Facies Analysis, Sedimentology and Paleocurrent of The Quaternary Nenering Formation, Pengkalan Hulu, Malaysia
Nenering Formation is essentially made up of semi-consolidated sediments, which are divided into basal conglomerate beds, conglomeratic sandstone, cross-bedded sandstone, and siltstone to muddy layers facies. It is overlie unconformable to the Berapit Formation, but conformable to the Kroh and Grik...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Center for Nuclear Minerals Technology
2014-11-01
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| Series: | Eksplorium: Buletin Pusat Pengembangan Bahan Galian Nuklir |
| Subjects: | |
| Online Access: | http://jurnal.batan.go.id/index.php/eksplorium/article/view/2755 |