1986
DOI: 10.2172/59981
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Chemistry of diagenetically altered tuffs at a potential nuclear waste repository, Yucca Mountain, Nye County, Nevada

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Cited by 28 publications
(44 citation statements)
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“…Other boreholes, where data is sufficient, show that CaO generally decreases with increasing depth. This relation has been noted by Broxton, et al (1986) and Szymanski (1 992 Calcic rich clinoptilolites occur at depth in boreholes USW G-4, UE-25 a&b#l , UE-25 p#l and J-13 in the southeastern portions of Yucca Mountain..…”
Section: Deep Calcium Rich Clinopfiloljfesupporting
confidence: 63%
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“…Other boreholes, where data is sufficient, show that CaO generally decreases with increasing depth. This relation has been noted by Broxton, et al (1986) and Szymanski (1 992 Calcic rich clinoptilolites occur at depth in boreholes USW G-4, UE-25 a&b#l , UE-25 p#l and J-13 in the southeastern portions of Yucca Mountain..…”
Section: Deep Calcium Rich Clinopfiloljfesupporting
confidence: 63%
“…In this report we examine the spatial distribution of the various types of chemical alteration indicated by the data reported in Broxton, et al (1986) in order to evaluate the location, spatial character and extent of the alteration with the hope of shedding light on the origin of the altering fluids and to test the hypogene hypothesis of Szymanski (1992). In this regard, it is of prime importance is to evaluate whether the metasomatic alteration reflects supergene or, conversely, hypogene processes.…”
Section: Purposementioning
confidence: 99%
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“…The phosphate in the rocks is apparently redistributed locally by groundwater, resulting in the precipitation of uranyl phosphate minerals within the zone of weathering (Snelling 1980). This retardation mechanism is not expected to be important at Yucca Mountain, given the low phosphate concentrations found in Yucca Mountain rock units (Broxton et al 1986). …”
Section: Uraniummentioning
confidence: 98%
“…Groundmass texture (crystals <4 mm) comprises the bulk of the formation and has a composition that includes a range of 76 to 78 wt% Si02 with A1203 next in abundance at just under 12 to 13 wt% and other minerals as shown in Table 4-6. The values in Table 4-6 are from an analysis of samples from USW G-4 (Broxton et al, 1986) from a vitric unit with a composition that was representative of the majority of units in the well. The values in Table 4-6 are similar to those shown in the SCP (DOE, 1988b, Table 1-5, p. 1-69), which gives a breakdown of composition by subunits (lower nonlithophysal, etc.).…”
Section: Geochemistrymentioning
confidence: 99%