Nature, Volume 434 |
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Page 373
We can now consider whether the physical properties of BIFs are consistent with observations of the ULVZs . The high - pressure / hightemperature seismic properties of the high - pressure FeO phases are not known at present , so we ...
We can now consider whether the physical properties of BIFs are consistent with observations of the ULVZs . The high - pressure / hightemperature seismic properties of the high - pressure FeO phases are not known at present , so we ...
Page 580
The estimates of Q for S2 , S3 and S4 are 525 , 405 and 380 , respectively , and are consistent with previously reported values " . 1 As well as the longest - period normalmode multiplets S2 , S3 and S4 , we analysed radial modes S and ...
The estimates of Q for S2 , S3 and S4 are 525 , 405 and 380 , respectively , and are consistent with previously reported values " . 1 As well as the longest - period normalmode multiplets S2 , S3 and S4 , we analysed radial modes S and ...
Page 591
These are consistent with the estimated parental melt compositions , considering that the lavas have been variably fractionated by olivine loss and addition . However , the pre - shield and post - shield lavas have consistently lower Ni ...
These are consistent with the estimated parental melt compositions , considering that the lavas have been variably fractionated by olivine loss and addition . However , the pre - shield and post - shield lavas have consistently lower Ni ...
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Contents
eating at heart p | 37 |
letters to nature | 50 |
Mesozoic Alpine facies deposition as a result | 59 |
16 other sections not shown
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Bibliographic information
| Title | Nature, Volume 434 |
| Editor | Sir Norman Lockyer |
| Publisher | Macmillan Journals Limited, 2005 |
| Original from | University of Illinois at Urbana-Champaign |
| Digitized | 25 Nov 2019 |
| Export Citation | BiBTeX EndNote RefMan |