Tectono - sedimentary evolution of the basin may be divided into three stages: continentalmargin rift, back-arc rift, and depression basin.
其沉积—构造演化可划分为三个阶段:大陆边缘裂谷、后裂谷和拗陷盆地。
2
Tectono -sedimentary evolution of the basin may be divided into three stages: continentalmargin rift, back-arc rift, and depression basin.
其沉积—构造演化可划分为三个阶段:大陆边缘裂谷、弧后裂谷和拗陷盆地。
3
The geochemistry of the cherts reflects that the cherts coexisting with island-arc volcanic rocks all formed the background of continentalmargin basin.