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Directory UMM :Data Elmu:jurnal:J-a:Journal of Asian Earth Science:Vol18.Issue6.Dec2000:

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Fig. 2. Generalised stratigraphic columns in the area surveyed in western Sarawak. The thickness shown for the Lubok Antu Me´lange is only approximate.
Fig. 3. A measured section in the lowest part of the Silantek Formation to the south of the Lupar Fault Zone near Enkilili
Fig. 4. Stratigraphy in the area surveyed in western Sarawak. Age data from Haile (1957), Liechti et al
Fig. 5. Geological profiles in the surveyed area along the route shown in Fig. 1. The thin vertical bar crossing the profiles marks the boundary of each profile.
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1, Himalaya Terrane (Tethys sediments); 2, Gangdese Arc Complex; 3, me´lange zones; 4, the Liuqu Group; 5, ophiolitic massifs; 6, the Chongdui Formation; 7, the Angren Formation; 8,

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together with comparable island arc terranes now found in Papua New Guinea and the Philippines, are interpreted to have formed part of a roughly east±west intraoceanic island arc