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Results of the Arctic Mid-Ocean Ridge Expedition (AMORE 2001) - Seafloor Spreading at the Top of the World

机译:北极中洋岭探险的结果(amORE 2001) - 海底传播在世界之巅

摘要

The Arctic Mid-Ocean Ridge Expedition (AMORE 2001) returned in early October 2001 after an incredibly sucessful ten-week study of the Gakkel Ridge and its surrounding basins in the high Arctic. AMORE 2001 was an international effort involving two icebreakers: PFS Polarstern, from the Alfred Wegener Institute in Bremerhaven, Germany and the new U.S. icebreaker, USCGC Healy. It was Healy's maiden scientific voyage, and she proved to be an excellent icebraker and scientific platform. This historic and highly sucessful expedition far exceeded anyone's expectations and went well beyond the goals set forth by InterRidge (Vol. 10 (1), 2001) in charting and sampling the Gakkel Ridge. Some of the highlights of the expedition are:1. Basalts and peridotites were recovered from over 200 sites within and near the axis of Gakkel Ridge, about three times as many sites as were planned. 2. Hydrothermal plumes were discovered and sampled along this ultraslow spreading ridge. 3. A high-resolution, well-navigated map of the ridge was unexpectedly produced using two hull-mounted multibeam sonar systems, which worked far better in the ice than anticipated. 4. Sucessful seismic measurements showed that crustal thickness varies strongly along the axis of Gakkel Ridge, most likely according to distinct volcanic centers. 5. The crustal thickness in the Nansen Basin does not follow theoretical models, which predict thin crust at slow spreading rates. The crust thickens towards the Gakkel Ridge.
机译:在对北极高海拔地区的Gakkel脊及其周围盆地进行了为期十周的成功研究之后,北极中海脊远征队(AMORE 2001)在2001年10月初返回。 2001年AMORE是一项国际努力,涉及两个破冰船:来自德国不来梅哈芬的阿尔弗雷德·韦格纳研究所的PFS Polarstern和新的美国破冰船USCGC Healy。这是希利的处女航,她被证明是一个极好的冰上手和科学平台。这项历史悠久且非常成功的考察活动远远超出了任何人的期望,并且远远超出了InterRidge(第10卷,第1期,2001年)在绘制和采样Gakkel岭时设定的目标。这次探险的一些亮点是:1。玄武岩和橄榄岩从Gakkel Ridge轴内及其附近的200多个地点中回收,约为计划地点的三倍。 2.在该超慢扩散脊上发现了热液羽流并对其进行了采样。 3.使用两个安装在船体上的多波束声纳系统意外地绘制了一个高分辨率,导航良好的山脊图,该系统在冰中的工作远比预期的要好。 4.足够的地震测量结果表明,地壳厚度沿Gakkel山脊的轴线变化很大,很可能是根据不同的火山中心。 5.南森盆地的地壳厚度未遵循理论模型,该模型预测了地壳缓慢扩散的速度。地壳向Gakkel山脊增厚。

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