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从热的角度,岩石圈可以定义为以热传导为主的地球外壳,它通常包括地壳和部分地幔。除了那些正在进行构造活动或岩浆活动的地区,这个定义可能描述了几乎所有大陆岩石圈的特征。控制大陆岩石圈热动态的因素很多,其中包括来自软流圈的热流、热传导率和放射性热产生在垂向和横向的变化、构造历史、以及诸如气候变迁史和浅部水热动态等近地表的作
From a thermal point of view, the lithosphere can be defined as a heat conduction-dominated Earth’s crust, which usually includes the crust and part of the mantle. Except for those areas undergoing tectonic or magmatic activity, this definition may describe the characteristics of almost all continental lithosphere. There are many factors that control the thermal dynamics of the continental lithosphere. These include the heat flow from the asthenosphere, thermal conductivity and radiative heat generation in vertical and horizontal variations, tectonic history, and near surface features such as the history of climate change and shallow hydrothermal dynamics Works