前言 风成城地区自风3井在石炭系地层获工业性高产油流以来,对该地区出油层组的沉积相研究,一直为广大地质工作者所关注。在1982年《新疆石油地质》第3期,刘敬奎、赵白同志就《风城地区中、上石炭统储层特征初步探讨》一文中,将风城组碳酸盐岩取芯井段所代表的沉积环境定为泻湖相或封闭的陆表海湾相沉积。本文试图采用萨胡判别 Preface The study on the sedimentary facies of the oil-bearing formation in this area has been of concern to the general geological workers since the wind-chengcheng self-wind 3 well obtained the industrial high-yield oil flow in the Carboniferous strata. In 1982, Xinjiang Petroleum Geology No. 3, Liu Jingkui, Zhao Baogong on “Fengcheng area, the Upper Carboniferous reservoir characteristics of a preliminary discussion,” the paper, The sedimentary environment is defined as a lagoon facies or a closed terrestrial Gulf deposition. This article attempts to use Sahu discrimination