高岭石、大部分菱铁矿、黄铁矿、硅质自生矿物及少部分方解石反映了陆相环境。
Kaolinite, a number of siderites, pyrites, siliceous authigenic minerals and a few calcites represent continental environment.
中国油页岩具有沉积时代以新生代为主，沉积环境以陆相为主的特征。
Oil shale of China has its own characters that mostly deposits in the Cenozoic and was formed in continental environment.
陆相断陷盆地具有特定的沉积环境。
Continental faulted basins formed in specific depositional environment.
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