Plate Motion Statistics and Relation of Propagation and Overlap for the Juan de Fuca Ridge

胡安德富卡海岭的板块运动统计及其传播与重叠关系

• 批准号: 8811061
• 负责人: Douglas Wilson
• 金额: --
• 依托单位: University of California-Santa Barbara
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 1988
• 资助国家: 美国
• 起止时间: 1988-09-01 至 1990-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=8811061&HistoricalAwards=false
• 关键词: Plate; Motion; Statistics; Relation; Propagation

Lithospheric plates that compose the outer shell of the earth form by volcanic processes at mid-ocean ridges (spreading centers) where igneous material is added more or less symmetrically to each plate which borders on the mid-ocean ridge. This growth process is accompanied by relative motion between the two plates on either side of the ridge crest-motion that can be determined from a study of amgnetic anomalies observed at the sea surface over the mid-ocean ridge. Over a short period of geologic time ( few million years) this relative motion can be described in terms of rotation about a point (pole) that remains fixed to each plate. Over longer periods of time the motion is moe complicated and is accompanied by changes in the configuration of the mid-ocean spreading center, changes which are manifest as overlapping spreading centers and proagating rifts. %%% This project investigates the details of this process for the Juan de Fuca Ridge, a spreading center off the Washington- Oregon coast. Wilson plans to determine a revised rotation pole with confidence limits for motion of the Juan de Fuca plate with respect to the Pacific plate. In the process he will make computer modesl to demonstarate the development of overlapping spreading centers and propagating rifts. He will also attempt to determine over what interval the relative plate motion can be described in terms of a sample rotation.

构成地球外壳的岩石圈板块是在大洋中脊（扩张中心）的火山作用下形成的，在那里，火成岩物质或多或少对称地添加到与大洋中脊接壤的每个板块。这一增长过程伴随着脊顶两侧两个板块之间的相对运动，这种运动可以通过研究大洋中脊海面上观测到的地磁异常来确定。在很短的地质时期内（几百万年），这种相对运动可以用围绕一个点（极点）的旋转来描述，这个点仍然固定在每个板块上。在较长的时间内，这种运动MoE复杂，并伴随着大洋中部扩张中心形态的变化，这种变化表现为扩张中心的重叠和扩张裂谷的扩大。%本项目调查了胡安德富卡岭这一过程的细节，这是华盛顿-俄勒冈州海岸的一个扩散中心。威尔逊计划确定一个修正的旋转极，并对胡安·德富卡板块相对于太平洋板块的运动确定置信限。在这个过程中，他将制作计算机模型来演示重叠传播中心和传播裂缝的发展。他还将试图确定在什么样的时间间隔内，板块的相对运动可以用样本旋转来描述。