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Стр. 819
It has not been observed in other crust at the oceanic ridges during seain continental crust that may be of the regions of the oceanic crust that we floor spreading : ( i ) volcanism , particorder of several kilometers thick .
It has not been observed in other crust at the oceanic ridges during seain continental crust that may be of the regions of the oceanic crust that we floor spreading : ( i ) volcanism , particorder of several kilometers thick .
Стр. 1085
The first limit corresponds to equality If the magmatic injection component of integrated radiogenic sources between of sea floor spreading initiates at depths average oceanic and continental secshallower than the interval considered ...
The first limit corresponds to equality If the magmatic injection component of integrated radiogenic sources between of sea floor spreading initiates at depths average oceanic and continental secshallower than the interval considered ...
Стр. 1087
The range of possible time conis the oceanic gradient normalized to a These intervals are related by magmatic stants for heat transfer in the earth do not permit an unambiguous distinction between basaltic surface composition and ...
The range of possible time conis the oceanic gradient normalized to a These intervals are related by magmatic stants for heat transfer in the earth do not permit an unambiguous distinction between basaltic surface composition and ...
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acid action activity addition American amount animals antigens appears application associated average blood cause cells changes Chem chemical complete concentration containing culture Department determined effect electron elements energy enzyme example experiments field formation function give given heat human illus increase indicate Institute laboratory less logical lower major material mean measured mechanism membrane ment method minutes nature normal Notes observed obtained occur oceanic organisms percent physics plants position possible preparation present Press problem produced protein range rats reactions recent References relative reported response sample Science similar single solution specific structure suggested surface Table temperature tion units University weight York