Use of Tmax as a maturation index for different types of organic matter: comparison with vitrinite reflectance
- Other title
- Utilisation des valeurs Tmax comme indice de maturation pour différents types de matière organique. Comparaison avec le pouvoir réflecteur de la vitrinite (fr)
- Author
- ESPITALIE, J1
[1] Inst. français pétrole, Rueil-Malmaison, France - Conference name
- IFP exploration research conference. 1 (1985)
- Source
Collection colloques et séminaires - Institut français du pétrole. 1986, Num 44, pp 475-496 ; Illustration , Table ; ref : 3 p
- Publisher
- Technip, Paris
- Publication country
- France
- Document type
- Conference Paper
- Language
- English
- Keyword (fr)
- Bassin Parisien Bassin Uinta Charbon Colorado Jurassique inf Matière organique Maturation Pouvoir réflecteur Pyrolyse Température Vitrinite Westphalien Shale Green River Amérique du Nord Carbonifère sup Etats Unis Europe France Primaire Roche carbonée Roche sédimentaire Secondaire
- Keyword (en)
- Paris Basin Uinta Basin Coal Colorado Lower Jurassic Organic materials Maturity Reflectance Pyrolysis Temperature Vitrinite Westphalian Europe France Mesozoic North America Organic residues Paleozoic Sedimentary rocks United States Upper Carboniferous
- Keyword (es)
- Region parisina Cuenca Uintal Carbon Colorado Jurásico inf Materia organica Maduracion Poder reflector Pirolisis Temperatura Vitrinita Westfaliense América del norte Carbonífero sup Estados Unidos Europa Francia Roca carbonosa Roca sedimentaria
- Classification
- Pascal
- 001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01G Sedimentary rocks / 001E01G02 Coal
- Discipline
- Earth sciences
- Origin
- Inist-CNRS
- Database
- PASCAL
- INIST identifier
- 7895690
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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