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October 01, 1997
Frio shale mineralogy and the stoichiometry of the smectite-to-illite reaction; the most important reaction in clastic sedimentary diagenesis
F. Leo Lynch
F. Leo Lynch
University of Texas at Austin, Department of Geological Sciences, Austin, TX, United States
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F. Leo Lynch
University of Texas at Austin, Department of Geological Sciences, Austin, TX, United States
Publisher: Clay Mineral Society
First Online:
02 Mar 2017
Online ISSN: 1552-8367
Print ISSN: 0009-8604
GeoRef, Copyright 2004, American Geological Institute.
Clays and Clay Minerals (1997) 45 (5): 618–631.
Article history
First Online:
02 Mar 2017
Citation
F. Leo Lynch; Frio shale mineralogy and the stoichiometry of the smectite-to-illite reaction; the most important reaction in clastic sedimentary diagenesis. Clays and Clay Minerals 1997;; 45 (5): 618–631. doi:
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Index Terms/Descriptors
- Brazoria County Texas
- Calhoun County Texas
- Cameron County Texas
- Cenozoic
- chemical reactions
- clastic rocks
- clay mineralogy
- clay minerals
- diagenesis
- Frio Formation
- Galveston County Texas
- geochemistry
- Gulf Coastal Plain
- Hidalgo County Texas
- illite
- Kenedy County Texas
- mass balance
- mineral composition
- Nueces County Texas
- Oligocene
- Paleogene
- San Patricio County Texas
- sedimentary rocks
- shale
- sheet silicates
- silicates
- smectite
- stoichiometry
- Tertiary
- Texas
- United States
- X-ray diffraction data
Latitude & Longitude
-
N29°04'00" - N29°34'60", W95°15'00" - W94°22'00" -
N28°40'00" - N29°40'00", W95°49'60" - W95°00'00" -
N28°07'00" - N28°45'00", W96°55'00" - W95°43'00" -
N27°30'00" - N27°55'00", W97°55'00" - W96°49'60" -
N27°49'60" - N28°13'60", W97°55'00" - W97°10'00" -
N26°03'00" - N26°46'00", W98°42'00" - W97°52'60" -
N26°34'60" - N27°10'00", W98°00'00" - W97°10'00" -
N25°45'00" - N26°19'60", W97°49'60" - W97°10'00"
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