Magnetic interpretation and general geology of Chini - Pekan area, Pahang Noradiba Prayitno.

By: Noradiba PrayitnoMaterial type: TextTextPublisher: 2010 Description: xxi, 59 p. col. ill. , maps 30 cmSubject(s): Geology -- Pahang | Topography -- Pahang | Petrography -- Pahang
Contents:
June, 2010
Summary: The study area is located in Chini - Penyur, Pahang. the geology of the area consists of rocks from permian rock of Mersing Group, Triassic rock of the Jasin - Gayong and Tembeling Group, cretaceous rock of the Gagau Group and the quaternary alluvium deposit. Research has been done by emphasizing on the magnetic anomolies. The magnetic anomolies were identified from the airbone data taken from Ayocs and Paton (1958, 1960). Information of the magnetic contour and geological had been processes using software Didger (GSI, 2000), Surfer (GSI, 1999), Excel (Microsoft Office, 20007) and MAGMS (Boot, 1988).
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Includes bibliographical references

June, 2010

The study area is located in Chini - Penyur, Pahang. the geology of the area consists of rocks from permian rock of Mersing Group, Triassic rock of the Jasin - Gayong and Tembeling Group, cretaceous rock of the Gagau Group and the quaternary alluvium deposit. Research has been done by emphasizing on the magnetic anomolies. The magnetic anomolies were identified from the airbone data taken from Ayocs and Paton (1958, 1960). Information of the magnetic contour and geological had been processes using software Didger (GSI, 2000), Surfer (GSI, 1999), Excel (Microsoft Office, 20007) and MAGMS (Boot, 1988).

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