deep time 2 Flashcards
unstable isotopes
Many isotopes are in an unstable energy state
They will “decay” to gain a more stable state
Decay
-Emission of particles and energy to become more stable
Parent isotope
-Atom that decays
Daughter isotope
-Isotope that results from the decay
Half life: time it takes for half the isotopes in a group to decay into daughter isotopes
ex: Parent Potassium-40 (40K) decays to daughter Argon-40 (40Ar)
Half-life = 1.25 billion years
half life
The time it takes for half the parent isotope to decay into the daughter isotope
Example: Carbon-14
Half-life: 5730 years
14C decays to 14N
After 5730 years, half of the 14C is now 14N
After 11,460 years
75% of the 14C is now 14N
After 17,190 years
87.5% of the 14C is now 14N
cab’t use carbon 14 in geology because it’s not old enough
after two half lives you have 1/4. You take half of remaining isotopes in second half life: theoretically: you can never get to zero. in reality after 1 your down to zero(can’t be 1/2)
Radioactive Dating
Age determination
- Measures the ratio of the parent-to-
daughter isotopes
Analytical precision and the right minerals
from table screen shot now rb, k, u ones. don’t memorize half lives of them
Confused by radiometric age determination? Hoped there would be no math in this class? Have no fear, your radiometric cheat sheet is here!
see screen shot
half life calculation example: You have a rock that, upon careful analysis, has only 1/16 of the original Fake Isotope remaining. Fake Isotope has a half-life of 1.28 million years. How old is your rock?
it takes 4 half lives to get to 1/16
1.28x4= 5.12 million years
relative dating: see screenshot and try to put them in order
EGLCHMDJANKBF
isotopes
Change the number of neutrons
Same element, different isotope
Example: Helium
Atomic number: 2
Total of neutrons and protons: 4 – in the idealized element
This would be known as the 4He isotope
Other helium isotopes
3He = 2 protons, 1 neutron
6He = 2 protons, 4 neutrons
small dots on relative dating map show
baked rocks around intrusion, wherever baked marks stop that rock is younger than the intrusion their meeting is an incomformity between crystal and rock ; rocks with baked marks are older than the intrusion no matter how deep it reaches
angles that don’t match up on relative dating map
angular uncomformity