首页> 美国政府科技报告 >Nature and Origin of Mineral Coatings on Volcanic Rocks of the Black Mountain, Stonewall Mountain and Kane Springs Wash Volcanic Centers,Southern Nevada. Semiannual Report,Period January-July 1987.
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Nature and Origin of Mineral Coatings on Volcanic Rocks of the Black Mountain, Stonewall Mountain and Kane Springs Wash Volcanic Centers,Southern Nevada. Semiannual Report,Period January-July 1987.

机译:内华达南部黑山,石墙山和凯恩斯普林斯火山中心火山岩矿物涂层的性质和成因。半年度报告,1987年1月至7月。

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Mineral coatings, including desert varnish on volcanic rocks of the semi-arid Basin and Range province are composted of amorphous, translucent films of Fe, Mn, Si, and Al rich compounds. Coatings are chiefly thin films that impregnate intergranularly to depths of about 0.1 to 0.3 mm, rarely deeper. Sixteen coating sections and subsurface interiors were probed by SEM; 20 samples were scanned by infrated spectrometry; 10 samples were scanned for visible-near IR spectra; inductin coupling plasma analyses were collected on 34 samples; 2 desert varnish surgaces were investigated by optical density slice imagery; a few XRD analyses were conducted in addition to the 50 reported in the last period; thin section observation continued; and imagery processing focused on classification techniques. In late May, approximately 10 field days were spent at the Stonewall and Black Mountain study sited conducting more detailed mapping and observation base on imagery results and collecting spectra with the Collins Field Spectrometer. Approximately 100 spectral analyses were collected and are currently being processed.

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