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santubong quarry

3216 Hornfels at Tanjung Santubong The northern tip of Tanjung Santubong is separated by a NWSE trending fault from the rest of Santubong It is composed of thinly bedded reddish mudstone interbedded with thin hornfelsed sandstone Fig 7d and thicker hornfelsed sandstone packages These lithologies have been intruded by a granitic sill

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