元古宙后弧扩张的理论探讨--《国外前寒武纪地质》1988年01期

排行榜 收藏 打印 发给朋友 举报 来源: 《地质调查与研究》 发布者:cjk3d
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【摘要】:正 早元古地球也许要比现代有一个更热的地幔和一个大洋板块表面上更少滞留的时间。该更热的地幔可能导致变成更薄的大洋板块。年青的洋底具有低负浮力,因此消减带会产生低的拉动板片力。如果板块越薄,其影响就越大,因为当它们下沉到地幔时热

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C6F|z e,rto;j;S0早元古地球也许要比现代有一个更热的地慢和一个大洋板块表面上更少滞留的时间。该更热的地慢可能导致变成更薄的大洋板块。年青的洋底具有低负浮力,因此消减带会产生低的拉动板片力。如果板块越薄,其影响就越大,因为当它们下沉到地慢时热得更快。因而板片的负浮力和拉动板片

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