Počet záznamů: 1
Mantle Zn Isotopic Heterogeneity Caused by Melt‐Rock Reaction: Evidence From Fe‐Rich Peridotites and Pyroxenites From the Bohemian Massif, Central Europe
SYS 0505049 LBL 01000a^^22220027750^450 005 20240111141019.8 014 $a 85065211757 $2 SCOPUS 014 $a 000468912000020 $2 WOS 017 $a 10.1029/2018JB017125 $2 DOI 100 $a 20190530d m y slo 03 ba 101 $a eng $d eng 102 $a US 200 1-
$a Mantle Zn Isotopic Heterogeneity Caused by Melt‐Rock Reaction: Evidence From Fe‐Rich Peridotites and Pyroxenites From the Bohemian Massif, Central Europe 215 $a 17 s. $c P 463 -1
$1 001 cav_un_epca*0389084 $1 011 $a 2169-9313 $e 2169-9356 $1 200 1 $a Journal of Geophysical Research-Solid Earth $v Roč. 124, č. 4 (2019), s. 3588-3604 $1 210 $c Wiley 610 $a zinc isotopes 610 $a peridotite 610 $a pyroxenite 610 $a melt‐rock reaction 610 $a mantle heterogeneity 700 -1
$3 cav_un_auth*0064809 $4 070 $a Huang $b J. $y CN 701 -1
$3 cav_un_auth*0203768 $4 070 $a Ackerman $b Lukáš $p GLU-S $i Oddělení geologických procesů $j Department of geological processes $w Department of Geological Processes $T Geologický ústav AV ČR, v. v. i. 701 -1
$3 cav_un_auth*0375552 $4 070 $a Zhang $b X-CH. $y CN 856 $9 RIV $q pdf soubor $u https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2018JB017125
Počet záznamů: 1