marginal sea basin

基本解釋

The East China Sea Shelf Basin is a marginal sea basin located on Continental crust of China eastern margin.
東海陸架盆地是位于中國(guó)大陸東部邊緣大陸地殼之上的邊緣海盆地。
During Middle Triassic, the Gejiu area was in a special sedimental environment, i. e. in a restricted marginal sea basin within the continental rift system.
中三疊世，個(gè)舊礦區(qū)處于特殊的沉積環(huán)境—陸裂谷系中的局限邊緣海盆。
The first was in the basin subsidence stage that was prior to the Caledonian movement. The second took place in the marginal sea deposition stage after the Caledonian movement.
區(qū)內(nèi)下古生界烴源巖經(jīng)歷了兩次成油過(guò)程，第一次發(fā)生在加里東運(yùn)動(dòng)前的盆地沉降階段，第二次發(fā)生在加里東運(yùn)動(dòng)后晚古生代陸表海沉積階段。