Rare earth elements as indicators of hydrothermal processes within the East Scotia subduction zone system
Rare earth elements as indicators of hydrothermal processes within the East Scotia subduction zone system
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DOI：
10.1016/j.gca.2014.05.018
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发表时间：
2014-09-01
影响因子：
5
通讯作者：
Hathorne, Ed C.
中科院分区：
文献类型：
--
作者：
Cole, Catherine S.;James, Rachael H.;Hathorne, Ed C.
东斯科舍俯冲带位于南大洋大西洋部分，在弧后和岛弧环境中有许多热液场所。在东斯科舍弧后扩张脊E2和E9段沿着的三个地点，对高温（>348摄氏度）“黑烟”喷口进行了取样，并对“白色烟”（
The East Scotia subduction zone, located in the Atlantic sector of the Southern Ocean, hosts a number of hydrothermal sites in both back-arc and island-arc settings. High temperature (>348 degrees C) 'black smoker' vents have been sampled at three locations along segments E2 and E9 of the East Scotia back-arc spreading ridge, as well as 'white smoker' (