A new method for estimating the age of the earth consists of calculating a Pb^207 / Pb^206 age from the observed differences between the isotropic composition of recent lead isolated from the surface of the earth where appreciable concentrations of uranium exist and the isotropic composition of lead isolated from iron meteorites where insignificant concentrations of uranium are found (1-3)
AbstractA model of a giant impact between two planetary bodies is widely accepted to account for the...
The results which have been found concerning the age of rocks determine the time which has elapsed s...
Precise determinations of the isotopic compositions of a variety of elements is a widely applied too...
A new method for estimating the age of the earth consists of calculating a Pb^207 / Pb^206 age from ...
Methods of using isotopic abundances of dated common lead samples to obtain the time since which the...
This web page addresses the question: How do we know the Age of the Earth? by citing radiometric dat...
The best estimate for the age of the material which forms the Earth is 4,566 million years, which is...
The first geochronological date obtained one century ago by Rutherford via the measurement of accumu...
Abstract: This paper presents a brief historical review of various attempts to estimate the age of t...
Unravelling the Earth’s 4.5-billion-year history is a mammoth task. Joe Hiess and Dan Condon describ...
The method of dating rocks and minerals is known as geochronology. Although in principle this term c...
Abstract The age of a fossil bone can be determined based on the chain of radioactive uranium as far...
one of the most common titles in the geological literature, and with good reason. The scientific and...
Thesis (M.A.)--Boston University, 1938. This item was digitized by the Internet Archive
Quantification of geological time represents one of the fundamental challenges for earth scientists...
AbstractA model of a giant impact between two planetary bodies is widely accepted to account for the...
The results which have been found concerning the age of rocks determine the time which has elapsed s...
Precise determinations of the isotopic compositions of a variety of elements is a widely applied too...
A new method for estimating the age of the earth consists of calculating a Pb^207 / Pb^206 age from ...
Methods of using isotopic abundances of dated common lead samples to obtain the time since which the...
This web page addresses the question: How do we know the Age of the Earth? by citing radiometric dat...
The best estimate for the age of the material which forms the Earth is 4,566 million years, which is...
The first geochronological date obtained one century ago by Rutherford via the measurement of accumu...
Abstract: This paper presents a brief historical review of various attempts to estimate the age of t...
Unravelling the Earth’s 4.5-billion-year history is a mammoth task. Joe Hiess and Dan Condon describ...
The method of dating rocks and minerals is known as geochronology. Although in principle this term c...
Abstract The age of a fossil bone can be determined based on the chain of radioactive uranium as far...
one of the most common titles in the geological literature, and with good reason. The scientific and...
Thesis (M.A.)--Boston University, 1938. This item was digitized by the Internet Archive
Quantification of geological time represents one of the fundamental challenges for earth scientists...
AbstractA model of a giant impact between two planetary bodies is widely accepted to account for the...
The results which have been found concerning the age of rocks determine the time which has elapsed s...
Precise determinations of the isotopic compositions of a variety of elements is a widely applied too...