Geology and uranium deposits of the Laguna district, New Mexico

Moench, Robert H.; Schlee, John Stevens

doi:10.3133/pp519

Cited by 55 publications

(117 citation statements)

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“…The X -ray intensity was estimated after monochromatization by pyrolytic graphite. The observed d -values and intensities are listed in Table 2 together with those of goldmanite (Moench and Meyrowitz, 1964). The X -ray diffraction patterns can be well indexed as a cubic cell and they are in good agreement with those of goldmanite.…”

Section: X-ray Propertiessupporting

confidence: 56%

“…Novak and Gibbs (1971) proposed an existence limit for garnet based * Novak and Gibbs (1971). Moench and Meyrowitz (1964). Table 2.…”

Section: Discussionmentioning

confidence: 99%

“…On the other hand, Momoi (1964) found a substitution between Ca and Mn in V -dominant garnet from the Yamato mine, Kagoshima Prefecture, Japan. Its solid solution can be expressed by two end -members: Mn 3 V 2 Si 3 O 12 and Ca 3 V 2 Si 3 O 12 , which is called as goldmanite (Moench and Meyrowitz, 1964). However, Mn 3 V 2 Si 3 O 12 was still a hypothetical end -member, because Mn occupancy in the X site was less than 50% in this garnet.…”

Section: Introductionmentioning

confidence: 99%

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Momoiite, (Mn2+,Ca)3(V3+,Al)2Si3O12, a new manganese vanadium garnet from Japan

Tanaka

Endo

Minakawa

et al. 2010

Journal of Mineralogical and Petrological Sciences

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Momoiite, (Mn 2+ ,Ca) 3 (V 3+ ,Al) 2 Si 3 O 12 , an Mn 2+ -and V 3+ -rich analog of silicate garnet, was found in three localities: the Kurase (type locality), Hokkejino, and Fujii mines that are respectively located in Ehime, Kyoto, and Fukui Prefectures, Japan. Momoiite is greenish -yellow to emerald -green in color, and it occurs in the form of an aggregate having a size of up to 1 mm in a vein having a thickness of several millimeters with calcite and tephroite. Momoiite is optically isotropic, with n = 1.86(1). Its calculated density is 4.01 g/cm

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Section: X-ray Propertiessupporting

confidence: 56%

“…Novak and Gibbs (1971) proposed an existence limit for garnet based * Novak and Gibbs (1971). Moench and Meyrowitz (1964). Table 2.…”

Section: Discussionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

See 1 more Smart Citation

Momoiite, (Mn2+,Ca)3(V3+,Al)2Si3O12, a new manganese vanadium garnet from Japan

Tanaka

Endo

Minakawa

et al. 2010

Journal of Mineralogical and Petrological Sciences

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show abstract

“…The introduced reductant can be either a water that carries residues from decaying plant (humic) material, such as occurs in the Ienticular deposits near Grants, New Mexico (Adler, 1974;Granger, 1968;Moench and Schlee, 1967), or an inorganic material, such as H2S, which is introduced through fault zones and is derived from other organic material or volcanic sources, such as occurs in the coastal uranium ore deposits in Texas.…”

Section: Uranium Ore Deposits Typically Form When Massive Amounts Of mentioning

confidence: 99%

Consideration of nuclear criticality when disposing of transuranic waste at the Waste Isolation Pilot Plant

Rechard¹,

Sanchez²,

Stockman³

et al. 2000

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“…They also noted (1957, p. 48) that in some areas the Cow Springs was equivalent to the Zuni Sandstone of Button (1885). Moench and Schlee (1967) made minor revisions to Jurassic nomenclature in the Laguna-Mesita area based on extensive mapping, and their report included a thorough discussion of the Bluff Sandstone of that area. The Bluff Sandstone was considered by Moench and Schlee (1967, p. 15) to be equivalent to the brown-buff and white sandstone members of the Morrison Formation of Kelley and Wood (1946) and Silver (1948).…”

Section: Previous Studiesmentioning

confidence: 99%