摘要
Plenty of geochemical analyses were carried out on natural gas, oil and condensate samplescollected from two wells in Tarim Basin and results were employed in interpreting their sources and distin-guishing one from the other. The chemical compositions of gases from the both wells showed that they are ofoilfied associated gas with a low dry coeffieient. Their carbon isotopic compositions might indicate a mixture ofgas sources, and the input of the mantle-derived materials was denied by the isotopic parameters of noble gas-es, such as 3He/4He and 4He/20Ne ratios. The age of gases from these two wells was identified to be thePalaeozoic by the 40Ar/36Ar ratio.