Počet záznamů: 1
Two Contrasting Fabric Patterns of Olivine Observed in Garnet and Spinel Peridotite from a Mantle-derived Ultramafic Mass Enclosed in Felsic Granulite, the Moldanubian Zone, Czech Republic
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$a Two Contrasting Fabric Patterns of Olivine Observed in Garnet and Spinel Peridotite from a Mantle-derived Ultramafic Mass Enclosed in Felsic Granulite, the Moldanubian Zone, Czech Republic 215 $a 23 s. $c WWW 463 -1
$1 001 cav_un_epca*0253979 $1 011 $a 0022-3530 $e 1460-2415 $1 200 1 $a Journal of Petrology $v Roč. 51, 1/2 (2010), s. 101-123 $1 210 $c Oxford University Press 610 0-
$a garnet peridotite 610 0-
$a spinel peridotite 610 0-
$a olivine fabrics 610 0-
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$3 cav_un_auth*0259399 $4 070 $a Michibayashi $b K. $y JP 701 -1
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$3 cav_un_auth*0102183 $i Oddělení geologických procesů $j Department of geological processes $w Department of Geological Processes $4 070 $a Svojtka $b Martin $p GLU-S $T Geologický ústav AV ČR, v. v. i. 856 $q pdf soubor
Počet záznamů: 1