1966
DOI: 10.1306/74d7146f-2b21-11d7-8648000102c1865d
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Opal, zeolites, and clays in an Eocene neritic bar sand

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Cited by 8 publications
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“…Reynolds ( 1966) reports considerable a-cristobalite, clinoptilolite, heulandite, and mont-Inorillonite, which, he concludes, formed by the alteration of volcanic material in the Paleocene and lower Eocene of Alaba1na. Similar minerals were found by Wermund and Moiola (1966) in the Meridian Sand Member of the Tallahatta Formation of Eocene age in l\1ississippi and Alabama. Eargle (1968) reported that indurated tuff or altered volcanic ash containing as n1uch as 50 percent clinoptilolite and lesser amounts of opal and montmorillonite occur in the base of the Jackson Group sediments of Texas.…”
Section: Volcanic Materialssupporting
confidence: 78%
“…Reynolds ( 1966) reports considerable a-cristobalite, clinoptilolite, heulandite, and mont-Inorillonite, which, he concludes, formed by the alteration of volcanic material in the Paleocene and lower Eocene of Alaba1na. Similar minerals were found by Wermund and Moiola (1966) in the Meridian Sand Member of the Tallahatta Formation of Eocene age in l\1ississippi and Alabama. Eargle (1968) reported that indurated tuff or altered volcanic ash containing as n1uch as 50 percent clinoptilolite and lesser amounts of opal and montmorillonite occur in the base of the Jackson Group sediments of Texas.…”
Section: Volcanic Materialssupporting
confidence: 78%