Reconstruction of paleo river systems and distribution of sedimentary facies of Shanxi and lower Shihezi formations in southern Ordos basin

Chao-yong WANG , Ze-cheng WANG , Ji-lin WANG , Yuan BAO , Xiu-mei HU
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引用次数: 11

Abstract

The study area is located in the south of Huanxian county, in Yan'an and Puxian counties and to the north of Xi'an. The Shanxi and lower Shihezi formations are important gas-bearing formations. Given our analysis of the direction of rivers, the contents of stable heavy minerals and of feldspar of palaeo river systems, the study area is divided into six palaeodrainage patterns corresponding to six feldspar regions and six sedimentary facies regions. On this basis, the distribution of sedimentary facies was also analyzed. During the Shanxi stage, a delta front was deposited in the Huanxian region and delta plains and fronts were deposited in the Pingliang, Chunhua-Yaoxian and Hancheng-Chengcheng regions. In the Yan'an-Daning region, only a delta front was developed. The distribution of sedimentary facies in the earlier Shihezi stage originated from the Shanxi stage. A delta front was developed in the Huanxian region while a delta plain and front developed in the Pingliang-Zhenyuan region during the same time. Lakes originated only in the Zhenyuan-Huanxian-Huachi-Zhengning and Daning-Jixian zones. This analytical method shows that different palaeodrainage patterns can be effectively distinguished in order to forecast sedimentary facies.

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鄂尔多斯盆地南部山西组和下石河子组古水系重建及沉积相分布
研究区位于环县南部、延安和浦县之间,西安市北部。山西组及下石河子组是重要的含气组。通过对河流走向、古水系稳定重矿物和长石含量的分析,将研究区划分为6个古水系,对应6个长石区和6个沉积相区。在此基础上,分析了沉积相的分布。山西期环县地区发育三角洲前缘,平凉地区、春华-尧县地区和汉城-城城地区发育三角洲平原和三角洲前缘。延安-大宁地区仅发育三角洲前缘。石河子早期沉积相的分布源于山西期。环县地区发育三角洲前缘,平凉—镇远地区同期发育三角洲平原和三角洲前缘。湖泊仅发源于镇原-环县-华池-正宁和大宁-蓟县一带。该分析方法表明,可以有效区分不同的古水系模式,从而预测沉积相。
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