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太古宙热流参数和可能的岩石圈转化及其形变作用受早期地球大地构造格架控制。它们指示由反映小规模对流通口和冲击热异常的分布无规律的原始岩浆源中心向线形脊状系统的转化。岩石圈消减型式的变化与这个转化过程相协调。由于早期地温梯度陡,榴辉岩难于形成,反映了岩石圈消减的缓倾带占优势。这种情况导致了次生岩浆作用和早期地壳广大地区原始大陆物质的形成。上壳岩平缓做迭瓦构造与原始硅铝物质之间的关系,和在岩石圈消减部位的钙碱性岩浆作用,有助于解释太古宙高级区很多基本特征。假设的弯曲构造结合薄岩石圈硅铝覆盖岩板的水平变形有助于解释低级区的特征。长期的总热流的衰减,意味着在前寒武纪某个时间突然出现了榴辉岩覆盖的下降的具狭窄火山弧陡倾斜消减岩石圈和岩石圈形变振幅/波长比值的减小。
Archean heat flow parameters and possible lithospheric transformations and their deformations are controlled by early Earth tectonics. They indicate the conversion from a linear magma center to a linear magma source that reflects irregular distribution of small anomalies and impact heat anomalies. The changes in lithospheric depletion patterns are coordinated with this transformation. Due to the steep geothermal gradient in the early stage, the eclogite is hard to form, indicating that the dominant dip of the lithosphere is gentle. This situation led to secondary magmatism and the formation of primitive continental material in vast areas of the early crust. The relationship between the upper crust ductile bedding structure and the original Si-Al material and the calc-alkaline magma in the subducted lithosphere are helpful to explain many basic features of the Archean high-rise area. The hypothetical curved structure combined with the horizontal deformation of the thin lithospheric Si-Al covered rock helps to explain the characteristics of the lower zone. Long-term attenuation of the total heat flux means that a sharp reduction in eclogitic cover of sharply narrowed volcanic arcs and a decrease in lithospheric deformation amplitude / wavelength ratio have been observed at some point in the Precambrian.