The Olivine normally crystalizes first from the magma of the mafic minerals, It crystalizes at between 1200°C and 1300°C. when the temperature of magma drops and there is a silica still remains in the magma so the olivine reacts with this silica to form pyroxene.and by more cooling of the temperature of magma and there is a silica still remains in magma pyroxene change to amphibole, and amphibole to biotite.when the pyroxene strat to form the plagioclase feldspar also forms.
Answer:
Rate law:
Integrated Rate Law:
Explanation:
We can see that the graph of time is linear compared to and the reaction is second order hence we get the rate law from .
The integrated rate law for second order is where A is .
The slope of the graph w.r.t time is equal to k. The slope of the graph from the table is 0.014 which is equal to k.
Answer:
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