bab iii. kompoisi mineral batuan sedimen klastik
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MINERAL rock sediment composition KLASTIK be: › FRAGMEN : THAT PART grain size LARGE AND MOST can be a fraction-fraction rock, MINERAL, AND CANGKANG-fossil CANGKANG OR OTHER Organic substance. › MATRIK : Grain size PART THAT MORE AND SMALL PERCENTAGE OF fragments located between fragments Mass AS BASIS. MATRIK can be a rock, MINERAL, OR fossil. › SEMEN : CEMENT: CEMENT MATERIAL BUT NOT grain hollow ANTAR the binder Butir AND IN BETWEEN AND MATRIK fragments. Sediments DETRITUS Subtile ON CEMENT MUST BE FOR ANY grain can contact each other BOUND BY cohesion Individual Butir