Science: v.1-v.219Moses King, 1966 |
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Page 1367
... present in olivine in the assemblage olivine + silica + iron is Fa68 , present at Q. Olivine in this assemblage becomes more iron- rich with cooling under all conditions of changing oxygen fugacity except with sharply decreasing fO2 ...
... present in olivine in the assemblage olivine + silica + iron is Fa68 , present at Q. Olivine in this assemblage becomes more iron- rich with cooling under all conditions of changing oxygen fugacity except with sharply decreasing fO2 ...
Page 1414
... present their findings in 17 chapters under four general headings : Geographical and clinical consideration . Nutrition and dental caries . Experimental considerations in oral soft tissue lesions . Prenatally induced oral anomalies ...
... present their findings in 17 chapters under four general headings : Geographical and clinical consideration . Nutrition and dental caries . Experimental considerations in oral soft tissue lesions . Prenatally induced oral anomalies ...
Page 1709
... present rate of overturn of the Atlantic deep water , on the order of a thousand years ( 43 ) would cer- tainly be shortened by a decrease in surface temperatures of perhaps as much as 10 ° C from the present mean of about 15 ° C . ( ii ) ...
... present rate of overturn of the Atlantic deep water , on the order of a thousand years ( 43 ) would cer- tainly be shortened by a decrease in surface temperatures of perhaps as much as 10 ° C from the present mean of about 15 ° C . ( ii ) ...
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