Arid
DOI10.2172/245579
报告编号DOE/NV/10461--T74-Vol.1
来源IDOSTI_ID: 245579
The origin and history of alteration and carbonatization of the Yucca Mountain ignimbrites. Volume I
Szymanski, J.S.
英文摘要This document contains Volume I of the report entitled The Origin and History of Alteration and Carbonatization of the Yucca Mountain Ignimbrites by Jerry S. Szymanski and a related correspondence with comments by Donald E. Livingston. In the Great Basin, the flow of terrestrial heat through the crust is affected in part by the flow of fluids. At Yucca Mountain, the role of fluids in crustal heat transport is manifested at the surface by youthful calcretes, sinters, bedrock veins, hydrothermal eruption breccias and hydrothermal alteration. This report discusses evidence for recent metasomatism high in the stratigraphic section at Yucca Mountain. Over the last several hundred years, episodes of calcite emplacement contemporaneous with local mafic volcanism have occurred at intervals that are not long in comparison with the isolation time required for a High-Level Radioactive Waste repository.
出版年1992
报告类型Technical Report
语种英语
国家美国
来源学科分类05 NUCLEAR FUELS ; YUCCA MOUNTAIN ; UNDERGROUND FACILITIES ; SITE CHARACTERIZATION ; GEOLOGY ; HIGH-LEVEL RADIOACTIVE WASTES ; UNDERGROUND STORAGE ; SPENT FUELS ; TUFF ; HYDROTHERMAL ALTERATION
URLhttp://www.osti.gov/scitech/servlets/purl/245579
资源类型科技报告
条目标识符http://119.78.100.177/qdio/handle/2XILL650/264729
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Szymanski, J.S.. The origin and history of alteration and carbonatization of the Yucca Mountain ignimbrites. Volume I,1992.
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