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The position of the laki limestone in the eocene succession of Western Pakistan

By: Eames, F.E.
Material type: ArticleArticleDescription: 214-216p.Subject(s): Laki limestone - Western Pakistan | Eocene succession - Western Pakistan | Historical geology - Pakistan In: Geological magazine : Vol. 87 Iss. 1-6 Year. 1950Summary: Abstract It has previously been thought that in Sind the Meting Limestone Laki Limestone succession was equivalent to the Bolan Limestone, and that argillaceous beds, which are occasionally developed above the Laki Limestone and below the overlying Khirthar, represented the Ghazij Shales. Recent evidence indicates that these higher argillaceous beds are the representatives of the Shales with Alabaster of the Western Punjab, that in Sind the Ghazij Shales are cut out at the Laki/Ranikot unconformity, and that the Meting Limestone-Laki Limestone succession represents calcareous horizons higher up in the Laki series than the Bolan Limestone.
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Article Article Library and Information Centre
Periodical Section
Bound Journal Collection Not for loan 002560_38
Serials/Scientific Journal Serials/Scientific Journal Library and Information Centre
Periodical Section
Bound Journal Collection 550 GEO (Browse shelf) Available 002560

Abstract
It has previously been thought that in Sind the Meting Limestone Laki Limestone succession was equivalent to the Bolan Limestone, and that argillaceous beds, which are occasionally developed above the Laki Limestone and below the overlying Khirthar, represented the Ghazij Shales. Recent evidence indicates that these higher argillaceous beds are the representatives of the Shales with Alabaster of the Western Punjab, that in Sind the Ghazij Shales are cut out at the Laki/Ranikot unconformity, and that the Meting Limestone-Laki Limestone succession represents calcareous horizons higher up in the Laki series than the Bolan Limestone.

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