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Haiti-Drill: an amphibious drilling project workshop

机译:海地演习:两栖钻探项目研讨会

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摘要

The Haiti region – bounded by two strike-slip faults expressed both onshore and offshore – offers a unique opportunity for an amphibious drilling project. The east–west (EW)-striking, left lateral strike-slip Oriente–Septentrional fault zone and Enriquillo–Plantain Garden fault zone bounding Haiti have similar slip rates and also define the northern and southern boundaries of the Gonave Microplate. However, it remains unclear how these fault systems terminate at the eastern boundary of that microplate. From a plate tectonic perspective, the Enriquillo–Plantain Garden fault zone can be expected to act as an inactive fracture zone bounding the Cayman spreading system, but, surprisingly, this fault has been quite active during the last 500?years. Overall, little is understood in terms of past and present seismic and tsunami hazards along the Oriente–Septentrional fault zone and Enriquillo–Plantain Garden fault zone, their relative ages, maturity, lithology, and evolution – not even the origin of fluids escaping through the crust is known. Given these unknowns, the Haiti-Drill workshop was held in May 2019 to further develop an amphibious drilling project in the Haiti region on the basis of preproposals submitted in 2015 and their reviews. The workshop aimed to complete the following four tasks: (1)?identify significant research questions; (2)?discuss potential drilling scenarios and sites; (3)?identify data, analyses, additional experts, and surveys needed; and (4)?produce timelines for developing a full proposal. Two key scientific goals have been set, namely to understand the nature of young fault zones and the evolution of transpressional boundaries. Given these goals, drilling targets were then rationalized, creating a focus point for research and/or survey needs prior to drilling. Our most recent efforts are to find collaborators, analyze existing data, and to obtain sources of funding for the survey work that is needed.
机译:海地地区 - 两次防滑断层的界限在陆上和海上表示 - 为两栖钻井项目提供独特的机会。东方(EW)-Striking,左侧滑动Origee-Septentional断层区和Reasizlo-Plantain Garden Fault区界定海地具有类似的滑移率,并且还定义了瓦瓦夫·微孔板的北部和南部边界。然而,它仍然尚不清楚这些故障系统如何在该微孔板的东部边界处终止。从板块构造的角度来看,可以预期烤箱 - 植物花园断裂带作为横向的无活性骨折区,令人惊讶的是,这个故障在过去的500岁时是非常活跃的。总体而言,在过去和沿着东方 - 梧桐断层区和富喹 - 班园园故障区,他们的相对年龄,成熟,岩性和进化方面,甚至甚至逃离的原因地壳是已知的。鉴于这些未知数未知数,海地钻机研讨会于2019年5月举行,在2015年提交的预批准和审查的基础上进一步开发海地地区的两栖钻探项目。研讨会旨在完成以下四个任务:(1)?确定重要的研究问题; (2)?讨论潜在的钻井场景; (3)?识别数据,分析,其他专家和所需的调查; (4)?制定全面提案的时间表。已经设定了两个关键的科学目标,即了解年轻断层区的性质和跨压边界的演变。鉴于这些目标,然后在钻井前创建钻井目标,创造了研究和/或调查需求的焦点点。我们最近的努力是找到合作者,分析现有数据,并获得所需的调查工作的资金来源。

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