cm 0cm 0pt" class=MsoNormal>ce="Times New Roman">///The terms of low-SlOe adakite cii-font-family: ’Times New Roman’; mso-hansi-font-family: ’Times New Roman’">(ce="Times New Roman">LSA, SlOe cii-font-family: ’Times New Roman’; mso-hansi-font-family: ’Times New Roman’">〈ce="Times New Roman"> 60% cii-font-family: ’Times New Roman’; mso-hansi-font-family: ’Times New Roman’">)ce="Times New Roman"> and high-SlOe adakite cii-font-family: ’Times New Roman’; mso-hansi-font-family: ’Times New Roman’">(ce="Times New Roman">HSA, SlOe cii-font-family: ’Times New Roman’; mso-hansi-font-family: ’Times New Roman’">〉ce="Times New Roman"> 60% cii-font-family: ’Times New Roman’; mso-hansi-font-family: ’Times New Roman’">)ce="Times New Roman"> were put forward by Martin et al. cii-font-family: ’Times New Roman’; mso-hansi-font-family: ’Times New Roman’">(ce="Times New Roman">2005cii-font-family: ’Times New Roman’; mso-hansi-font-family: ’Times New Roman’">)ce="Times New Roman">. This paper does not agree with this classification, because the low-SlOe adakite is sanukite rather than adakite. Sanukite is a mantle source rock, whereas adakite is a crust-derived rock. Although adakite can be mixed with the mantle to form high-Mg adakite, it is still of the crust source. Crust- and mantle-derived magmas are different types of magma, so it is not proper to confuse them.