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关于沉积盆地的分类按照形成机制分拗陷型和断陷型两类。在这两类盆地中,以断陷型盆地比较常见。断陷型盆地还可依据应力性质进一步划分为张性盆地和压性盆地两种。一、青藏高原陆相第三系盆地的发育特征 1.分布规律
The classification of sedimentary basins is divided into two types according to the forming mechanism: sub-sag and subsidence. In both types of basins, faulted basins are more common. Fault-depression basins can be further divided into two types of extensional basins and pressure basins according to the stress properties. First, the Qinghai-Tibet Plateau terrigenous Tertiary Basin development characteristics 1. Distribution