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目前在青藏高原使用的古高程定量恢复的方法有:氧同位素古高程计(包含热动力学模型和经验模型)、△47古温度—古高程计、氢同位素古高程计、古植物古高程计(包含共存分析法、叶相分析法)和古环境分析。详细分析了各古高程计的原理、应用条件、影响因素和优缺点,进一步总结了各种研究方法取得的成果和存在的问题,探讨了各研究方法在青藏高原定量古高程研究方向的应用潜力和发展前景,并对完善现有的古高程计和今后开发新的古高程计提出相关建议。
At present, the methods of quantitative recovery of paleo-elevations used in the Qinghai-Tibet Plateau are as follows: the ancient isotopes (including the thermodynamic models and empirical models), the ancient paleosols of △ 47, the ancient isotopes of ancient isotopes, (Including coexistence analysis, leaf phase analysis) and paleoenvironmental analysis. The principle, application conditions, influencing factors, advantages and disadvantages of each ancient altimeter were analyzed in detail. The achievements and existing problems of various research methods were further summarized, and the potential of each research method in the quantitative paleo-elevation research of the Qinghai-Tibet Plateau And development prospects, and make recommendations on improving the existing ancient altimeter and the future development of new ancient altimeter.