这阶段的观点主要认为是瑞利-泰勒不稳定性（Rayleigh-Taylor instability）导致了盐构 造的产生，即拥有微小抗屈强度(yield strength)密度流的上覆岩层沉入低密度流的盐层，替 换了它并向上流动。
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双层喷气负载作为减小瑞利-泰勒不稳定性的重要手段，在Z箍缩实验中得到广泛应用。
The double shell gas puff is applied extensively in Z pinch experiments because it can reduce R-T instability during the implosion phase.
发现了横向电子热传导烧蚀在长波长扰动的非线性瑞利·泰勒不稳定性演变中起重要作用。
It is discovered that lateral ablation of electron conduction plays an important role in nonlinear evolution of the Rayleigh-Taylor instability with a longer wavelength.
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