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.
浙江金衢盆地白垩系红层，共发现二个化石孢粉组合。
Two fossil spore-pollen assemblages are found in the Cretaceous red beds of Jin Ju Basin, Chekiang Province.
南雄红层是指位于南雄盆地的红色岩层，长约80公里，宽18公里，面积约1500平方公里。
Nanxiong red layer is located in the red rock Nanxiong Basin, about 80 kilometers wide and 18 km, an area of about 1500 square kilometers.
辽西金羊盆地南部陆相红层土城子组较为发育，其沉积物具明显旋回性。
In the south of Jinlinsi Yangshan basin of West Liaoning, continental red beds of Tuchengzi F. developed well with obvious cyclic features.
辽西金羊盆地南部陆相红层土城子组较为发育，其沉积物具明显旋回性。
In the south of Jinlinsi Yangshan basin of West Liaoning, continental red beds of Tuchengzi F. developed well with obvious cyclic features.
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