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pro vyhledávání: '"B. N. Pisakin"'
Publikováno v:
Mathematical Geology. 35:381-398
A principal feature of stratiform basic-ultrabasic intrusions is alternation of rocks characterized by different proportions of the salic (plagioclase) and mafic (mainly pyroxene) constituents. Owing to considerable density variation of the component
Publikováno v:
Geophysical Journal International. 137:691-712
The palaeomagnetic data that are available for the eastern Fennoscandian Shield are too sparse to allow any palaeomagnetic constraints to be determined for intracratonic horizontal movements in this part of the shield. To address this issue we have o
Publikováno v:
Mathematical Geology; May2003, Vol. 35 Issue 4, p381-398, 18p