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
Material type:
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.
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JMG IBUPEJABAT Thesis | Thesis | 551.095951122 SFA (Browse shelf) | Available | 00002933 |
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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