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Frans S.P. van Buchem

Researcher at Maersk Oil

Publications -  29
Citations -  1416

Frans S.P. van Buchem is an academic researcher from Maersk Oil. The author has contributed to research in topics: Sedimentary depositional environment & Facies. The author has an hindex of 17, co-authored 26 publications receiving 1261 citations. Previous affiliations of Frans S.P. van Buchem include Institut Français & Maersk.

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Stratigraphic organization of carbonate ramps and organic-rich intrashelf basins: Natih Formation (middle Cretaceous) of northern Oman

TL;DR: In this article, a high-resolution sequence stratigraphic study of the Natih Formation in Oman is presented, which shows distinct and predictive patterns in the distribution and geometries of reservoir, source rock, and seal facies.
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High Resolution Sequence Stratigraphy of the Natih Formation (Cenomanian/Turonian) in Northern Oman: Distribution of Source Rocks and Reservoir Facies

TL;DR: In this paper, a high-resolution sequence stratigraphic study has been carried out in the Adam Foothills of Northern Oman, where three orders of stacked depositional sequences have been found based on the reoccurrence of facies.
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Ecological succession, palaeoenvironmental change, and depositional sequences of Barremian–Aptian shallow‐water carbonates in northern Oman

TL;DR: In this article, three orders of depositional sequences are defined (third to fifth order) and correlated between sections over the course of three third-order sequences, covering the Barremian to Lower Aptian, a thirdorder depositional pattern is documented that consists of a succession of three distinct faunal assemblages: discoidal orbitolinids and calcareous algae were deposited during early transgression; microbialites and microencrusters dominated the late transgressive to early highstand facies; and a rudist and milioliddominated facies is typical
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The Barremian-Aptian Evolution of The Eastern Arabian Carbonate Platform Margin (Northern Oman)

TL;DR: In this article, a detailed sedimentological and sequence stratigraphic model of the platform margin of the Cretaceous carbonate margin is presented to reveal the relative importance of global and regional controls on platform evolution.