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Determination of principal stress orientations from wireline logging caliper data and borehole images in deep drilling

机译:深井中钻井井线数据和钻孔图像的主应力取向的确定

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During IODP Expedition 319, a deep ocean borehole was drilled in the center of the Kumano forearc basin in the south-west Japan Nankai subduction zone, as a part of the scientific ocean drilling project called NanTroSEIZE. The borehole penetrated the Kumano forearc basin sediments and the underlying accretionary prism. In a depth range from approximately 700 mbsf (meters below seafloor) to the target depth of 1600 mbsf, wireline logging was carried out including caliper and the FMI borehole images. I used both the borehole images and caliper data to identify borehole breakouts that could be interpreted in terms of principal horizontal stress orientations. The results of stress orientaion determination and thier scien-tifc interpretations have been published (Lin et al., 2010). This report is focused on the method of stress orientation analyses based on borehole breakouts.
机译:在IODP探险队在319期间,在日本南南南南南开郊区的Kumano Forearc盆地的中心钻了一座深海钻孔,作为称为Nantroseize的科学钻探项目的一部分。钻孔穿透了Kumano Forearc盆地沉积物和潜在的增生棱镜。在深度范围内,从大约700 MBSF(海底下方)到目标深度为1600 MBSF,进行了有线测井,包括卡尺和FMI钻孔图像。我使用了钻孔图像和卡尺数据来识别可以在主要水平应力取向方面解释的钻孔突破。出版了应力Riadenion确定和Scien-TIFC解释的结果(Lin等人,2010)。本报告专注于基于钻孔突破的应力取向分析方法。

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