机译:东太平洋崛起的异质地幔熔融和岩浆工艺(2.6-3.1摄氏度):来自中海脊玄武岩地球化学和SR-ND-PB同位素的证据
Minist Nat Resources Inst Oceanog 2 State Ocean Adm Key Lab Submarine Geosci Hangzhou 310012 Zhejiang Peoples R China;
Minist Nat Resources Inst Oceanog 2 State Ocean Adm Key Lab Submarine Geosci Hangzhou 310012 Zhejiang Peoples R China;
Minist Nat Resources Inst Oceanog 2 State Ocean Adm Key Lab Submarine Geosci Hangzhou 310012 Zhejiang Peoples R China;
Minist Nat Resources Inst Oceanog 2 State Ocean Adm Key Lab Submarine Geosci Hangzhou 310012 Zhejiang Peoples R China;
Minist Nat Resources Inst Oceanog 2 State Ocean Adm Key Lab Submarine Geosci Hangzhou 310012 Zhejiang Peoples R China;
East Pacific Rise; mantle heterogeneity; magmatic process; mid-ocean ridge basalts; Sr-Nd-Pb isotopes;
机译:东太平洋崛起的异质地幔熔融和岩浆工艺(2.6-3.1摄氏度):来自中海脊玄武岩地球化学和SR-ND-PB同位素的证据
机译:异质地幔的流动和融化:1.方法和对海洋岛屿和中海脊玄武岩地球化学的重要性
机译:富型中洋脊玄武岩的成因是远离地幔柱的山脊:东太平洋上升,北纬11度20分钟
机译:东太平洋北部崛起下方的极端地幔源异质性 - 来自近岭海山的痕量元素证据
机译:海洋中脊的岩浆过程:来自印度洋东南部,胡安·德富卡岭的奋进段和东太平洋北部北部的熔岩和熔体包裹体的证据。
机译:铁同位素分馏在海洋脊髓崎(Morb)演变中:来自熔岩在东太平洋上涨10°30'n的证据及其含义
机译:东太平洋上升近21度N,13度N和20度s:中海脊轴向过程沿线变化的推论