adj.更熱的；更熱烈的
An alternative theory is that the sinking part of the plate, which is denser than the hotter surrounding mantle, pulls the rest of the plate after it. 另外一個(gè)理論認(rèn)為，板塊的下沉部分，其密度高于更熱的周圍地幔，會(huì)牽拉板塊的其余部分。
