Earth's core and the part of mantle under the lithosphere is the inner background of ESL and the astrospace outside atmosphere is its outer surroundings.
岩石圈以下的地幔和地核与大气圈以外的宇宙空间均为地球表层的环境。
The orogenic types were controlled by the relative motion mechanism between lithosphere and asthenosphere.
板块和软流圈之间不同的相对运动机制是形成不同类型造山作用的主要原因.
Geological characteristics at their locations show continuous or pulsive westward slipping of lithosphere convection cell.
它们产出的地质特征表明,岩石圈相对地幔对流体,持续或幕式地向西滑移.
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