超基性岩侵入于白垩系红色盆地中，主要有玻基辉橄岩、角砾状玻基辉橄岩等。
They are mainly limburgite and breccia like limburgite and intruded the Cretaceous red basins.
四川盆地西部侏罗系沙溪庙组是河流—三角洲—滨浅湖沉积为主的红色砂泥岩系，天然气资源相当丰富。
Abundant in natural gas sources, Jurassic Shaximiao Formation in west Sichuan Basin is a red sandstone and shale mainly deposited in fluvial, deltaic shoal faces.
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（金岭寺-羊山）盆地土城子组为一套红色陆相碎屑岩组合。
The Tuchengzi formation in Jinlingsi-Yangshan basin, Western Liaoning Province is composed of a series of red continental detrital rocks.
四川盆地是中国白垩纪最具代表性的陆相沉积盆地之一，主要发育一套广布的红色碎屑岩沉积，且膏盐、沙漠相沉积发育。
The Sichuan Basin is one of the most representative basins in Cretaceous terrestrial basin, in which a suite of red clastic deposition, especially gypsum and desert facies had been widely deposited.
四川盆地是中国白垩纪最具代表性的陆相沉积盆地之一，主要发育一套广布的红色碎屑岩沉积，且膏盐、沙漠相沉积发育。
The Sichuan Basin is one of the most representative basins in Cretaceous terrestrial basin, in which a suite of red clastic deposition, especially gypsum and desert facies had been widely deposited.
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