Please go through following reference. I hope it may be helpful to you.
Petrology and Geochemistry of Adakitic Dacites and High-MgO Andesites, and Related Calc-alkaline Dacites from the Miocene Okoppe Volcanic Field, N Hokkaido, Japan
M. Ayabe1,
K. Takanashi2,
K. Shuto3,*,
H. Ishimoto4 and
H. Kawabata5
+Author Affiliations
1Sezax Co., Ltd., 3-19-1 Shibuya, Shibuya-Ku, Tokyo 150-0002, Japan
2Graduate School of Science and Technology, Niigata University, 2-8050 Ikarashi, Nishi-Ku, Niigata 950-2181, Japan
3Institute of Science and Technology, Niigata University, 2-8050 Ikarashi, Nishi-Ku, Niigata 950-2181, Japan
4Exploration Section, Technical Department Itochu Oil Exploration Co., Ltd., 2-5-1 Kita-Aoyama, Minato-Ku, Tokyo 107-0061, Japan
5Institute for Frontier Research on Earth Evolution (Ifree), Japan Agency for Marine–Earth Science and Technology (Jamstec), Yokosuka 237-0061, Japan
Usually, the partial melting of subducted oceanic crust can produce adakites which have Mg# = ~50 or higher. Moreover, the melts can be given more magnesium component when they interact with the overlying mantle wedge during their ascent to surface.
Yes, there are many papers about it. Normaly, the origin of High-Mgo adakites is partial melting of metasomatized mantle source above of young subduction zones.
There is a version that adakite felsic rocks are formed by of a mantle wedge melting (Macpherson et al., 2006).
Macpherson, C.G., Dreher, S.T., Thirlwall, M.F., 2006, Adakites without slab melting: High pressure differentiation of island arc magma, Mindanao, the Philippines: Earth and Planetary Science Letters, v. 243, p. 581–593.