bab iii. kompoisi mineral batuan sedimen klastik


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