Citation
Kamal Roslan Mohamed, . and Che Aziz Ali, . (2007) Microfacies diagenesis and depositional setting of Kenong limestone. In: Taman Rimba Kenong Pahang: Pengurusan persekitaran fizikal dan kepelbagaian biologi. Jabatan Perhutanan Semenanjung Malaysia, Kuala Lumpur (Malaysia), pp. 66-71. ISBN 978-983-9269-58-1
Abstract
Kenong Limestone which is part of the Gua Musang Formation was deposited in shallow marine setting during the Middle Permian to early Triassic period. The deposition occurred during a phase of volcanic activity in the region which is marked by the presenc
Download File
Full text available from:
|
Abstract
Kenong Limestone which is part of the Gua Musang Formation was deposited in shallow marine setting during the Middle Permian to early Triassic period. The deposition occurred during a phase of volcanic activity in the region which is marked by the presenc
Additional Metadata
| Item Type: | Book Section |
|---|---|
| Additional Information: | 6 ref. |
| AGROVOC Term: | Limestone |
| AGROVOC Term: | Rock |
| AGROVOC Term: | Geology |
| AGROVOC Term: | Malaysia |
| Geographical Term: | MALAYSIA |
| Depositing User: | Mr. AFANDI ABDUL MALEK |
| Last Modified: | 24 Apr 2025 00:50 |
| URI: | http://webagris.upm.edu.my/id/eprint/6233 |
Actions (login required)
 |
View Item |
