Geological charact eristics at their locations show continuous or pulsive westward slipping of lith osphere with respect to convection cell.
它们产出的地质特

,岩石圈
地幔

,持续或幕式地向西滑移。
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Almost all the large sediment hosted deposits in that mineral blessed country are located not in areas of thick lithosphere but rather near the junctions between thick and thin areas Such junctions often mark the edges of crayons.
几乎所有的大型沉积矿床都位于该矿物丰富的国家的厚
圈区域与薄
圈区域的交界处,而不是
厚
圈区域内。这样的交界处通常标志着克拉通的边缘。