radiogenic isotope sentence in Hindi
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- For radiogenic isotopes that decay slowly enough, or that are stable isotopes, a primordial fraction is always present, since all sufficiently long-lived and stable isotopes do in fact naturally occur primordially.
- All forms of isochron dating assume that the source of the rock or rocks contained unknown amounts of both radiogenic and non-radiogenic isotopes of the daughter element, along with some amount of the parent nuclide.
- A radiogenic isotope tracer involves an isotope produced by radioactive decay, which is usually in a ratio with a non-radiogenic isotope ( whose abundance in the earth does not vary due to radioactive decay ).
- A radiogenic isotope tracer involves an isotope produced by radioactive decay, which is usually in a ratio with a non-radiogenic isotope ( whose abundance in the earth does not vary due to radioactive decay ).
- Thus, at the moment of crystallization, the ratio of the concentration of the radiogenic isotope of the daughter element to that of the non-radiogenic isotope is some value independent of the concentration of the parent.
- Thus, at the moment of crystallization, the ratio of the concentration of the radiogenic isotope of the daughter element to that of the non-radiogenic isotope is some value independent of the concentration of the parent.
- Both short-lived and long-lived radiogenic isotopes indicate that a large-ion lithophile enriched reservoir ( which is the early " crustal " reservoir ) separated from the primitive mantle very early in the history of Mars.
- By the early 20th Century radiogenic isotopes had been discovered and British Association for the Advancement of Science came to a rough consensus that the Age of the Earth was a few billion years old, and that radiometric dating was credible.
- The relative abundances of different isotopes are then used to describe the chemical fractionation of different isotopes, travel in different reservoirs of non-radiogenic isotopes, and age or origins of solar system objects by the presence of radiogenic daughter isotopes.
- To wit, P-\ Delta { P } _ t, D + \ Delta { P } _ t and D _ i respectively correspond to the concentrations of parent, daughter and non-radiogenic isotopes found in the rock at the time of measurement.
- However, the natural abundance of a given isotope is also affected by the probability of its creation in nucleosynthesis ( as in the case of samarium; radioactive 147 Sm and 148 Sm are much more abundant than stable 144 Sm ) and by production of a given isotope as a daughter of natural radioactive isotopes ( as in the case of radiogenic isotopes of lead ).
- The ratios D + \ Delta { P } _ t \ over D _ i ( relative concentration of daughter and non-radiogenic isotopes ) and { P-\ Delta { P } _ t \ over D _ i } ( relative concentration of parent and non-radiogenic isotope ) are measured by mass spectrometry and plotted against each other in a three-isotope plot known as an " isochron plot ".
- The ratios D + \ Delta { P } _ t \ over D _ i ( relative concentration of daughter and non-radiogenic isotopes ) and { P-\ Delta { P } _ t \ over D _ i } ( relative concentration of parent and non-radiogenic isotope ) are measured by mass spectrometry and plotted against each other in a three-isotope plot known as an " isochron plot ".
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