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Ocean crustal drilling at the Hawaii-2 Observatory

机译:夏威夷2天文台的海洋地壳钻探

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In preparation for a permanent borehole seismometer at the Hawaii-2 Observatory (H2O) site, Ocean Drilling Project Leg 200 drilled Hole 1224D 1.48 km northeast of the H2O junction box. A reentry cone and cemented casing were installed through 28 m of soft, red clay and 30 m into basaltic basement. The cased basement interval consisted of massive basalt flows that had been cemented by calcite and it should provide good coupling for the seismometer to true earth motion. We also drilled a second single-bit hole, which was cored and logged, within 20 m of the first to a depth of 145 m into basement. The second hole was left with a free-fall funnel so that it also could be reentered using the wireline reentry technology to carry out other borehole experiments at the site. A suite of shipboard physical properties, well log, chemical and microbiological analyses that can be used to characterize the crust surrounding the observatory, was carried out. Measurements of ship noise during the drilling operations were also acquired on the shallow buried seismometer at the Hawaii-2 observatory.
机译:为在Hawaii-2天文台(H2O)现场准备永久钻孔地震仪,Ocean Drilling Project Leg 200在H2O接线盒东北1.48公里处钻了1224D孔。通过28 m的软红粘土和30 m的玄武岩地下室安装了一个折返锥和水泥套管。套管地下室间隔由方解石胶结的大量玄武岩流组成,应该为地震仪与真实的地球运动提供良好的耦合。我们还钻出了第二个单孔,该孔已取芯并记录下来,距第一个单孔不到20 m,至地下室的深度为145 m。第二个孔留有自由下落的漏斗,因此也可以使用电缆再入技术将其重新进入现场进行其他钻孔实验。进行了一系列船上物理性能,测井,化学和微生物学分析,可用于表征天文台周围的地壳。在夏威夷2号天文台的浅埋地震仪上也获得了钻井作业中船舶噪声的测量值。

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