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Lithofacies and biomarkers in Precambrian Nonesuch Formation : Petroleum source potential of midcontinent rift system, North America

Other title
Lithofaciès et biomarqueurs dans la Formation Nonesuch (Antécambrien): potentiel pétrolier d'un système de rift du Midcontinent, Amérique du Nord (fr)
Author
PRATT, L.M; HIESHIMA, G.B; HAYES, J.M; SUMMONS, R.E
Indiana univ., Bloomington IN, United States
Conference title
International geological congress. 28
Conference name
International geological congress. 28 (1989-07-09)
Source

International geological congress. 28. 1989, pp 637-638, 2 p

Document type
Conference Paper
Language
English
Keyword (fr)
Carbone organique Composé hydrocarbure Keweenaw Maturation Protérozoïque sup Roche clastique Roche mère Sédimentation lacustre Wisconsin Amérique du Nord Amérique Antécambrien Etats Unis Roche sédimentaire
Keyword (en)
Organic carbon Hydrocarbons Keweenawan Maturity Ripening Upper Proterozoic Clastic rocks Source rocks Parent rock Lacustrine sedimentation Wisconsin America North America Precambrian Sedimentary rocks United States
Keyword (es)
Carbono orgánico Compuesto hidrocarburo Maduración Proterozoico sup Roca clástica Roca madre Sedimentación lacustre Wisconsín America del norte America Antecámbrico Estados Unidos Roca sedimentaria
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01B Geochemistry / 001E01B03 Soil and rock geochemistry

Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01G Sedimentary rocks / 001E01G03 Hydrocarbons

Discipline
Earth sciences
Origin
BRGM
Database
PASCAL
INIST identifier
19379919

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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