On the occurrence of Campanian rudist biostrome, Aruma Formation, Central Saudi Arabia
NOPR - NISCAIR Online Periodicals Repository
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Title |
On the occurrence of Campanian rudist biostrome, Aruma Formation, Central Saudi Arabia
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Creator |
El-Sorogy, Abdelbaset
Nour, Hamdy |
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Subject |
Rudist biostrome
Upper Cretaceous Campanian Aruma Formation Saudi Arabia |
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Description |
780-784
The lower limestone Khanasir Member of the Aruma Formation in central Saudi Arabia is characterized by Campanian rudist biostrome at its uppermost part. The most abundant rudist fauna are Eodictyoptychus arumaensis, Durania sp. and Biradiolites sp. Succession is overlying continental siliciclastics of Wasia Formation and comprises shale at the base followed by slightly dolomitized, burrow, nodular limestone and caps with rudist biostrome. Abundant microfacies types are wackestones, packstones, grainstones and floatstones with green algae, benthic foraminifers. The succession in general, indicated shallowing upward sequence and rudist biostrome represents a shallow marine lagoonal environment. |
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Date |
2017-04-05T10:16:50Z
2017-04-05T10:16:50Z 2017-04 |
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Type |
Article
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Identifier |
0975-1033 (Online); 0379-5136 (Print)
http://nopr.niscair.res.in/handle/123456789/41096 |
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Language |
en_US
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Rights |
CC Attribution-Noncommercial-No Derivative Works 2.5 India
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Publisher |
NISCAIR-CSIR, India
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Source |
IJMS Vol.46(04) [April 2017]
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