对晚侏罗世漠河盆地的沉积特征进行了分析，并探讨了其构造类型和成因机制。
The authors deals with the sedimentary characteristics of the Late Jurassic Mohe basin, and studies its tectonic type and genetic mechanism.
根据基底性质分析，探讨了东海大陆边缘新生代沉积盆地的形成演化与成因机制。
Along the continental margin in East China Sea, the origin and evolution of Tertiary sedimentary basins are discussed, based on analyses of basement nature.
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