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Fracture patterns, lineaments and seismic reflection data: Integration for fault mapping in the Appalachian Basin of east-central New York State.

机译:断裂模式,地层和地震反射数据:纽约州中东部阿巴拉契亚盆地断层测绘的积分。

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摘要

This study integrates surface structure data with faults observed in 2-D seismic reflection profiles and lineaments identified from aeromagnetic gradients, DEMs, slope aspect, and satellite imagery in order to map probable fault patterns. The study area is located in the Middle to Upper Devonian Catskill Delta Complex in the Appalachian Basin in central New York State. This previously unmapped study area is significant because of active oil and gas exploration in the region.; Several characteristics of surface bedrock fractures were collected within the study area. Fracture characteristics include orientation, dip, spacing, fracture abutting relationships and fracture geometry. Fracture characteristics are displayed using modified rose diagrams to illustrate trends in orientation, frequency and fracture relationships. Three regional fracture orientations are common in the area. Fracture Intensification Domains (FIDs) are characterized by relatively closely spaced fractures; FIDs can indicate areas where faulting is probable. Each of the three regional fracture orientations have zones of closely spaced fractures. FIDs recognized at the surface correlate spatially with thrust and high angle faults observed in 2-D seismic and with lineaments.; Lineaments identified from satellite imagery, DEMs, and aeromagnetic gradients are combined with exposed bedrock fracture data and seismic reflection data. Two anomalously long NW-striking aeromagnetic lineaments are located in the center of the study area. NNE- and NS-striking lineaments are dense where appropriately trending aeromagnetic gradients are located. NNE-, WNW-, ENE-striking lineaments are also coincident with fractures and FID orientations. The integration of these data promote mapping of FIDs in order to define areas with a higher probability of faults. This fault map will point to exploring areas that should be high-graded in the exploration for fractured-plays.
机译:这项研究将表面结构数据与从地震波梯度,DEM,坡度和卫星图像中识别出的二维地震反射剖面和沿线中观察到的断层进行了整合,以便绘制出可能的断层图。研究区域位于纽约州中部阿巴拉契亚盆地的中上泥盆统卡茨基尔三角洲综合体。由于该地区正在积极进行油气勘探,因此该先前未映射的研究区域意义重大。在研究区域内收集了表层基岩裂缝的一些特征。断裂特征包括取向,倾角,间距,断裂邻接关系和断裂几何形状。使用修改后的玫瑰图显示断裂特性,以说明取向,频率和断裂关系的趋势。该区域常见三种区域性裂缝取向。骨折强化域(FID)的特征是骨折间距相对较近。 FID可以指示可能发生故障的区域。三个区域裂缝取向中的每一个都具有紧密间隔的裂缝区域。在地面上识别的FID在空间上与在2D地震中观测到的逆冲断层和大角度断层以及与构造有关。从卫星图像,DEM和航空磁梯度中识别出的线性与裸露的基岩裂缝数据和地震反射数据结合在一起。在研究区域的中心,有两个异常长的西北空袭气动磁质。 NNE和NS打击的线条浓密,并有适当趋势的航磁梯度。 NNE,WNW和ENE的冲击线也与裂缝和FID方向一致。这些数据的集成促进了FID的映射,以便定义故障可能性更高的区域。该断层图将指出在勘探裂缝裂缝时应高度分级的地区。

著录项

  • 作者

    Terech, Nicholas.;

  • 作者单位

    State University of New York at Buffalo.;

  • 授予单位 State University of New York at Buffalo.;
  • 学科 Geology.; Remote Sensing.
  • 学位 M.S.
  • 年度 2006
  • 页码 270 p.
  • 总页数 270
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;遥感技术;
  • 关键词

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