There is no question about it

Binding energy potassium 40 dating

Beta-minus decay indicates a nucleus with too many neutrons, electron capture a nucleus with too many protons. Thus these rocks give a date which is older than what normally would happen if the rocks were fully reset.

Betaminus decay indicates a

Man is thought to have progressed through a long period of prehistory cave man's experience before some sort of civilization is started. An interesting point to make is that the Potassium-Argon process does not date the age of the rock.

Thus these rocks give a

However there may be a new development in the field of nuclear reactions that could change this situation. Before we start, lets look at the specific K-Ar dating assumptions. So in both cases the Argon flows down the concentration gradient. These are the areas that deal with the here and now. They rapidly lose their kinetic energy as they pass through matter.

Only the rocks in the precambrian layers could have been affected by the creation event. We do not have an issue of weight of evidence. On the other hand, It is possible that the creation event could have caused changes in the half-lives of nuclides.

When the rock is molten hot, it is more liquid in texture, allowing the Argon gas to escape. The process can continue until some answer to the problem is understood. These flows are on the surface of the earth, where the Argon is able to escape into the atmosphere. They are looking for answers that would fit their present model. The product of -decay is easy to predict if we assume that both mass and charge are conserved in nuclear reactions.

The problem is only limited by money, ingenuity, and the technical difficulties that have to be surmounted. The ratio of neutrons to protons in stable nuclides gradually increases as the number of protons in the nucleus increases.

The heating only allows the Argon gas to reach equilibrium with its surroundings. The neutrinos emitted in these captures defy detection. Synthetic introduction of argon into mica at high pressures and temperatures.