Stratigraphy of the Ransi Member of the Middle Eocene to Oligocene Tatau Formation in the Tatau-Bintulu area, Sarawak, East Malaysia / Wong Yien Lim
A recent study in the Tatau-Bintulu area indicates that the Ransi Member which was originally dated as Upper Miocene to Pliocene (Kamaludin Hassan, 2004) is part of the Upper Eocene to Upper Oligocene Tatau Formation. This finding is inconsistent with that of Liechti, et.al (1960) who proposed that...
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http://studentsrepo.um.edu.my/3871/3/Chapter_2_General_Geology_%26_Structure.pdf
http://studentsrepo.um.edu.my/3871/4/Chapter_3_METHODOLOGY.pdf
http://studentsrepo.um.edu.my/3871/6/Chapter_4_Stratigraphy.pdf
http://studentsrepo.um.edu.my/3871/5/Chapter_5_PETROLOGY_OF_CONGLOMERATE_AND_SANDSTONE.pdf
http://studentsrepo.um.edu.my/3871/7/Chapter_6_Environment.pdf
http://studentsrepo.um.edu.my/3871/8/Chapter_7_CONCLUSION.pdf
http://studentsrepo.um.edu.my/3871/9/References.pdf
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