Abstract
A detailed discussion is presented on the possibility of determining the uranium and thorium content of ordinary rocks by observing ..cap alpha..-particle tracks in a photographic film applied to the rocks' surface. Such determinations can be made only where radioactive equilibrium can be assumed. For the examination of normal granite, exposures of several months are needed. The same method can be used to study the distribution of radioactive elements within the rock.
Citation Formats
Curie, I.
Possibility of studying the activity of rocks by the observation of. cap alpha. -particle tracks in a photographic emulsion.
France: N. p.,
1946.
Web.
Curie, I.
Possibility of studying the activity of rocks by the observation of. cap alpha. -particle tracks in a photographic emulsion.
France.
Curie, I.
1946.
"Possibility of studying the activity of rocks by the observation of. cap alpha. -particle tracks in a photographic emulsion."
France.
@misc{etde_5955957,
title = {Possibility of studying the activity of rocks by the observation of. cap alpha. -particle tracks in a photographic emulsion}
author = {Curie, I}
abstractNote = {A detailed discussion is presented on the possibility of determining the uranium and thorium content of ordinary rocks by observing ..cap alpha..-particle tracks in a photographic film applied to the rocks' surface. Such determinations can be made only where radioactive equilibrium can be assumed. For the examination of normal granite, exposures of several months are needed. The same method can be used to study the distribution of radioactive elements within the rock.}
journal = []
volume = {7}
journal type = {AC}
place = {France}
year = {1946}
month = {Jan}
}
title = {Possibility of studying the activity of rocks by the observation of. cap alpha. -particle tracks in a photographic emulsion}
author = {Curie, I}
abstractNote = {A detailed discussion is presented on the possibility of determining the uranium and thorium content of ordinary rocks by observing ..cap alpha..-particle tracks in a photographic film applied to the rocks' surface. Such determinations can be made only where radioactive equilibrium can be assumed. For the examination of normal granite, exposures of several months are needed. The same method can be used to study the distribution of radioactive elements within the rock.}
journal = []
volume = {7}
journal type = {AC}
place = {France}
year = {1946}
month = {Jan}
}