Mathematics – Logic
Scientific paper
Feb 1988
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988geokh......180r&link_type=abstract
Geokhimiia (ISSN 0016-7525), Feb. 1988, p. 180-199. In Russian.
Mathematics
Logic
Basalt, Chemical Composition, Earth Crust, Granite, Igneous Rocks, Sedimentary Rocks, Earth Planetary Structure, Earth Surface, Lithology, Phase Transformations
Scientific paper
A survey of a large (45,000 analyses) global-wide data base on the chemical composition of the three most abundant rocks of the earth's crust (shales, basalts, and granitoids) is conducted. It is demonstrated that, during the entire geological history of the earth, the average compositions of these genetically different rocks have undergone regular similarly-directed changes. For each of these rock types, a definite decreasing trend in the contents of Mg, Ni, Co, and Cr was accompanied by an increase in the contents of K, Rb, and REE, and other lithophile elements. These changes reflect the successive growth in the differentiation of the deep-seated material reaching the surface of the earth and of the products of its transformations. These changes in the rock composition are consistent with independently determined changes in the thermal regime of the earth's history and with data on the growth of the continental crust's mass and thickness.
Bredanova N. V.
Migdisov Art A.
Ronov A. B.
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