中国中生代到新生代初期主要在热带或亚热带干旱环境下沉积的陆相红色砂岩、砾岩和页岩所组成的红色地层。主要堆积于中生代燕山期造山运动所形成的断陷盆地中，故其分布区常被称为“红层盆地”（或红盆地）
长(沙)—平(江)白垩系红层盆地，公认为贫水地区。
It is well known that Changsha Pingjiang basin of Cretaceous red strata is an area short of water.
火山岩岩浆的形成既与古特提斯洋的俯冲洋壳在深部脱水有关，又与南澜沧江带红层盆地形成初期的拉张作用有关，为山—盆转化阶段特殊岩浆类型。
The origination of the magma is related with the dehydration of the subducting plate of the Palezoic Tethy Sea and the early tension of the form of the Lancangjiang belt red layer basin.
运用露头层序地层学原理及沉积体系分析方法，对随州盆地晚白垩世“红层”进行了层序地层学的研究。
Applying sequence stratigraphy principle and sedimentary system analysis, the "red beds" in Upper Cretaceous Epoch in Suizhou basin has been studied on sequence stratigraphy.
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