Science: v.1-v.219Moses King, 1972 |
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Стр. 860
... determined by ion microprobe mass anal- ysis for five separate feldspar grains . The initial Sr / Sr ratio and the isochron of 1860 X 10 " years were determined by Tilton and Sinha ( 26 ) for bulk specimens , with isotope dilution . The ...
... determined by ion microprobe mass anal- ysis for five separate feldspar grains . The initial Sr / Sr ratio and the isochron of 1860 X 10 " years were determined by Tilton and Sinha ( 26 ) for bulk specimens , with isotope dilution . The ...
Стр. 1000
... determined by calculating the filtered load ( serum P , XGFR ) , and measuring the excreted P in urine ( P , per milliliter times flow rate [ milliliters per minute ] ) ; the reabsorbed amount was calculated as the difference and ...
... determined by calculating the filtered load ( serum P , XGFR ) , and measuring the excreted P in urine ( P , per milliliter times flow rate [ milliliters per minute ] ) ; the reabsorbed amount was calculated as the difference and ...
Стр. 1246
... determined in this study ( ref . 14 ) Previously published values ( refs . 2-5 7,8 ) Range of Phanerozoic values ( ref . 12 ) Age ( 109 years ) Fig . 1. The CDB values of organic carbon in sedimentary rocks . HOOGGENOEG Fm . A and ...
... determined in this study ( ref . 14 ) Previously published values ( refs . 2-5 7,8 ) Range of Phanerozoic values ( ref . 12 ) Age ( 109 years ) Fig . 1. The CDB values of organic carbon in sedimentary rocks . HOOGGENOEG Fm . A and ...
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