117,443 research outputs found
(Table 37) Chemical composition of olivines and pyroxenes from ultrabasic rocks of the Mariana Trench
Analyses have been carried out by Yu.G. Lavrentjev and N.L. Dobretsov at the participation of G.N. Savelyeva
(Table 41) Chemical composition of chrome-spinellids from ultrabasic rocks of the Yap Fault and Yap Trench
Analyses have been carried out by Yu.G. Lavrentjev and N.L. Dobretsov at the participation of G.N. Savelyeva
(Table 34) Chemical composition of minerals from ophiolite gabbro of the Yap Trench
Analyses have been carried out by Yu.G. Lavrentjev and N.L. Dobretsov at the participation of G.N. Savelyeva
(Table 35) Chemical composition of minerals from amphibole gabbro in breccia of the Yap Trench
Analyses have been carried out by Yu.G. Lavrentjev and N.L. Dobretsov at the participation of G.N. Savelyeva
(Table 52) K-Ar age of amphibolite, gabbro, and diabase from ophiolite associations of the western Philippine Sea
Analyses have been carried out by Yu.G. Lavrentjev and N.L. Dobretsov at the participation of G.N. Savelyeva
(Table 46) Chemical composition of amphibolites from the Yap Trench
Analyses have been carried out by Yu.G. Lavrentjev and N.L. Dobretsov at the participation of G.N. Savelyeva
(Table 39) Chemical composition of serpentines and chlorites from ultrabasic rocks of the Mariana Trench and Yap Trench
Analyses have been carried out by Yu.G. Lavrentjev and N.L. Dobretsov at the participation of G.N. Savelyeva
(Table 42) Chemical composition of amphiboles from serpentinite of the Yan Trench
Analyses have been carried out by Yu.G. Lavrentjev and N.L. Dobretsov at the participation of G.N. Savelyeva
(Table 29) Chemical composition of typical ore mineral grains from heavy fraction of breccia from the Yap Trench
Analyses have been carried out by Yu.G. Lavrentjev and N.L. Dobretsov at the participation of G.N. Savelyeva
(Table 47) Chemical composition of minerals in horblendites, amphibolites, and amphibolite schists from the Yap Trench
Analyses have been carried out by Yu.G. Lavrentjev and N.L. Dobretsov at the participation of G.N. Savelyeva
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