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Genesis of chrysotile-asbestos veins and asbestos deposits
Hydrothermal solutions have moved along fractures and have generated reactions between olivine and solutions; reaction was followed by serpentinization and increase of volume, thus initiating fracturing and disintegration of rock; this fact made easier penetration of new solutions; important factor in studies is relation between thicknesses of chrysotile asbestos veins and bands of serpentinite.
Genesis of chrysotile-asbestos veins and asbestos deposits
Hydrothermal solutions have moved along fractures and have generated reactions between olivine and solutions; reaction was followed by serpentinization and increase of volume, thus initiating fracturing and disintegration of rock; this fact made easier penetration of new solutions; important factor in studies is relation between thicknesses of chrysotile asbestos veins and bands of serpentinite.
Genesis of chrysotile-asbestos veins and asbestos deposits
Genezis zhil khrizotil-asbesta i ego mestorozhdenii
Tatarinov, P.M. (author)
1966
13 pages
Article (Journal)
Russian
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