兰州马衔山北缘断裂带为一条全新世活动断裂，大致由4条次级断裂段组成。

The northern margin fault zone of Maxian Mt. in Lanzhou area is a Holocene active fault which includes about 4 secondary fault segments.

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本文采用非平衡态热力学理论，研究兰州马衔山深季节冻土区的森林生态系统，从研究森林演替入手得出生态环境演变的规律。

In this paper, a theory of non-equilibrium thermodynamics is applied to the ecologic system offorest in zone of deep seasonal frozen soil on Mt. Maxian.

youdao

本文采用非平衡态热力学理论，研究兰州马衔山深季节冻土区的森林生态系统，从研究森林演替入手得出生态环境演变的规律。

In this paper, a theory of non-equilibrium thermodynamics is applied to the ecologic system offorest in zone of deep seasonal frozen soil on Mt. Maxian.

youdao