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高压—超高压变质岩的成岩深度:争论及评述

             

摘要

The rock-forming depth of high pressure-ultra-high pressure metamorphic rocks has been studied and debated for a long time. Writer tries to do some review and comments for it and gives some views and suggestions in this paper. Writer is in the opinion that ①the view that UHP rocks are formed in crust depth may be more reasonable, because of existence of the tectonic additional pressure; ②the method for calculating rock-forming depth should be improved in theory and practical use; ③up to now there is no sufficient evidence to refute the view that UHP rocks are formed in mantle depth owing to the continental subduction;and ④geologists with different views should pay more attention to reasonable parts of dissenters'academic ideas to develop the research in this field by cooperation each other.%有关高压、超高压岩石的成岩深度的争论由来已久,本文对此进行了较全面、详实的回顾、介绍和评述;结合自己的研究心得.作者提出了几点认识和建议,供争论的双方参考或做进一步的争辩:①因为有构造压力的存在,超高压变质岩壳内成因观点更合理;②成岩深度的测算方法需要在理论和实际应用中改进和完善;③不应完全否定基于静岩压力的大陆深俯冲机制;④建议争论双方相互吸收对方观点中的合理成分,联手开展相关研究.

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