Liu, Wei <br/><br/>
Two disequilibrium quartz feldspar 18O/16O fractionations within the Aral granite batholithm Altay mountains of China: evidence for occurrence of two stages of O and H isotopic exchange of a heterogeneous granite system with aqueous fluids 

 - Oxford  Oxford University Press  September 2000 
 - pp. 1455-1466  ilus., map., tbls. 
<br/><br/><label>ISSN: </label>0022-3530 
<br/><br/><label>Subjects--Topical Terms: </label><br/>CUARZO<br/>FELDESPATO<br/>GRANITOS<br/>ISOTOPOS DE HIDROGENO<br/>ISOTOPOS DE OXIGENO<br/>PSEUDOISOTERMA
<br/><br/><label>Subjects--Geographic Terms: </label><br/>ALTAY<br/>CHINA