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Oxygen-isotope evidence for upward, cross-formational porewater flow in a sedimentary basin near maximum burial

Author
DE CARITAT, P; BAKER, J. C
Univ. Calgary, dep. geology geophysics, Calgary AB T2N 1N4, Canada
Source

Sedimentary geology. 1992, Vol 78, Num 3-4, pp 155-164 ; Illustration , Table ; ref : 33 ref

CODEN
SEGEBX
ISSN
0037-0738
Scientific domain
Geology
Publisher
Elsevier, Amsterdam
Publication country
Netherlands
Document type
Article
Language
English
Keyword (fr)
Ankerite Authigenèse Bassin sédimentaire C 13-C 12 Carbonate Diagenèse Eau connée Eau interstitielle Grès Isotope stable O 18-O 16 Permien moyen Trias Grès Aldebaran Queensland Roche clastique Roche sédimentaire Secondaire Australasie Australie
Keyword (en)
ankerite authigenesis sedimentary basins C-13/C-12 carbonates diagenesis connate waters pore water sandstone stable isotopes O-18/O-16 Middle Permian Triassic Queensland clastic rocks sedimentary rocks Mesozoic Australasia Australia
Keyword (es)
Ankerita Autigénesis Cuenca sedimentaria fósil C 13-C 12 Carbonato Diagénesis Agua connata Agua intersticial Gres Isótopo estable O 18-O 16 Pérmico medio Triásico Queensland Roca clástica Roca sedimentaria Secundario Australasia Australia
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01C Isotope geochemistry. Geochronology / 001E01C01 Isotope geochemistry

Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01G Sedimentary rocks / 001E01G01 Petrology of sedimentary rocks except quaternary rocks

Discipline
Earth sciences
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
5440799

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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