Middle-Late Ordovician iron-rich nodules on Yangtze Platform, South China, and their palaeoenvironmental implications
Xiaocong Luan Artikkel Engelsk
*0011288702 *008190716s2018 xx# 000 0 eng *019 $bk *08230$a560.45 *100 $aLuan, Xiaocong$4aut$_151102800 *245 $aMiddle-Late Ordovician iron-rich nodules on Yangtze Platform, South China, and their palaeoenvironmental implications *300 $aS. [523]-537 : ill. *500 $aVitenskapelig artikkel *650 $aJern$2norart$_14004400 *650 $aPaleoøkologi$2norart$_55605100 *650 $anoduler$9nor$2norart$_151102900 *651 $aYangtze (Kina)$_151103000 *653 $aGreat Ordovician Biodiversification Event$9eng$_150027300 *653 $acoated grain$9eng$_151103100 *653 $amicrofacies analysis$9eng$_151103200 *653 $aoncoid$9eng$_151103300 *653 $ared nodules$9eng$_151103400 *700 $aBrett, Carlton E.;$4aut$_135133600 *700 $aGong, Fangyi$4aut$_151103500 *700 $aJin, Jisuo;$4aut$_151103600 *700 $aWu, Rongchang;$4aut$_151103700 *700 $aZhan, Renbin;$4aut$_142725300 *773 $tLethaia$gVol. 51, no. 4 (2018)$x0024-1164$w(NO-LaBS)5212(tnr) *8564 $uhttps://doi.org/10.1111/let.12271 *999 $z1900643137$anorart:1900643137 ^