Socorro Region 1963
DOI: 10.56577/ffc-14.220
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K-Ar ages of Tertiary volcanic and intrusive rocks in Socorro, Catron, and Grant Counties, New Mexico

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Cited by 13 publications
(19 citation statements)
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“…Similarities in physical character and mode of origin with the No Agua and Grants pumiceous perlites are noteworthy. Potassium-argon age determinations were inconsistent at 23.7 and 33.2 million years (Weber and Bassett, 1963).…”
Section: Perlitementioning
confidence: 97%
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“…Similarities in physical character and mode of origin with the No Agua and Grants pumiceous perlites are noteworthy. Potassium-argon age determinations were inconsistent at 23.7 and 33.2 million years (Weber and Bassett, 1963).…”
Section: Perlitementioning
confidence: 97%
“…Zones of abundant spherulites and of montmorillonitic and zeolitic alteration impair the commercial possibilities of the deposit. Potassium-argon age determinations averaging about 14.3 million years (late Miocene) have been obtained from this perlite (Weber and Bassett, 1963).…”
Section: Perlitementioning
confidence: 99%
“…Two small outcrops of Pennsylvanian rocks were mapped recently by Robert H. Weber (Weber and Willard, 1959a) northwest of Luna. The larger of these occurs in secs.…”
Section: Pennsylvanian Systemmentioning
confidence: 99%
“…Most of Catron County is underlain by a complex sequence of extrusive volcanic rocks and associated sediments of Tertiary and Quaternary age. Reconnaissance mapping of most of Catron County by Willard (1957aWillard ( , 1957b, Willard and Givens (1958), Willard and Weber (1958), Weber and Willard (1959a, 1959b), and Willard, Weber, and Kuellmer (1961 has been published by the New Mexico Bureau of Mines and Mineral Resources. In addition, a detailed study by Stearns of a part of the north side of the San Agustin Plains is now available.…”
Section: Tertiary and Quaternary Systemsmentioning
confidence: 99%
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