Sulfuric acid speleogenesis of Carlsbad Cavern and its relationship to hydrocarbons, Delaware basin, New Mexico and Texas
Journal Article
·
· AAPG Bulletin (American Association of Petroleum Geologists); (USA)
OSTI ID:5690298
- Cave Research Foundation, Albuquerque, NM (USA)
Sulfur-isotope data and pH-dependence of the mineral endellite support the hypothesis that Carlsbad Cavern and other caves in the Guadalupe Mountains were dissolved primarily by sulfuric acid rather than by carbonic acid. Floor gypsum deposits up to 10 m thick and native sulfur in the caves are significantly enriched in {sup 32}S; {delta}{sup 34}S values as low as {minus}25.8 {per thousand} (CDT) indicate that the cave sulfur and gypsum are the end products of microbial reactions associated with hydrocarbons. A model for a genetic connection between hydrocarbons in the basin and caves in the Guadalupe Mountains is proposed. As the Guadalupe Mountains were uplifted during the late Pliocene-Pleistocene, oil and gas moved updip in the basin. The gas reacted with sulfate anions derived from dissolution of the Castile anhydrite to form H{sub 2}S, CO{sub 2}, and castile limestone. The hydrogen sulfide rose into the Capitan reef along joints, forereef carbonate beds, or Bell Canyon siliciclastic beds and there reacted with oxygenated groundwater to form sulfuric acid and Carlsbad Cavern. A sulfuric-acid mode of dissolution may be responsible for large-scale porosity of some Delaware basin reservoirs and for oil-field karst reservoirs in other petroleum basins of the world. 8 figs.
- OSTI ID:
- 5690298
- Journal Information:
- AAPG Bulletin (American Association of Petroleum Geologists); (USA), Journal Name: AAPG Bulletin (American Association of Petroleum Geologists); (USA) Vol. 74:11; ISSN AABUD; ISSN 0149-1423
- Country of Publication:
- United States
- Language:
- English
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OSTI ID:61805
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Related Subjects
02 PETROLEUM
020200* -- Petroleum-- Reserves
Geology
& Exploration
03 NATURAL GAS
030200 -- Natural Gas-- Reserves
Geology
& Exploration
58 GEOSCIENCES
580000 -- Geosciences
ALKALINE EARTH METAL COMPOUNDS
ALLUVIAL DEPOSITS
ANHYDRITE
CALCIUM COMPOUNDS
CALCIUM SULFATES
CARBON
CARBON COMPOUNDS
CARBONATE ROCKS
CARBONIC ACID
CAVES
CAVITIES
CENOZOIC ERA
CHALCOGENIDES
COBALT
DEPOSITION
DISSOLUTION
ELEMENTS
EVEN-EVEN NUCLEI
FEDERAL REGION VI
GEOLOGIC AGES
GEOLOGIC DEPOSITS
GEOLOGIC STRUCTURES
GROUND WATER
GYPSUM
HYDROGEN COMPOUNDS
HYDROGEN SULFIDES
INORGANIC ACIDS
ISOTOPE RATIO
ISOTOPES
LIGHT NUCLEI
LIMESTONE
METALS
MINERAL RESOURCES
MINERALS
NATURAL GAS DEPOSITS
NEW MEXICO
NONMETALS
NORTH AMERICA
NUCLEI
ORIGIN
OXYGEN COMPOUNDS
PETROLEUM DEPOSITS
PH VALUE
PLEISTOCENE EPOCH
POROSITY
QUATERNARY PERIOD
REEFS
RESERVOIR ROCK
RESOURCES
ROCKS
SAND
SEDIMENTARY BASINS
SEDIMENTARY ROCKS
STABLE ISOTOPES
SULFATE MINERALS
SULFATES
SULFIDES
SULFUR 32
SULFUR 34
SULFUR COMPOUNDS
SULFUR ISOTOPES
SULFURIC ACID
TERTIARY PERIOD
TEXAS
TRANSITION ELEMENTS
USA
WATER
020200* -- Petroleum-- Reserves
Geology
& Exploration
03 NATURAL GAS
030200 -- Natural Gas-- Reserves
Geology
& Exploration
58 GEOSCIENCES
580000 -- Geosciences
ALKALINE EARTH METAL COMPOUNDS
ALLUVIAL DEPOSITS
ANHYDRITE
CALCIUM COMPOUNDS
CALCIUM SULFATES
CARBON
CARBON COMPOUNDS
CARBONATE ROCKS
CARBONIC ACID
CAVES
CAVITIES
CENOZOIC ERA
CHALCOGENIDES
COBALT
DEPOSITION
DISSOLUTION
ELEMENTS
EVEN-EVEN NUCLEI
FEDERAL REGION VI
GEOLOGIC AGES
GEOLOGIC DEPOSITS
GEOLOGIC STRUCTURES
GROUND WATER
GYPSUM
HYDROGEN COMPOUNDS
HYDROGEN SULFIDES
INORGANIC ACIDS
ISOTOPE RATIO
ISOTOPES
LIGHT NUCLEI
LIMESTONE
METALS
MINERAL RESOURCES
MINERALS
NATURAL GAS DEPOSITS
NEW MEXICO
NONMETALS
NORTH AMERICA
NUCLEI
ORIGIN
OXYGEN COMPOUNDS
PETROLEUM DEPOSITS
PH VALUE
PLEISTOCENE EPOCH
POROSITY
QUATERNARY PERIOD
REEFS
RESERVOIR ROCK
RESOURCES
ROCKS
SAND
SEDIMENTARY BASINS
SEDIMENTARY ROCKS
STABLE ISOTOPES
SULFATE MINERALS
SULFATES
SULFIDES
SULFUR 32
SULFUR 34
SULFUR COMPOUNDS
SULFUR ISOTOPES
SULFURIC ACID
TERTIARY PERIOD
TEXAS
TRANSITION ELEMENTS
USA
WATER