1) low-velocity and high-conduction zone
低速高导体
1.
The tectonic characters of deep layer and high abnormal thermal-flow of Songliao Basin show that the crust low-velocity and high-conduction zone in the deep layer of Songliao Basin may be the magma chamber accumulated in the mid or lower crust and produced from the partly melting inside mantle under the interaction of crust and mantle.
根据松辽盆地深部地质结构、异常高的热流值等特征,认为对松辽盆地深层的壳内低速高导体可以有两种解释:①上地幔发生部分熔融,析离出来的流体相在静压力作用之下上升并穿过莫霍面后,在下地壳上部或中地壳内聚集而成的岩浆房;②在缺水条件下,高热流值作用形成的壳内熔融体。
2) Lower velocity-high electrical conductivity reservoirs
低速-高导体
3) low-velocity-and-high-conduction layer in mid-crust
中地壳低速高导体
4) high-conductivity and low-velocity layer
高导低速层
1.
The results show that a high-conductivity and low-velocity layer of the earth′s crust is detected in the Beishan area,with the depth of more than 30 km.
研究结果显示,北山地区30 km以下的下地壳中存在着高导低速层,附近地区历史上曾发生过多次大地震,是一个相对不稳定地块。
5) low velocity-high conductive layer
低速-高导层
6) Low velocity and high conductive layer of mid-crust
中地壳低速高导层
补充资料：半导体导电性(见半导体的导电与电荷输运)
半导体导电性(见半导体的导电与电荷输运)
electrical conductivity of semiconductor
半导体导电性eleetr、ea一conou以，v:‘，_‘ 一J一“。，瓜米早伙鼓幕由乌教着给话_
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条