首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >The Terceira Rift as hyper-slow, hotspot-dominated oblique spreading axis: A comparison with other slow-spreading plate boundaries
【24h】

The Terceira Rift as hyper-slow, hotspot-dominated oblique spreading axis: A comparison with other slow-spreading plate boundaries

机译:Terceira裂谷为超慢,热点占主导的倾斜扩展轴:与其他慢速扩展板块边界的比较

获取原文
获取原文并翻译 | 示例
       

摘要

We suggest the 550 km long Terceira Rift (TR, Azores Plateau) is the world's slowest-spreading (hyper-slow, 4 mm/a plate separation; 2.3-3.8 mm/a perpendicular to oblique axial segments) organized accreting plate boundary. In its slightly sinuous (ca. 300 km radius of curvature) axial trace, its oblique spreading angles (ca. 40°-65°), and in frequency and first motions of earthquakes, the TR resembles better-known 'ultra-' or 'super-' slow spreading ridges (e.g. Gakkel and Southwest Indian ridges). Interpreted simply as volcanically 'unfilled' rift valley segments, the inter-island basins (e.g. the 3200 m deep Hirondelle Basin) are slightly wider (30–60 km), but not significantly deeper (1000-2200 m) than the Mid-Atlantic Ridge (MAR) median valley (20-28 mm/a; 10°N-53°N). However, along-axis segmentation wavelengths (ca. 100 km) are double those along the central MAR, but make TR comparable to the 'ultra-slow' (15-16 mm/a) Southwest Indian and Gakkel (7-13 mm/a) ridges. If this segmentation wavelength reflects Rayleigh-Taylor instabilities, the viscosity contrast between the overlying axial lithosphere and the partial melt zones is about an order of magnitude greater at ca. 4-16 mm/a than at 20-30 mm/a. The TR differs dramatically from ultra-slow ridges only in the large amplitude of along-strike topography (2000-4000 m; 4200 m total variation) owing perhaps to a copious melt flux from the Azores 'hotspot', combined with a spreading-rate-determined greater axial flexural strength and plate thickness, and slower export of volcanics from the rift axis. The probable TR youth (ca. 1 Ma?, requiring less than 4 km new oceanic crust) suggests lack of steady-state spreading conditions, which may explain the published gravity evidence against TR spreading. Absolute plate motions support the creation of the Azores Plateau by successive NE jumps of the rift axis to maintain its position over a fixed 'hotspot'.
机译:我们建议,长550公里的Terceira Rift(亚速尔群岛高原TR)是世界上铺展最缓慢的区域(超慢,板块间距为4 mm / a;垂直于斜轴段的间距为2.3-3.8 mm / a),是有组织的板块边界。在其曲折的(大约300 km曲率半径)轴向轨迹,倾斜的扩展角(大约40°-65°)以及地震的频率和初次运动中,TR类似于众所周知的“超”或“超”。 “超级”缓慢扩散的山脊(例如Gakkel和西南印度山脊)。岛间盆地(如深3200 m的Hirondelle盆地)被解释为火山“未填充”的裂谷谷段,比大西洋中部稍宽(30–60 km),但深度不深(1000-2200 m)脊(MAR)中值谷(20-28 mm / a; 10°N-53°N)。但是,沿轴的分割波长(约100 km)是中央MAR的两倍,但使TR可以与“超慢”(15-16 mm / a)的西南印度和Gakkel(7-13 mm / a)山脊。如果该分段波长反映了瑞利-泰勒不稳定性,则重叠的轴向岩石圈与部分熔体区之间的粘度差在大约50℃时会大一个数量级。 4-16 mm / a,而不是20-30 mm / a。 TR与超慢山脊的区别仅在于大幅度的沿走向地形(2000-4000 m;总变化为4200 m),这可能是由于亚速尔群岛“热点”的大量熔体通量以及扩展速率所致。 -确定更大的轴向抗弯强度和板厚,以及从裂谷轴缓慢导出火山。可能的TR青年(大约1 Ma ?,需要不到4 km的新大洋壳)表明缺乏稳定的扩展条件,这可能解释了已发表的反对TR扩展的重力证据。绝对的板块运动通过裂谷轴的连续NE跳跃来支持亚速尔高原的建立,以保持其在固定“热点”上的位置。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号