fluxoturbidite

基本解释

Seismicity can damage the stability of delta front and form liquefied fluxoturbidite and faulted fluxoturbidite.
其中地震作用可以破坏三角洲前缘的稳定性，形成液化滑塌浊积体和断阶滑塌浊积体。
In contrast , the regular and good reserved delta front is disadvantaged to form fluxoturbidite.
相反,形态规则、保存完好的三角洲前缘反而不利于滑塌浊积岩的形成。
The fluxoturbidite in front of delta is an important kind of lithologic hydrocarbon reservoirs in fault basins.
摘要三角洲前缘滑塌浊积体是断陷盆地内一类重要的岩性油气藏。
According to interior flume experiment simulations, the formation of fluxoturbidite in front of delta is studied under different conditions.
通过室内水槽实验模拟了不同条件下三角洲前缘滑塌浊积体的形成过程。
Without external mechanisms the sands in inlet of main stem can compact and descent to underneath mudstone and form fluxoturbidite.
无外界触发机制作用下主河道入水口处的砂体在重力作用下向下部泥岩压实沉陷，也可形成滑塌浊积体。