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Aeromagnetic interpretation and general geology of Maran, Pahang Siti Humaira Mohammad.

By: Siti Humaira MohammadMaterial type: Text

TextPublisher: 2010Description: xvii, 78p. col., ill., maps 30cmSubject(s): Geology -- Pahang -- Maran | Aeromagnetic interpretation -- Pahang -- Maran | Maran (Pahang)Summary: The study is about aeromagnetic interpretation and general geology of Maran, Pahang area. The area is located at latitude from 3'27'00'N to 3'3712'N and longitude from 102'4210'E to 102'5830'E. The geology of the area consists of rock from upper Palaezoic rock, Tembeling Group, Semantan Formation, igneous rock in triassic age and alluvium deposit. Research has been done by emphasizing on the area of magnetic anomalies.

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Item type	Current location	Collection	Call number	Status	Date due	Barcode	Item holds
Books	JMG IBUPEJABAT Thesis	Thesis	555.9512314 SIT (Browse shelf)	Available		00002941

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Previous	555.95121 MAQ Geologi am kawasan Kuala Besar - Pantai Cahaya Bulan, Kelantan Darul Naim dengan penekanan terhadap kajian perubahan pesisian pantai	555.95121 MUS General geology of Renyok Waterfall with emphasize on the mineralogy and petrology of leucogranite and metasediments (enclaves)	555.95123 HAM Geologi dan permineralan emas di kawasan Chini Timur, Pahang	555.9512314 SIT Aeromagnetic interpretation and general geology of Maran, Pahang	555.951232 MHI General geology of Pos Belau, Jalan Cameron Highlands - Gua Musang	560.17 FAT Thesis Seismic Stratigraphic Interpretation and Facies Analysis of the Offshore Southern Gippsland Basin, Australia	560.1759512311 HAS Paleontogi dan Biostratigrafi Gunung Sinyum dan Gunung Jebak Puyuh, Jengka, Pahang Darul Makmur	Next

May, 2010.

Includes bibliographical references

The study is about aeromagnetic interpretation and general geology of Maran, Pahang area. The area is located at latitude from 3'27'00'N to 3'3712'N and longitude from 102'4210'E to 102'5830'E. The geology of the area consists of rock from upper Palaezoic rock, Tembeling Group, Semantan Formation, igneous rock in triassic age and alluvium deposit. Research has been done by emphasizing on the area of magnetic anomalies.

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