1) menber 1 of Xishanyao formation
西山窑组一段
2) member 1 of Shanxi Formation
山西组一段
1.
Previous studiesdrew different conclusionsafter studying the depositionalenvironmentalof member 1 of Shanxi Formation during the evolution.
在这一演化过程中山西组一段沉积环境前人研究后得出了不同的结论,有的认为属于陆相湖泊三角洲沉积,有的认为是海陆过渡三角洲沉积,还有的认为是湖泊三角洲,但受到间歇性海侵影响。
3) Xishanyao Formation
西山窑组
1.
Characteristics of unconformity between the Xishanyao Formation and Toutunhe Formation of Middle Jurassic in Junggar Basin and its significance in petroleum exploration;
准噶尔盆地中侏罗统西山窑组与头屯河组间不整合面特征及其油气勘探意义
2.
Stress field and fractures distribution characteristics of the reservoir of Xishanyao formation in wellblock Cai 9 in Cainan oil field;
彩南油田彩9井区西山窑组油藏应力场及裂缝分布特征
3.
Geological Estimation of Denuded Strata Comeback of Xishanyao Formation in Junggar Basin;
地质学方法估算准噶尔盆地西山窑组剥蚀厚度
6) Shan 2 member
山西组2段
1.
Permian Shan 2 member sandstone is the main reservoir,and the diagenesis process of the member was complicated.
榆林气田是鄂尔多斯盆地的重要气田之一,其主力储层为下二叠统山西组2段砂体,但该套砂体的成岩演化过程复杂,受控因素很多,给勘探带来较大困难。
补充资料:西山窑
西山窑 古代瓷窑。在浙江温州西山。东晋时烧制青瓷,胎为灰色和淡土黄色,质较松。釉肥厚,以淡青为主,少细开片。装饰上多在器物内外刻划莲瓣纹,也有青褐加褐彩的。深口宽底高碗为其典型作品。西山窑在唐、五代和宋时,继续烧造青瓷。
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