Send mail to Author

The chemical evolution from older (323–318 Ma) towards younger highly evolved tin granites (315–314 Ma)—sources and metal enrichment in variscan granites of the western Erzgebirge (central european variscides, Germany) (Article)

Please indicate your contact information and select, which author you want to contact.



 
  _____     _____    __   _    __   __   __   _    _    _   
 / ____||  |  ___|| | || | ||  \ \\/ // | || | || | || | || 
/ //---`'  | ||__   | '--' ||   \ ` //  | '--' || | || | || 
\ \\___    | ||__   | .--. ||    | ||   | .--. || | \\_/ || 
 \_____||  |_____|| |_|| |_||    |_||   |_|| |_||  \____//  
  `----`   `-----`  `-`  `-`     `-`'   `-`  `-`    `---`
 


Back to frontdoor view

OPUS4 Logo