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Identification, Characterization and Analysis of Wrench Related Faulting in Southwestern Warren County, Kentucky

机译:肯塔基州西南沃伦县与扳手相关的断层的识别,表征和分析

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摘要

Warren County, Kentucky is located south of the southern boundary of the Rough Creek Graben marked by the Pennyrile fault system. The Pennyrile fault system is a regional southwest-northeast trending fault system that extends into Kentucky from the Reelfoot rift zone. The Rough Creek fault system bounds the northern arm of the Rough Creek Graben and trends northwest-southeast also extending from the Reelfoot rift zone. The Rough Creek fault system is related to the Shawneetown fault system in southeastern Illinois and occupies the southern end of the Illinois Basin. The East Continent Rift Basin intersects the Rough Creek Graben near its Eastern terminus and is parallel and west of the Grenville front. The structure under investigation in this paper was discovered west of the town of Woodburn, Kentucky. In 1992, West Bay Exploration Company of Michigan conducted a seismic survey of the Woodburn area and produced a series of two-dimensional profiles of the subsurface extending down to the Precambrian basement. Analysis of these profiles revealed a number of u27pop-upsu27 or possible wrench-related structures that can be traced upward through faulting from the Precambrian basement through the Knox Group and into the Mississippian section. Recent analysis of well log, seismic, and Radar images indicate extensive faulting in the Woodburn area indicative of wrench-fault related activity. A convincing surface expression of the deeper structure can be discerned from Radar imaging, aeromagnetic, and topographic maps of the region. An anomalous concentration of sinkholes is also visible from topographic maps and is aligned parallel to the curvature of the wrench structure on its western, southern, and eastern flanks.Wrench faults and associated structures are known to be productive traps for petroleum. West Bay Exploration Company of Traverse City Michigan drilled the subject structure in 1993 but the borehole test proved negative. Nonetheless, a detailed analysis of the subsurface using GIS and related software should aid in developing a prospecting tool for exploration geologists and aid in understanding the characteristic geologic sections of the Rough Creek Graben.
机译:肯塔基州沃伦县位于Rough Creek Graben南部边界的南部,以Pennyrile断层系统为标志。 Pennyrile断层系统是一个西南偏北走向的区域性断层系统,从Reelfoot裂谷带延伸到肯塔基州。 Rough Creek断层系统界定了Rough Creek Graben的北臂,并向西北偏东南方向延伸,也从Reelfoot裂谷带延伸。 Rough Creek断层系统与伊利诺伊州东南部的Shawneetown断层系统有关,并位于伊利诺伊盆地的南端。东大陆裂谷盆地在其东终点附近与Rough Creek Graben相交,并且与Grenville锋线平行并在其西部。本文所研究的结构是在肯塔基州伍德本镇以西发现的。 1992年,密歇根州的西湾勘探公司对伍德本地区进行了地震勘测,并绘制了一系列二维剖面,一直延伸到前寒武纪基底。对这些剖面的分析揭示了一些 u27pop-ups u27或可能与扳手相关的结构,这些结构可以通过从前寒武纪基底穿过诺克斯组并进入密西西比地区进行向上追踪。最近对测井,地震和雷达图像的分析表明,伍德本地区发生了广泛的断层,表明与扳手断层有关的活动。可以从该区域的雷达成像,航空磁和地形图中辨别出更深层结构的令人信服的表面表达。从地形图上也可以看到异常集中的陷坑,并与扳手结构的西,南和东侧面的扳手结构的曲率平行排列。众所周知,扳手断层和相关结构是石油的生产陷阱。密歇根州特拉弗斯市的西湾勘探公司于1993年对主体结构进行了钻探,但钻孔测试被证明是阴性的。但是,使用GIS和相关软件对地下进行详细分析应该有助于开发勘探地质学家的勘探工具,并有助于理解Rough Creek Graben的特征地质部分。

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    Islas Joseph;

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