Relationship Between Mid-Ocean Ridge Topography and Gravity,Spreading Rate, and Plate Boundary Geometry
Relationship Between Mid-Ocean Ridge Topography and Gravity,Spreading Rate, and Plate Boundary Geometry
批准号:
9012235
负责人:
Alberto Malinverno
金额:
$5.01万
依托单位:
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
1991
资助国家:
美国
项目状态:
已结题
起止时间:
1991-02-15 至 1993-01-31
中文摘要
本文还讨论了中、高密度聚乙烯轴向形态变化的原因。 对洋脊的了解很少, 许多因素,如传播速度和距离, 脊变换交点。从2004年至2005年的 在北大西洋,首席研究员提取了 以下参数:纬度,扩展率,距离 脊转换交点,零年龄深度,裂谷-谷 地形、裂谷宽度以及后者的平滑变化 三个变量他做过线性相关和多重相关 这些数据的回归分析,并达到了几个 根据参数之间的相关性得出结论。这 项目将扩展这项工作,以类似的方式分析 全球测深和重力数据集,目标是 确定哪些是最重要的控制因素, 大洋中脊的总体形态。
英文摘要
The causes of variations in the axial morphology of mid- ocean ridges is poorly understood and has been related to a number of factors such as spreading rate and distance from ridge-transform intersections. From bathymetric profiles from the North Atlantic, the Principal Investigator has extracted the following parameters: latitude, spreading rate, distance from ridge-transform intersection, zero-age depth, rift-valley relief, rift-valley width, and smoothed variations of the latter three variables. He has done linear correlation and multiple regression analyses of these data and reached several conclusions based on the correlations among parameters. This project will extend this work to analyze in a similar manner a world-wide bathymetric and gravity data set with the goal of determining which are the most important factors controlling the overall morphology of mid-ocean ridges.
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依托单位:
海外基金