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首页> 外文期刊>Scientific Drilling >IODP Expedition 319, NanTroSEIZE Stage 2: First IODP Riser Drilling Operations and Observatory Installation Towards Understanding Subduction Zone Seismogenesis
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IODP Expedition 319, NanTroSEIZE Stage 2: First IODP Riser Drilling Operations and Observatory Installation Towards Understanding Subduction Zone Seismogenesis

机译:IODP Expedition 319,NanTroSEIZE阶段2:首次IODP立管钻探操作和天文台安装,旨在了解俯冲带地震成因

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The Nankai Trough Seismogenic Zone Experiment(NanTroSEIZE) is a major drilling project designed toinvestigate fault mechanics and the seismogenic behaviorof subduction zone plate boundaries. Expedition 319 is thefirst riser drilling operation within scientific ocean drilling.Operations included riser drilling at Site C0009 in the forearcbasin above the plate boundary fault, non-riser drillingat Site C0010 across the shallow part of the megasplay faultsystem – which may slip during plate boundary earthquakes – and initial drilling at Site C0011 (incoming oceanicplate) for Expedition 322. At Site C0009, new methods weretested, including analysis of drill mud cuttings and gas, andin situ measurements of stress, pore pressure, and permeability.These results, in conjunction with earlier drilling,will provide (a) the history of forearc basin development(including links to growth of the megasplay fault system andmodern prism), (b) the first in situ hydrological measurementsof the plate boundary hanging wall, and (c) integrationof in situ stress measurements (orientation and magnitude)across the forearc and with depth. A vertical seismic profile(VSP) experiment provides improved constraints on thedeeper structure of the subduction zone. At Site C0010,logging-while-drilling measurements indicate significantchanges in fault zone and hanging wall properties overshort (< 5 km) along-strike distances, suggesting differentburial and/or uplift history. The first borehole observatoryinstruments were installed at Site C0010 to monitorpressure and temperature within the megasplay fault zone,and methods of deployment of more complex observatoryinstruments were tested for future operations.doi:href="http://dx.doi.org/10.2204/iodp.sd.10.01.2010" target="_blank">10.2204/iodp.sd.10.01.2010
机译:南海海槽低震带试验(NanTroSEIZE)是一项重大的钻探工程,旨在研究俯冲带板边界的断裂力学和地震行为。 Expedition 319是科学海洋钻探中的第一个立管钻探操作。操作包括在板块边界断层上方的前盆地的C0009站点上的立管钻探,在兆张断裂系统浅层部分上的C0010站点的无立管钻探-在板块边界地震中可能会滑动–以及在C0011站点(进入的洋板)进行322号远洋钻探的初始钻探。在C0009站点,测试了新方法,包括分析钻探泥屑和气体,以及就地测量应力,孔隙压力和压力。这些结果与较早的钻探相结合将提供(a)前盆地发育的历史(包括与兆张断裂系统和现代棱镜的发育相关的联系),(b)第一个原位板边界悬挂壁的水文测量,以及(c)跨前臂并随深度的原位应力测量(方向和大小)的积分。垂直地震剖面(VSP)实验对俯冲带深层结构提供了改善的约束。在站点C0010处,随钻测井表明沿走向距离短(<5 km)的断层带和悬壁特性发生了重大变化,表明了不同的埋藏和/或隆升历史。第一个钻孔天文台仪器安装在站点C0010处,以监测兆发断裂带内的压力和温度,并测试了部署更复杂的天文台仪器的方法,以供将来使用。 doi:href =“ http:// dx.doi.org/10.2204/iodp.sd.10.01.2010“ target =” _ blank“> 10.2204 / iodp.sd.10.01.2010

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