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结合现代火山岛弧资料的模拟 ,受孕地幔熔融模型的应用成果可概括为以下几点 :与活动陆缘之弧后盆地伴生的洋内弧主要派生自亏损的受孕的大洋中脊玄武岩地幔 (fertile MORB mantle,简称 F MM) ,它在早期熔融事件中已丢失了 3%的熔体 ;亏损发生在尖晶石二辉橄榄岩相中 ,它支持把它与弧后盆地熔融事件相联系的模型 ;与弧后盆地不伴生的大洋岛弧主要派生自FMM,不过富集岩浆源在局部可能起重要作用 ;内陆弧一般派生自富集地幔 ,可能是因为有陆下岩石圈混入 ;在薄层地壳上的洋内弧中 ,熔融程度可能很高 (约 2 5 %～ 30 % ) ,而在岩石圈较厚的地区熔融量则减至 15 %或更少 ;挥发分加入到地幔中诱发的熔融约占 10 % ,余者则是由减压作用所引起的。
Based on the simulation of modern volcanic island arc data, the application results of the fused mantle model for conception can be summarized as follows: The intracavity arc associated with the arc-back basin of the active continental margin is mainly derived from the depleted mantle of fertile mid-oceanic ridges (fertile MORB mantle, FMM for short), which lost 3% of the melt in the early melting event; the loss occurred in the spinel lherzolite facies, which supported the model linking it to the melting event in the backarc basin; and The unconforming oceanic arc in the backarc basin is mainly derived from the FMM, but enriched magma source may play an important role locally. The inland arc generally derives from enrichment of the mantle probably due to the intrusion of subterranean lithosphere. In the thin crust , The melting degree may be high (about 25% ~ 30%) in the intracrystalline arc, while the melting amount is reduced to 15% or less in the thicker lithosphere; the volatility is added to the induced melting in the mantle About 10%, while the rest are caused by the role of decompression.