-26
申请号：PCT/US2008003599
申请日：2008-03-19
申请人： EXXONMOBIL UPSTREAM RES CO , NEELAMANI RAMESH , KROHN CHRISTINE E , KREBS JERRY , DEFFENBAUGH MAX , ANDERSON JOHN
发明人： NEELAMANI RAMESH , KROHN CHRISTINE E , KREBS JERRY , DEFFENBAUGH MAX , ANDERSON JOHN
IPC分类号： G01V1/00
CPC分类号： G01V1/37 , G01V1/005 , G01V2210/127 , G01V2210/32
摘要： The invention discloses a way to recover separated seismograms with reduced interference noise by processing vibroseis data recorded (or computer simulated) with multiple vibrators shaking simultaneously or nearly simultaneously (200). A preliminary estimate of the separated seismograms is used to obtain improved seismograms (201). The preliminary estimate is convolved with the vibrator signature and then used to update the seismogram. Primary criteria for performing the update include fitting the field data and satisfying typical criteria of noise-free seismograms (202). Alternative ways to update are disclosed, including signal extraction, modeled noise extraction, constrained optimization based separation, and penalized least-squares based separation. The method is particularly suited for removing noise caused by separating the combined record into separate records for each vibrator, and is advantageous where the number of sweeps is fewer than the number of vibrators (200).
摘要翻译：本发明公开了一种通过利用多个振动器同时或几乎同时振动（200）处理记录（或计算机模拟）的震动数据来恢复具有降低的干扰噪声的分离的地震图的方法。使用分离地震图的初步估计来获得改进的地震图（201）。初步估计与振动器签名一起卷积，然后用于更新地震图。执行更新的主要标准包括拟合现场数据并满足无噪声地震图的典型标准（202）。公开了替代的更新方式，包括信号提取，建模噪声提取，基于约束优化的分离以及基于最小二乘法的惩罚分离。该方法特别适用于消除由组合记录分离为每个振动器的独立记录而引起的噪声，并且在扫描次数少于振动器数目（200）的情况下是有利的。

8. 发明申请

WO2004106974A3 METHOD FOR PREDICTING GRAIN SIZE DISTRIBUTION FROM THE SHAPE OF A SEDIMENTARY BODY 审中-公开
标题翻译：用于预测颗粒形状的尺寸分布的方法
公开(公告)号：WO2004106974A3
公开(公告)日：2005-06-23
申请号：PCT/US2004015896
申请日：2004-05-20
申请人： EXXONMOBIL UPSTREAM RES CO
发明人： DEFFENBAUGH MAX , VAN WAGONER JOHN C , HUH CHUN , SUN TAO
IPC分类号： G01V20060101 , G01V1/28 , G01V1/30 , G06F19/00
CPC分类号： G01V1/282 , G01V1/306
摘要： The internal properties of a water-lain sediment body can be determined from the shape of the deposit. One method comprises solving equations relating the shape of a sediment body to the flow field that produced the body and using the flow field to solve for the sediment body properties in at least one point within the body. The flow field properties include flow velocity, suspended sediment volume fractions, deposition time, and flow height. The properties of the water-lain sediments include, in addition to the flow properties associated with deposition of the sediments, the thickness of the sediment body, the size of the body, the shape of the body, and the grain size distribution at points within the body.
摘要翻译：水沉积物的内部特性可以根据沉积物的形状来确定。一种方法包括将沉积物的形状与产生身体的流场相关联的方程式，并且使用流场来解决体内至少一个点的沉积物体性质。流场特性包括流速，悬浮物体积分数，沉积时间和流动高度。除了与沉积物沉积相关的流动性质，沉积物的厚度，体的大小，体的形状，以及在内部的点内的颗粒尺寸分布之外，水沉积物的性质还包括身体。

9. 发明申请

WO2004099816A2 METHOD FOR PREDICTING PROPERTIES OF A SEDIMENTARY DEPOSIT FROM A THICKNESS CONTOUR OF THE DEPOSIT 审中-公开
标题翻译：从沉积物的厚度方向预测沉积物的性质的方法
公开(公告)号：WO2004099816A2
公开(公告)日：2004-11-18
申请号：PCT/US2004012436
申请日：2004-04-22
申请人： EXXONMOBIL UPSTREAM RES CO
发明人： DEFFENBAUGH MAX , VAN WAGONER JOHN C , ADAIR NEAL L
IPC分类号： G01V20060101 , G01V1/30 , G01V3/00 , G01V7/00 , G06F19/00 , G01V
CPC分类号： G01V1/306
摘要： The properties of a water-lain sedimentary deposit may be predicted at any location from a contour of constant deposit thickness. One embodiment of the method comprises (a) determining an outline of constant deposit thickness in a measured deposit, (b) determining the fluid flow properties at the inlet of the measured deposit, (c) determining a property of the deposit at any point inside the deposit from modeling the fluid flow. The properties of the deposit at any point may include the thickness of the sediment body, the size of the body, the shape of the body, and the grain size distribution at each point within the body, and any combination thereof.
摘要翻译：可以从恒定沉积厚度的轮廓的任何位置预测水沉积沉积物的性质。该方法的一个实施例包括（a）确定测量沉积物中恒定沉积物厚度的轮廓，（b）确定测量沉积物入口处的流体流动性质，（c）确定沉积物在任何点内的性质沉积物从流体流动建模。沉积物在任何点的性质可以包括沉积物的厚度，体的大小，体的形状，以及体内各点的粒度分布，以及它们的任何组合。

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