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.
Your question has been heard loud and clear.
Both scientific laws and scientific theories are not based on hypothesis.
Because , scientific laws are proven and so they are real not hypothetical.
Whereas scientifc theories can be hypothetical.
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<span>f(t) = 250g * 0.9524^t
Since we have a half-life of 14.2 days we want to find an X such that
X^14.2 = 0.5
We can do that easily using logarithms. Just take the logarithm of 0.5, divide by 14.2, and the get the anti-log. So
10^(log(0.5)/14.2) = 10^(-0.301029996/14.2) =10^(-0.021199295) = 0.952359031 = 0.9524
So the function now becomes
f(t) = 250g * 0.9524^t
Let's check the function with a few test points at t = 14.2 and t = 28.4 which should return a result of 125 and 62.5 grams respectively. It will actually return slightly larger values since the growth constant was rounded up. But should be close enough to verify the formula
f(14.2) = 250g * 0.9524^14.2 = 250 * 0.500305517 = 125.0763791
f(28.4) = 250g * 0.9524^28.4 = 250 * 0.25030561 = 62.57
As predicted, the values are close, but slightly high. To demonstrate the effects of the rounding, consider this function using 0.952359031 as the growth factor.
250g * 0.952359031^ 28.4 = 250 * 0.25 = 62.5</span>
Answer:
A , B, C
Explanation: D is a Diamagnetic
No 500ml is not greater than 5L