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  1. .... Chemically, Earth can be divided into the crust , upper mantle, lower mantle, outer core, and inner core. The geologic component ...

  2. ...core-古騰堡介面gutenberg discontinuity-下地幔lower mantle-岩流圈asthenosphere-上地幔 upper mantle-莫氏介面mohorovicic discontinuity-地核earth s  crust .岩流層的似核分裂與消耗當然是會想到熱散冷卻後的地球內體變化.會是空虛...

  3. 火山底部岩漿庫的最深處估計是深到地球的地函外層( upper mental、上地幔),距地表深度35–60公里。軟流圈深度...upload.wikimedia.org/wikipedia/commons/b/b5/Earth- crust -cutaway-chinese.png http://www.nms.ac.uk/images...

  4. ...(硫):  N/A Oceanic crust (海洋地殼)--Element(元素)及比重: Oxygen...鎳):  0.014 Sulfur(硫):  N/A Upper mantle(地函)--Element(元素)及比重: Oxygen...