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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Quantitative textural analysis of ilmenite in Apollo 17 high-titanium mare basalts
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Quantitative textural analysis of ilmenite in Apollo 17 high-titanium mare basalts

机译:阿波罗17号高钛母马玄武岩中钛铁矿的定量组织分析

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摘要

Quantitative textural analysis is a powerful tool in the investigation of basalt crystallization. We present the first comprehensive crystal size distribution analysis of Apollo 17 high-titanium lunar basalts, with a focus on ilmenite. Crystal size distributions of ilmenite, pyroxene, plagioclase, olivine and armalcolite were determined for 18 high-Ti mare basalt samples from the Apollo 17 mission. A subset of the ilmenite size distribution (size bins of <0.6 mm in length) reflects growth at post-eruption or post-emplacement cooling rates. Growth of these small ilmenite crystals is controlled by cooling rate and not bulk composition or ilmenite abundance. CSD characteristics tied to cooling rate determined by experiments yield estimates of cooling rate in natural samples. Matrix ilmenite grew at rates up to 250 degrees C/h, while most samples contained phenocrysts that originated in environments cooling at <3 degrees C/h. Textural characteristics of ilmenite phenocrysts are used to develop a relative stratigraphy for the samples within a lava flow based upon comparisons with terrestrial analogues. (C) 2014 Elsevier Ltd. All rights reserved.
机译:定量纹理分析是研究玄武岩结晶的有力工具。我们介绍了阿波罗17号高钛月球玄武岩的首次综合晶体尺寸分布分析,重点是钛铁矿。确定了来自Apollo 17任务的18个高钛母马玄武岩样品的钛铁矿,辉石,斜长石,橄榄石和白云母的晶体尺寸分布。钛铁矿尺寸分布的一个子集(长度小于0.6毫米的尺寸仓)反映了喷发后或放置后冷却速率的增长。这些小的钛铁矿晶体的生长是由冷却速率控制的,而不是由整体组成或钛铁矿丰度控制的。通过实验确定的与冷却速率相关的CSD特性可得出自然样品中冷却速率的估计值。基质钛铁矿以高达250摄氏度/小时的速度生长,而大多数样品中含有的隐晶石起源于冷却速度低于3摄氏度/小时的环境。基于与地面类似物的比较,钛铁矿的结晶特征被用于发展熔岩流内样品的相对地层。 (C)2014 Elsevier Ltd.保留所有权利。

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