The sandstones of the Turpan Basin belong mostly to graywacke and their compositional and textural maturity are generally low,indicating a strong erosional and rapid transportational environment.
吐-哈盆地
砂岩主要属杂砂岩
，
结构成熟度和成分成熟度均较低，形成于强烈剥蚀、快
搬运沉积环境中。
The sandstones of the Turpan Basin belong mostly to graywacke and their compositional and textural maturity are generally low,indicating a strong erosional and rapid transportational environment.
吐-哈盆地砂岩主要属杂砂岩，结构成熟度和成分成熟度均较低，形成于强烈剥蚀、快搬运沉积环境中。
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