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Quantitative Relations between Submarine Volcanic Eruption Rates and Lava Flow Morphologies at Mid-Ocean Ridges: Analysis of Field Data and Laboratory Simulations

Quantitative Relations between Submarine Volcanic Eruption Rates and Lava Flow Morphologies at Mid-Ocean Ridges: Analysis of Field Data and Laboratory Simulations
海底火山喷发率与大洋中脊熔岩流形态之间的定量关系：现场数据分析和实验室模拟
批准号：
9505384
负责人：
Daniel Fornari
金额：
$8.72万
依托单位：
Woods Hole Oceanographic Institution
依托单位国家：
美国
项目类别：
Continuing Grant
财政年份：
1995
资助国家：
美国
项目状态：
已结题
起止时间：
1995-10-01 至 1998-03-31
来源：
https://www.nsf.gov/awardsearch/showAward?AWD_ID=9505384&HistoricalAwards=false
关键词：
QuantitativeRelationsbetweenSubmarineVolcanic

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中文摘要
翻译
小行星9505384 这项工作的目的是开发一个定量模型的基础上流动形态的海底熔岩流侵位的方法开发的研究外星熔岩流。 该模型将包括下伏坡度、微地形和可变渗出率的影响。 它将把从目前的数据收集技术中获得的海底熔岩流的通常空间有限的视图放在整个流动的广泛背景下，允许从这些狭窄的视图中推断出整个流动的渗出率。 ***
英文摘要
9505384 Fornari The objective of this work is to develop a quantitative model of submarine lave flow emplacement based on flow morphology using methods developed for the study of extraterrestrial lava flows. The model will include the effect of underlying slope, microtopography and variable effusion rate. It will place the often spatially limited views of submarine lava flows available from current data-collection techniques in the broad context of an entire flow, allowing effusion rates for a whole flow to be extrapolated from these narrow views. ***
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