Aeromagnetic interpretation and the general geology of Bandar Pusat Jengka, Jerantut area Nur Ain Anuar
Material type:
TextPublisher: 2010Description: v, 48 p. col. ill. , maps 30 cmSubject(s): Dissertations, Academic -- Malaysia | Geology -- Pahang -- Jengka -- Survey | Geology -- Pahang -- Jerantut | Jengka, Jerantut (Pahang) -- Survey | Jerantut (Pahang) -- SurveyDissertation note: Thesis (B.Sc) Applied Geology - Universiti Malaya, 2010 Summary: The study area is located along the way fom North Temerloh passing by Bandar Pusat Jengka, a small town in Maran district and extends up until Kota Gelanggi in Jerantut. It covers from latitude 3.65 north up to 3.90 north, and longitude 102.43 east until 102.72 east. The geology of this area is largely occupied by sedimentary rocks. Semantan formation aged ikate - mid triassic is the major formation within the study area, where the rocks are interbedded shale / mudstone with tuff, wackestone, limestone and chert
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JMG IBUPEJABAT Thesis | Thesis | 551.095951231 NAA (Browse shelf) | Available | 00002935 |
Thesis (B.Sc) Applied Geology - Universiti Malaya, 2010
The study area is located along the way fom North Temerloh passing by Bandar Pusat Jengka, a small town in Maran district and extends up until Kota Gelanggi in Jerantut. It covers from latitude 3.65 north up to 3.90 north, and longitude 102.43 east until 102.72 east. The geology of this area is largely occupied by sedimentary rocks. Semantan formation aged ikate - mid triassic is the major formation within the study area, where the rocks are interbedded shale / mudstone with tuff, wackestone, limestone and chert
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