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Petrology of the Sams Creek peralkaline granite dike, Takata, New Zealand

Author
TULLOCH, A. J
DSIR geology & geophysics, Lower Hull, New Zealand
Source

New Zealand Journal of Geology and Geophysics. 1992, Vol 35, Num 2, pp 193-200 ; Illustration , Table ; ref : 1 p

CODEN
NEZOAY
ISSN
0028-8306
Scientific domain
Geology; Geophysics
Publisher
Department of Scientific and Industrial Research, Wellington
Publication country
New Zealand
Document type
Article
Language
English
Keyword (fr)
Aegirine Analyse chimique Arfvedsonite Axe pli Composition hyperalcaline Datation Direction Dyke Granite Ilmenite K-Ar Microscopie Métamorphisme régional Pétrologie Riebeckite Trias Nouvelle Zélande Roche ignée Secondaire Australasie
Keyword (en)
aegirine chemical composition arfvedsonite fold axes peralkalic composition absolute age strike dikes granites ilmenite K/Ar microscope methods regional metamorphism petrology riebeckite Triassic New Zealand igneous rocks Mesozoic Australasia
Keyword (es)
Egirina Análisis químico Arfvedsonita Eje de plegamiento Composición hiperalcalina Fechado Dirección Dique Granito Ilmenita K-Ar Microscopía Metamorfismo regional Petrología Riebequita Triásico Nueva Zelandia Roca ignea Secundario Australasia
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01F Crystalline rocks / 001E01F01 Igneous and metamorphic rocks petrology, volcanic processes, magmas

Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01L Tectonics. Structural geology. Plate tectonics

Discipline
Earth sciences
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
5369038

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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