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Volumn 279, Issue 5358, 1998, Pages 1919-1922

Age and origin of Carlsbad Cavern and related caves from 40Ar/39Ar of alunite

Author keywords

[No Author keywords available]

Indexed keywords

MINERAL;

EID: 0032549779     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.279.5358.1919     Document Type: Article
Times cited : (130)

References (46)
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    • 34S = -30 to 0 per mil relative to troilite in the meteorite Canyon Diablo) indicate that the sulfuric acid responsible for cave genesis was derived from biogenic hydrogen sulfide (4, 9, 10) most likely produced at the base of the Castile Formation in the Delaware Basin immediately south of the Guadalupe Mountains (9). the caves were formed when the hydrogen sulfide was oxidized to sulfuric acid as it migrated upward and approached the water table in the Capitan reef and forereef facies (Capitan Limestone) (9); massive amounts of limestone and dolostone were subsequently dissolved or replaced by gypsum.
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    • note
    • 39Ar geochronology work was provided by the New Mexico Bureau of Mines and Mineral Resources.


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