Survei geologi marin di perairan Teluk Brunei hingga Kota Kinabalu, Sabah laporan geofizik Hairani Sham Manas, Rohimi Che Wan
Material type:
TextPublisher: 1997Description: v, 18p. col. ill. 30 cmSubject(s): Marine sediments -- Sabah -- Teluk Brunei | Submarine geology -- Sabah -- Teluk Brunei | Teluk Brunei (Sabah) | Kota Kinabalu (Sabah)Summary: Echo sounding records indicate the sea floor to be generally flat in Teluk Brunei ang Teluk Kimanis with depth of 18 meters, and increasing gradually to 45 meters into the open sea with an average of 25 meters. In the open sea area, water column varies between 10 meters and 60 meters du to the presence of shoals and banks.
| Item type | Current location | Collection | Call number | Status | Date due | Barcode | Item holds |
|---|---|---|---|---|---|---|---|
| Reports | JMG IBUPEJABAT Open Shelf | Open Shelf | 551.4680959521 HAI (Browse shelf) | Available | 00003419 |
Total holds: 0
Browsing JMG IBUPEJABAT shelves, Shelving location: Open Shelf, Collection: Open Shelf Close shelf browser
| 551.46809595119 SUR Survei geologi marin di perairan Johor Barat dan Johor Timur | 551.4680959512331 ARA Survei geologi marin susulan di perairan Kuantan, Pahang Darul Makmur | 551.4680959512331 ARA Survei geologi marin susulan di perairan Kuantan, Pahang Darul Makmur | 551.4680959521 HAI Survei geologi marin di perairan Teluk Brunei hingga Kota Kinabalu, Sabah | 551.4680959523 REC Reconnaissance marine geophysical and sampling surveys offshore Pulau Labuan, federal territory | 551.4680959523 REC Reconnaissance marine geophysical and sampling surveys offshore Pulau Labuan, federal territory | 551.46859511931 LAP Laporan bersepadu |
Includes bibliographical references
Echo sounding records indicate the sea floor to be generally flat in Teluk Brunei ang Teluk Kimanis with depth of 18 meters, and increasing gradually to 45 meters into the open sea with an average of 25 meters. In the open sea area, water column varies between 10 meters and 60 meters du to the presence of shoals and banks.
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