高压—超高压变质岩的成岩深度: 争论及评述
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Forming Depth of High Pressure—Ultrahigh Pressure Metamorphic Rocks: A Review
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  • 中国地质科学院地质力学研究所,北京,100081    
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    摘要:

    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。

    Abstract:

    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.

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武红岭.2011.高压—超高压变质岩的成岩深度: 争论及评述[J].地质论评,57(4):555-564,[DOI].
.2011. Forming Depth of High Pressure—Ultrahigh Pressure Metamorphic Rocks: A Review[J]. Geological Review,57(4):555-564.

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