This report is a compilation of papers and a letter providing technical information on the origin and geochemistry of calcite veins and calcretes in the vicinity of the Yucca Mountain repository. The information is presented to demonstrate that these deposits may be ``thermogenic`` in origin with some alteration by pedogenic processes. The papers present isotope ratios of uranium, strontium, and carbon to support the claims for a hydrothermal source. The letter provides a critical review of a previous paper presented at the 64th Advisory Committee on Nuclear Waste. The report makes an attempt to emphasize the need to review this possible origin because it has dramatic implications on the geologic history, paleo-ground water levels, and inte...
Meteoric water percolating through 500 to 700 m of hydrologically unsaturated felsic tuffs provides ...
At Yucca Mountain, currently under consideration as a potential permanent underground repository for...
The unsaturated zone (UZ) in Miocene-age welded tuffs at Yucca Mountain, Nevada, is under considerat...
This report is a critical review of a US Geological Survey (USGS) paper regarding the origin of the ...
This document includes several reports describing scientific studies of the origin of near surface c...
This document contains Volume I of the report entitled The Origin and History of Alteration and Carb...
This document is an annual report describing investigations of natural groundwater hazards at the pr...
Yucca Mountain, Nevada, is under consideration as a potential high-level radioactive waste repositor...
In the near future a decision will be made as to whether or not Yucca Mountain, 90 miles northwest o...
Large vein-like deposits of calcite and opaline silica that infill the Bow Ridge fault are exposed b...
Chemical, mineralogic, and petrographic analyses of siliceous calcretes from Exile Hill east of Yucc...
This study is part of the research program of the Yucca Mountain Project intended to provide the Sta...
Several faults near Yucca Mountain, Nevada, contain abundant calcite and opal-CT, with lesser amount...
Calcite and opal coatings found on fracture footwalls and lithophysal cavity bottoms in the volcanic...
The origin of secondary calcite-silica minerals in primary and secondary porosity of the host Miocen...
Meteoric water percolating through 500 to 700 m of hydrologically unsaturated felsic tuffs provides ...
At Yucca Mountain, currently under consideration as a potential permanent underground repository for...
The unsaturated zone (UZ) in Miocene-age welded tuffs at Yucca Mountain, Nevada, is under considerat...
This report is a critical review of a US Geological Survey (USGS) paper regarding the origin of the ...
This document includes several reports describing scientific studies of the origin of near surface c...
This document contains Volume I of the report entitled The Origin and History of Alteration and Carb...
This document is an annual report describing investigations of natural groundwater hazards at the pr...
Yucca Mountain, Nevada, is under consideration as a potential high-level radioactive waste repositor...
In the near future a decision will be made as to whether or not Yucca Mountain, 90 miles northwest o...
Large vein-like deposits of calcite and opaline silica that infill the Bow Ridge fault are exposed b...
Chemical, mineralogic, and petrographic analyses of siliceous calcretes from Exile Hill east of Yucc...
This study is part of the research program of the Yucca Mountain Project intended to provide the Sta...
Several faults near Yucca Mountain, Nevada, contain abundant calcite and opal-CT, with lesser amount...
Calcite and opal coatings found on fracture footwalls and lithophysal cavity bottoms in the volcanic...
The origin of secondary calcite-silica minerals in primary and secondary porosity of the host Miocen...
Meteoric water percolating through 500 to 700 m of hydrologically unsaturated felsic tuffs provides ...
At Yucca Mountain, currently under consideration as a potential permanent underground repository for...
The unsaturated zone (UZ) in Miocene-age welded tuffs at Yucca Mountain, Nevada, is under considerat...