Miocene larger benthic foraminifera from the Kalumpang formation in Tawau, Sabah
Miocene larger benthic foraminifera have been discovered from a limestone unit of the Kalumpang Formation. The limestone is exposed at the Teck Guan Quarry, Tawau, southeast Sabah. The Kalumpang Formation consists predominantly of interbedded mudstone and sandstone (graywacke), conglomerate, limesto...
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| Format: | Article |
| Language: | English English |
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Universiti Kebangsaan Malaysia
2015
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| Online Access: | https://eprints.ums.edu.my/id/eprint/27483/1/Miocene%20Larger%20Benthic%20Foraminifera%20from%20the%20Kalumpang%20Formation%20in%20Tawau%2C%20Sabah%20ABSTRACT.pdf https://eprints.ums.edu.my/id/eprint/27483/2/Miocene%20larger%20benthic%20foraminifera%20from%20the%20Kalumpang%20formation%20in%20Tawau%2C%20Sabah%20FULL%20TEXT.pdf https://eprints.ums.edu.my/id/eprint/27483/ https://www.ukm.my/jsm/pdf_files/SM-PDF-44-10-2015/04%20Junaidi%20Asis.pdf |
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https://eprints.ums.edu.my/id/eprint/27483/1/Miocene%20Larger%20Benthic%20Foraminifera%20from%20the%20Kalumpang%20Formation%20in%20Tawau%2C%20Sabah%20ABSTRACT.pdfhttps://eprints.ums.edu.my/id/eprint/27483/2/Miocene%20larger%20benthic%20foraminifera%20from%20the%20Kalumpang%20formation%20in%20Tawau%2C%20Sabah%20FULL%20TEXT.pdf
https://eprints.ums.edu.my/id/eprint/27483/
https://www.ukm.my/jsm/pdf_files/SM-PDF-44-10-2015/04%20Junaidi%20Asis.pdf