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在庐山科学考察中 ,新发现乌龙潭岩石表皮构造 .从其地质空间位置、变形特征、应力场状态和动力学机制 ,均表明该表皮构造是由冰川作用所形成的 .运用理论与实践相结合的分析方法 ,论证了庐山第四纪冰川作用发生的可能性 ,对青藏高原在中国东部气候环境变化的作用给予了充分的注意 .
In the scientific investigation of Lushan Mountain, the epidermal structure of the rocks in Wolongtan has been newly discovered, which shows that the epidermis is formed by the action of glaciers from its geological location, deformation features, stress field and dynamical mechanism. , The feasibility of Quaternary glaciation in Lushan Mountain is demonstrated, and sufficient attention is given to the role of the Tibetan Plateau in climate and environmental change in eastern China.