Groundwater potential in Gajah Puteh, Mukim Jeneri, Sik, Kedah : RAK (D1) Zahir Yahya.
Material type:
TextPublisher: 2004Description: iv, 25p. col., ill., maps 30cmSubject(s): Hydrology -- Kedah -- Gajah Puteh | Physiography -- Kedah -- Gajah Puteh | Topography -- Kedah -- Gajah Puteh | Hydrogeology -- Kedah -- Gajah Puteh | Geology -- Kedah -- Gajah Puteh | Gajah Puteh (Mukim Jeneri, Sik, Kedah)Summary: The well located near the Muda River which is main drainage system in Kedah. The study area is underlained by Mahang Formation consisting of phyllite, shale, mudstone and sandstone. The area is highly deformed with occurrences of fault, fracture and folding as a result of granite intrusion. The well is located 1km from the major Bok-bak fault in the east.
| Item type | Current location | Collection | Call number | Status | Date due | Barcode | Item holds |
|---|---|---|---|---|---|---|---|
| Reports | BPT Open Shelf | Report | 553.7909595 ZAH (Browse shelf) | Available | |||
| Reports | JMG IBUPEJABAT Open Shelf | Open Shelf | 553.7909595 ZAH (Browse shelf) | Available | 00003266 |
Total holds: 0
Browsing JMG IBUPEJABAT shelves, Shelving location: Open Shelf, Collection: Open Shelf Close shelf browser
| 553.7909595 POT Potential of groundwater resources in Malaysia and recommendation for their planned development | 553.7909595 POT Potential of groundwater resources in Malaysia and recommendation for their planned development | 553.7909595 SEN Senarai laporan teknikal Pusat Penyelidikan Mineral | 553.7909595 ZAH Groundwater potential in Gajah Puteh, Mukim Jeneri, Sik, Kedah : RAK (D1) | 553.7909595 ZAH Groundwater potential in Gajah Puteh, Mukim Jeneri, Sik, Kedah | 553.7909595 ZAH Groundwater potential in Gajah Puteh, Mukim Jeneri, Sik, Kedah | 553.7909595111 ZAH Potensi air tanah di Sungai Batu Pahat, Perlis |
Includes bibliographical references
The well located near the Muda River which is main drainage system in Kedah. The study area is underlained by Mahang Formation consisting of phyllite, shale, mudstone and sandstone. The area is highly deformed with occurrences of fault, fracture and folding as a result of granite intrusion. The well is located 1km from the major Bok-bak fault in the east.
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