Radiometric dating paper

Thus, determining the age of the Earth with alternative techniques could serve to strengthen the conclusions that have been reached with radioisotope dating methods.

In this paper, a different approach to solving the problem is proposed.

Studies of geological time typically begin with event relation determinations (early–late events, ancient–recent events) and finish with continuity determinations and positioning on the modern geochronological scale.

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Such estimates can span from the modern era into the deep geological past and are presented in descending order (i.e., from the past to the present).

The estimates are derived from isotope data, which are converted into radiological ages.

To obtain a truly absolute chronology, corrections must be made, provided by measurements on samples of know age.

The most suitable types of sample for radiocarbon dating are charcoal and well-preserved wood, although leather, cloth, paper, peat, shell and bone can also be used.

As is known from studies of 400 million year old fossil corals, Earth years were 400 days in duration in distant times because the Earth rotated faster than it does today.

According to calculations based on the fundamental law of rotational motion dynamics involving the moment of inertia of a body, the radius of the ancient Earth 400 million years ago was 553.379 km less than it is today.

In the latter case, quantitative estimates of time are conducted in modern astronomical units—years or Earth’s rotation time around the Sun.

Specific geological ages, which can be referred to as absolute times versus relative times, are determined conventionally by radiometric methods.

Visit for more related articles at International Journal of Advance Innovations, Thoughts & Ideas Radioisotope dating has revealed that the age of the Earth is 4.54–4.6 billion years, and these results are widely accepted.

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