壳内局部熔融则来源于板块俯冲、地壳增厚产生的热而非幔源侵入所造成。
The partial melting is caused by the heat derived from subduction and crust shortening rather than by the mantle material intrusion.
对中国东部侏罗纪时期地壳增厚和岩石圈显著变薄的现象，提出一个新的形成机制假说。
A new hypothesis for explaining crustal thickening and significant lithospheric thinning in the Jurassic in eastern China is proposed.
是麻粒岩相变质作用发生于地壳大幅度增厚的环境，强烈的构造变动和区域性高热流共同作用的结果。
The above shows that granulite facies metamorphism occurred in the crust of (increasing) thickness and caused by strong tectonic disturbance and regional high heat flow.
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