Structure, stratigraphy, and sedimentology of Mong Gajah area, along km 36.1 to km 41.6, Trans Eastern Kedah Interland Highway, Kedah Sheikh Fadzil Mohamed
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TextPublisher: 2009Description: x, 55 p. col. ill., maps 30 cmSubject(s): Projek Lebuhraya Lingkaran Timur Kedah | Sedimentation and deposition -- Kedah | Sediments (Geology) -- Kedah | Geology -- Kedah -- Survey | Geology, StratigraphicSummary: The area study consists of Semanggol formation which range in age from Lower Permian to Upper Triassic. The main lithology of the Semanggol formation that can be found in the study area is consist of interbedded sandstone - shale and conglomerate belonging to the rhytmite and conglomerate member respectively. The rhythmite member also known as turbidite sequence, can be further be divided into two main facies namely thick sandstone - thick shale which and thin sandstone - thin shale. The conglomerate member that is found in the study area can be clasified as poorly sorted, matric supported conglomerate.
| Item type | Current location | Collection | Call number | Status | Date due | Barcode | Item holds |
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Books
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JMG IBUPEJABAT Thesis | Thesis | 551.095951122 SFA (Browse shelf) | Available | 00002933 |
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| 551.09595 FER Geology kawasan Felda Chiku, Gua Musang, Kelantan | 551.09595112 MLM Geology of Sungai Tiang area with emphasis on quaternary sediments | 551.09595112 MZA Pemetaan geoelektrik di kawasan Kubang Rotan, Kedah | 551.095951122 SFA Structure, stratigraphy, and sedimentology of Mong Gajah area, along km 36.1 to km 41.6, Trans Eastern Kedah Interland Highway, Kedah | 551.0959511222 MFM Geology of Pandang Terap area with emphasis on quaternary sediments | 551.09595113 SNL Geology and slope assessment along Jalan Tun Sardon, Penang | 551.09595113 SNL Geology and slope assessment along Jalan Tun Sardon, Penang |
Student project paper, May 2009
Includes bibliographical references
The area study consists of Semanggol formation which range in age from Lower Permian to Upper Triassic. The main lithology of the Semanggol formation that can be found in the study area is consist of interbedded sandstone - shale and conglomerate belonging to the rhytmite and conglomerate member respectively. The rhythmite member also known as turbidite sequence, can be further be divided into two main facies namely thick sandstone - thick shale which and thin sandstone - thin shale. The conglomerate member that is found in the study area can be clasified as poorly sorted, matric supported conglomerate.
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