1) low-velocity-and-high-conduction layer in mid-crust
中地壳低速高导体
2) Low velocity and high conductive layer of mid-crust
中地壳低速高导层
3) 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。
4) Lower velocity-high electrical conductivity reservoirs
低速-高导体
5) Low velocity layer in the middle crust
中地壳低速层
6) Crustal lower-velocity layers
地壳低速层
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