Mica alteration reactions in Jurassic reservoir sandstones from the Haltenbanken area, offshore Norway

S. Morad

doi:10.1346/CCMN.1990.0380603

Mica alteration reactions in Jurassic reservoir sandstones from the Haltenbanken area, offshore Norway

S. Morad

Earth Science

Research output: Contribution to journal › Article › peer-review

49 Scopus citations

Abstract

Suggests limited elemental mobility during sandstone diagenesis. The alteration of mica to kaolinite occurred in sandstones buried <200 m deep (present temperature <70°C), whereas illitization and chloritization of biotite occurred during burial to depths >3000 m (present temperature >95°C). -from Author

Original language	British English
Pages (from-to)	584-590
Number of pages	7
Journal	Clays & Clay Minerals
Volume	38
Issue number	6
DOIs	https://doi.org/10.1346/CCMN.1990.0380603
State	Published - 1990

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title = "Mica alteration reactions in Jurassic reservoir sandstones from the Haltenbanken area, offshore Norway",

abstract = "Suggests limited elemental mobility during sandstone diagenesis. The alteration of mica to kaolinite occurred in sandstones buried <200 m deep (present temperature <70°C), whereas illitization and chloritization of biotite occurred during burial to depths >3000 m (present temperature >95°C). -from Author",

author = "S. Morad",

year = "1990",

doi = "10.1346/CCMN.1990.0380603",

language = "British English",

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pages = "584--590",

journal = "Clays \& Clay Minerals",

publisher = "Clay Minerals Society",

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T1 - Mica alteration reactions in Jurassic reservoir sandstones from the Haltenbanken area, offshore Norway

AU - Morad, S.

PY - 1990

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N2 - Suggests limited elemental mobility during sandstone diagenesis. The alteration of mica to kaolinite occurred in sandstones buried <200 m deep (present temperature <70°C), whereas illitization and chloritization of biotite occurred during burial to depths >3000 m (present temperature >95°C). -from Author

AB - Suggests limited elemental mobility during sandstone diagenesis. The alteration of mica to kaolinite occurred in sandstones buried <200 m deep (present temperature <70°C), whereas illitization and chloritization of biotite occurred during burial to depths >3000 m (present temperature >95°C). -from Author

UR - https://www.scopus.com/pages/publications/0025621117

U2 - 10.1346/CCMN.1990.0380603

DO - 10.1346/CCMN.1990.0380603

M3 - Article

AN - SCOPUS:0025621117

VL - 38

SP - 584

EP - 590

JO - Clays & Clay Minerals

JF - Clays & Clay Minerals

IS - 6

ER -

Mica alteration reactions in Jurassic reservoir sandstones from the Haltenbanken area, offshore Norway

Abstract

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