Silica Replacement in the Southern White Pine Range, East Central Nevada| A Stable Isotope Study
<p> In the southern White Pine Range (SWPR) silica is found to have been deposited from hydrothermal solution within the Currant Gap Detachment fault (CGD). Silica has been observed to occur in three modes of deposition: (1) narrow veins within the lower plate Pole Canyon limestone, (2) bulk s...
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| Language: | EN |
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California State University, Long Beach
2018
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| Online Access: | http://pqdtopen.proquest.com/#viewpdf?dispub=10841608 |